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vox_mundi

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Re: What's new in the Arctic ?
« Reply #850 on: June 28, 2023, 09:26:20 PM »
might have some impact on the appearance/disappearance of the cold blob SE of Greenland ...

Stronger Winds Shift Water From the Labrador Current Eastward, With Dire Consequences for Marine Ecosystems
https://phys.org/news/2023-06-stronger-shift-labrador-current-eastward.html



Changes to the flow of the Labrador Current along the coast of Newfoundland and Labrador to Nova Scotia are leading to sudden warmings or drops in the oxygen levels of the waters in several regions including the St. Lawrence Gulf and Estuary. This change has dire consequences for marine ecosystems and fisheries.

To better predict what could happen in the future, researchers from McGill University set out to answer the question: What controls the pathway of the Labrador Current?

Their study is published in the journal Nature Communications.

The Labrador Current is a cold water current in the North Atlantic Ocean that flows south along the coast of Newfoundland and Labrador, continuing partially along the east coast of Nova Scotia and partially turning eastward towards Europe. This cold water current then meets the warm waters of the Gulf Stream, which flows from the Gulf of Mexico into the Atlantic Ocean.

The Labrador Current, which flows from the Arctic Ocean, transports cold waters southwards, producing a cooling effect on the Atlantic provinces in Canada and on the United States' northeast coast from Maine to Massachusetts.

However, since 2008, less of the Labrador Current reaches the Atlantic Provinces and the northeast coast of the United States. "The result is less dissolved oxygen in the water, meaning species must spend more energy on respiration and less on feeding and other activities. The lower the oxygen concentrations, the smaller species like cod and halibut become," says Mathilde Jutras a Ph.D. candidate in the Department of Earth and Planetary Sciences at McGill University. "It also leads to the displacement of individuals, as they generally try to avoid hypoxic areas or where oxygen is very low."

"We want to understand why the Labrador Current sometimes veers east to feed the subpolar North Atlantic seas and other times it veers west to flow along the eastern American continental shelf, stretching from the United States' east coast to Nova Scotia," says Jutras, who studies oceanography. "When the Labrador Current goes east, we have heat waves along the American continental shelf and deoxygenation in the St. Lawrence Estuary."

To find answers, the team used an algorithm to track the flow and trajectories of water particles in three dimensions in an ocean simulation model. They found that the fate of the Labrador Current waters depends on a complex combination of factors.

According to the researchers, winds over the Labrador coast appear to play a role, with stronger winds veering the Labrador Current eastward. This eastward export of water is also stronger when the Gulf Stream that flows from the Gulf of Mexico comes closer to the shore, as has been the case in recent years. This happens when the Labrador Current retracts, leaving room for the Gulf Stream to shift north. The latter shift appears to also be partly driven by the winds.



Mathilde Jutras et al, Large-scale control of the retroflection of the Labrador Current, Nature Communications (2023).
https://www.nature.com/articles/s41467-023-38321-y
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Glen Koehler

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Re: What's new in the Arctic ?
« Reply #851 on: June 29, 2023, 10:46:10 PM »


     "The Atlantic has warmed ~2 degrees Fahrenheit since 1900, due to warming from emissions of greenhouse gases due to the burning of fossil fuels and also, more recently, the decrease in air pollution, allowing more sunlight through."

from:  ‘Off the charts’: Earth’s vital signs are going haywire
by Jeff Berardelli. June 29, 2023 
https://www.wfla.com/weather/climate-classroom/off-the-charts-earths-vital-signs-are-going-haywire/
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binntho

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Re: What's new in the Arctic ?
« Reply #852 on: June 30, 2023, 07:01:42 AM »
     "The Atlantic has warmed ~2 degrees Fahrenheit since 1900, due to warming from emissions of greenhouse gases due to the burning of fossil fuels and also, more recently, the decrease in air pollution, allowing more sunlight through."

Glen, I am not sure if you are somehow intending this to be some sort of comment on the sulfur claims by the toothwalker, but the "decrease in air pollution" mentioned is less airborn sand from the Sahara, which is what is causing the unusually high SSTs. It helps to give context!
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binntho

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Re: What's new in the Arctic ?
« Reply #853 on: June 30, 2023, 02:21:51 PM »
I'm sure this has been mentioned in one of the Greenland threads, thought it would be interesting to throw in here as well:

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Sigmetnow

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Re: What's new in the Arctic ?
« Reply #854 on: June 30, 2023, 04:18:23 PM »
—- Sentinel-1B replacement satellite launch likely to be delayed
The Vega-C rocket that was to launch the replacement for the Sentinel-1B satellite failed during testing on June 28.  It had been expected that the satellite’s launch would take place in the first half of 2023. Now, it is likely that the rocket’s return to flight (after its earlier failure in December 2022) will slip to no earlier than the first quarter of 2024.

Background:  An equipment failure on Sentinel-1B in December 2021 accelerated work on Sentinel-1C, originally planned to launch in December 2023.  Sentinel-1B has been retired, leaving Sentinel-1A the only satellite of the constellation.

Quote
In mid-March, a source within ESA speaking to European Spaceflight explained that the team working on Sentinel-1C was examining the possibility of qualifying the satellite to fly aboard [a SpaceX Falcon 9 rocket]. With the Sentinel-1 constellation continuing to operate under a reduced capacity, it would not be surprising if this latest delay finally pushes the satellite to the Falcon 9 launch manifest.

Of note:  SpaceX has been launching a Falcon 9 about every 4.5 days so far in 2023.

Vega C Return to Flight Delayed After Z40 Test Failure
June 29, 2023
https://europeanspaceflight.com/vega-c-return-to-flight-delayed-after-z40-test-failure/

 
https://en.wikipedia.org/wiki/Sentinel-1
 
https://en.wikipedia.org/wiki/Sentinel-1B
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johnm33

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Re: What's new in the Arctic ?
« Reply #855 on: July 05, 2023, 03:09:48 PM »
uniquorn has another post up about the openin forming north of Greenland that aligns above the Gakel ridge


I discounted it being hydrothermal vents since this is too co-incidental to my interest in them, seems the evidence begins to point that way. We should be looking for altered mineral content of seawater both in the opening and towards Svalbard, since if the heat can rise to the surface so too can the mineral discharge.

binntho

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Re: What's new in the Arctic ?
« Reply #856 on: July 06, 2023, 08:56:22 AM »
Nothing to do with ice, but might be of interest to some of you. The Reykjanes Peninsula is (most likely) about to erupt, the pattern seen now is the same as last year and similar to the first eruption in 2021.

This is likely to become another "tourist eruption" with easy access and minimal danger of poisonous gases. So if anybody hasn't yet made their holiday plans, now you know where to go! I myself will be going at the end of August, with a bit of luck the eruption will still be ongoing (if it ever starts, that is!).

Live cams here: https://www.ruv.is/frettir/innlent/2023-07-06-beint-streymi-fra-fagradalsfjalli-387091

And earthquake activity shown below - the amplitude has been dropping since yesterday and the depth decreasing, was around 2-3 km yesterday which is minimal. Both indicate that an eruption might happen any minute.

From https://en.vedur.is/earthquakes-and-volcanism/earthquakes/reykjanespeninsula/
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johnm33

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Re: What's new in the Arctic ?
« Reply #857 on: July 06, 2023, 10:13:58 AM »
Maybe I'm missing something but so far as the models go there seems to be no indication of changes to chemistry or biology associated with the opening so I'm thinking it's most likely that the motion of the ocean has begun to stir the depths, and what we have are something like cross hatched 'spouting out' from pressure waves moving both E/W and N/S in the densest strata 'punching' there way through towards the surface. From

Bardian

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Re: What's new in the Arctic ?
« Reply #858 on: July 11, 2023, 10:58:44 AM »
https://www-sintef-no.translate.goog/projectweb/gonorth/daglige-rapporter-fra-toktet2/daglige-rapporter-2023/daglig-rapport-dag-5-10.-juli/?_x_tr_sl=no&_x_tr_tl=en&_x_tr_hl=en&_x_tr_pto=wapp

"FF Crown Prince Haakon had a positioning instrument damaged by ice during an operation near the Molloy Deep northwest of Svalbard on Sunday. Now the ship has to make the trip around Tromsø for repairs. We hope to continue north to Gakkelryggen when the repair is complete."

vox_mundi

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Re: What's new in the Arctic ?
« Reply #859 on: July 13, 2023, 02:23:07 PM »
New Radar Technique Lets Scientists Probe Invisible Ice Sheet Region On Earth and Icy Worlds
https://phys.org/news/2023-07-radar-technique-scientists-probe-invisible.html

The near-surface layers of ice sheets are difficult to study with airborne or satellite ice-penetrating radar because much of what's scientifically important happens too close to the surface to be accurately imaged. That has left scientists relying on ground instruments that give only limited coverage, or extracting ice cores—a difficult and time-consuming operation currently impossible to do on other planets.

The new radar technique combines two different radar bandwidths and looks for discrepancies as a way of boosting the resolution. Because the instruments are carried on airplanes or satellites, scientists can quickly survey vast regions of ice.

To test the new technique, the team flew radar surveys over the Devon Ice Cap in the Canadian Arctic where they mapped a slab-like layer of impermeable ice near the surface. Further analysis suggested that the ice layer is redirecting surface melt from the ice cap's snow-packed surface into water channels downhill. The research was published May, 2023, in the journal The Cryosphere.

... Surface melt is normal on ice sheets during summer months. As the top of the previous winter's snow warms up, meltwater sinks in and refreezes deeper in the snow, forming thin ice layers.

Most of the ice layers on Devon Ice Cap, however, are much thicker than expected, some forming slabs as much as 16 feet thick over several miles. That makes them very effective at redirecting meltwater, which the researchers confirmed when they matched the location of the thickest ice slabs with that of meltwater rivers.



Kristian Chan et al, Spatial characterization of near-surface structure and meltwater runoff conditions across the Devon Ice Cap from dual-frequency radar reflectivity, The Cryosphere (2023)
https://tc.copernicus.org/articles/17/1839/2023/
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binntho

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Re: What's new in the Arctic ?
« Reply #860 on: July 27, 2023, 03:59:11 PM »
A recent article in Nature has generated a lot of steam in Iceland and some puffs of vapor elsewhere. Basically, a team of Danish researchers have concluded that the AMOC is about to collapse, and that this will happen as early as 2025!

Warning of a forthcoming collapse of the Atlantic meridional overturning circulation (Peter Ditlevsen, Susanne Ditlevsen, July 25 2023)

The article is quite technical and seems to be a purely mathematical analysis of a fairly limited data set. In Iceland, many people have understood this to mean that the Gulf Stream is about to stop, which would be catastrophic for Iceland and a great inconvenience for the entire European Atlantic seabord. But recently scientists have pointed out the following in Icelandic media.

1) The Nature article is about the AMOC overturning, which is only a part of the entire Gulf Stream system. The AMOC is called a "vertical" current and thought to be less stable than the larger "lateral" current, with small and large hiccups fairly common.

2) The data series used by the Ditlevsen siblings is limited and their conclusions tentative.

3) Icelandic scientists have been monitoring currents that cross the Greenland - Scotland ridge (which crosses through Iceland) for the last 30 years and the cold deep currents are remarkably stable, but the warmer surface currents seem to be speeding up with more warm water passing northwards.

The Abstract from the Nature article:

Quote
The Atlantic meridional overturning circulation (AMOC) is a major tipping element in the climate system and a future collapse would have severe impacts on the climate in the North Atlantic region. In recent years weakening in circulation has been reported, but assessments by the Intergovernmental Panel on Climate Change (IPCC), based on the Climate Model Intercomparison Project (CMIP) model simulations suggest that a full collapse is unlikely within the 21st century. Tipping to an undesired state in the climate is, however, a growing concern with increasing greenhouse gas concentrations. Predictions based on observations rely on detecting early-warning signals, primarily an increase in variance (loss of resilience) and increased autocorrelation (critical slowing down), which have recently been reported for the AMOC. Here we provide statistical significance and data-driven estimators for the time of tipping. We estimate a collapse of the AMOC to occur around mid-century under the current scenario of future emissions.
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Jim Hunt

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Re: What's new in the Arctic ?
« Reply #861 on: July 27, 2023, 06:00:02 PM »
There's been much debate in the XTwattosphere about that article.

1) "Nature Communications" is not "Nature"

2) Re assorted MSM misinterpretations - "Gulf Stream" != "AMOC"

3) See also: https://twitter.com/PFriedling/status/1684145458221043712 et seq.
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binntho

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Re: What's new in the Arctic ?
« Reply #862 on: July 27, 2023, 06:15:47 PM »
1) "Nature Communications" is not "Nature"

My bad!
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vox_mundi

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Re: What's new in the Arctic ?
« Reply #863 on: July 27, 2023, 06:26:15 PM »
AMOC.          =90 Sv (sverdrup)

Gulf Stream =15 Sv

https://forum.arctic-sea-ice.net/index.php/topic,1755.msg376088.html#msg376088
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binntho

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Re: What's new in the Arctic ?
« Reply #864 on: July 27, 2023, 07:23:30 PM »
Gulf stream is 30 sv at Florida, 150 sv at Newfoundland ... at least according to Wikipedia, I haven't actually  measured it myself.
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kassy

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Re: What's new in the Arctic ?
« Reply #865 on: July 29, 2023, 07:33:23 PM »
Earlier and earlier high-Arctic spring replaced by 'extreme year-to-year variation'



About 15 years ago, researchers reported that the timing of spring in high-Arctic Greenland had advanced at some of the fastest rates of change ever seen anywhere in the world. But, according to new evidence reported in the journal Current Biology on July 26, that earlier pattern has since been completely erased. Instead of coming earlier and earlier, it seems the timing of Arctic spring is now driven by tremendous climate variability with drastic differences from one year to the next.

"As scientists we are obliged to revisit previous work to see whether the knowledge obtained at that time still holds," says Niels Martin Schmidt of Aarhus University in Denmark. "We looked at previously reported extreme rates of phenological advancements in the Arctic and found that directional advancement is no longer the prevailing pattern. Actually, the previously observed trend has disappeared completely and has been replaced by extreme year-to-year variation in the onset of spring."

Global changes in climate are expected to take place faster in the Arctic than in places at lower latitudes. To follow those trends, researchers at Zackenberg in Northeast Greenland launched an ecosystem-wide monitoring program in 1996. Among a suite of ecosystem variables, the program also tracks the timing of spring based on flowering plants, arthropod emergence, and bird nesting.

When the first 10 years of data were analyzed for 1996-2005, the findings showed a clear pattern of advancement across plants and animals included in the study. For instance, they saw some arthropods emerging up to 4 weeks earlier. In the new study, Schmidt and his colleagues wanted to see how these trends look now that they have 15 additional years of data available.

After analyzing the phenological data from 1996-2020, they report little evidence of directional change in the timing of events even as climate change continues. The researchers attribute this shift to a high degree of climate variability from year to year.

"That the extreme rates of phenological advancement we reported back in 2007 would not have continued unabated was not surprising to us," Schmidt said. "However, that we see such a consistent shift from directional to extreme variability across so many different organisms and that the entire ecosystem now seems driven by variation in climatic conditions, was surprising."

Schmidt says that the previous pattern showed steadily rising temperatures and declining snow cover. Now, what they see is a lot messier. Temperature increases have stalled while snow cover fluctuates dramatically from year to year.

https://www.sciencedaily.com/releases/2023/07/230726113056.htm
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gerontocrat

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Re: What's new in the Arctic ?
« Reply #866 on: July 29, 2023, 08:49:43 PM »
Yet more evidence that the climate is entering a chaotic state?
Earlier and earlier high-Arctic spring replaced by 'extreme year-to-year variation'

Instead of coming earlier and earlier, it seems the timing of Arctic spring is now driven by tremendous climate variability with drastic differences from one year to the next.

...the previously observed trend has disappeared completely and has been replaced by extreme year-to-year variation in the onset of spring."

After analyzing the phenological data from 1996-2020, they report little evidence of directional change in the timing of events even as climate change continues. The researchers attribute this shift to a high degree of climate variability from year to year.

Schmidt said. "However, that we see such a consistent shift from directional to extreme variability across so many different organisms and that the entire ecosystem now seems driven by variation in climatic conditions, was surprising."

Schmidt says that the previous pattern showed steadily rising temperatures and declining snow cover. Now, what they see is a lot messier. Temperature increases have stalled while snow cover fluctuates dramatically from year to year.

https://www.sciencedaily.com/releases/2023/07/230726113056.htm
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kassy

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Re: What's new in the Arctic ?
« Reply #867 on: July 30, 2023, 07:38:07 PM »
I think so. I half wanted to mention spinning tops but the implication is clear enough.

Also the focus is shifting. Where once we were waiting on a BOE to wake people up attention should have shifted to the ridiculous ocean temperatures by now. For the next decade and a half we will see Thwaites collapse, the effects from AABW that AMOC thingy maybe etc. And of course a BOE so yes i would vote for chaotic state.

 
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gerontocrat

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Re: What's new in the Arctic ?
« Reply #868 on: August 12, 2023, 12:43:21 PM »
Rainy days in the Arctic are increasing. This study suggests the analysis of these events is unreliable - another data deficiency.

https://www.sciencedirect.com/science/article/pii/S1674927823000916?via%3Dihub
Performance of climate reanalyses in the determination of pan-Arctic terrestrial rain-on-snow events
Quote
Abstract
Rain-on-snow (ROS) events can cause rapid snowmelt, leading to flooding and avalanches in the pan-Arctic and can also lead to starvation and the death of massive ungulates. Reanalysis products (e.g., ERA-I, ERA5-land, JRA55, MERRA2) are the primary source data for the research about ROS events in the large-scale region. However, the accuracy and reliability of reanalyses have never been evaluated with respect to the determination of terrestrial ROS events. The present study aims to statistically evaluate the performance of reanalysis datasets in identifying ROS events with different criteria based on in-situ rainfall data and MODIS snow cover product. The results show that all reanalysis datasets exhibit poor performance (Recall ≤ 0.16, kappa coefficient ≤ 0.26, F-score ≤ 0.42, MCC ≤ 0.33) in all criteria in the pan-Arctic, mainly due to the low accuracy of rainfall data (r≤ 0.56). Nevertheless, the spatial distribution pattern and hot spots of ROS from all reanalysis datasets are essentially close. The hot spots of ROS are mainly located on the coast of Alaska, Norway, and Greenland.

All reanalyses demonstrate an increase in rainy days, but there is little overall change in ROS events due to the reduction in snow cover days. This work suggests that none of the current reanalyses are reliable in the determination of ROS events due to the poor representation of the rainfall parameterization scheme. The development of alternative strategies that can investigate ROS events at large-scale is urgently needed in a changing Arctic under rapid warming.
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binntho

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Re: What's new in the Arctic ?
« Reply #869 on: August 19, 2023, 12:03:25 PM »
The Barents Observer: China's icebreaker Xuelong-2 is sailing to the North Pole

Quote
It is the country’s 13th Arctic Ocean scientific expedition and the fourth voyage to the region by Xuelong-2, the new and fully Chinese-built icebreaker.
...
The researchers will also conduct investigations of atmospheric, sea ice, marine and subsurface environmental surveys, as well as surveys of biomes and pollutants.

According to Wang Jinhui, head of the expedition team, a key objective is to collected genetic specimens from the region.
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vox_mundi

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Re: What's new in the Arctic ?
« Reply #870 on: September 02, 2023, 02:27:14 AM »
New Research Explains 'Atlantification' of the Arctic Ocean
https://phys.org/news/2023-09-atlantification-arctic-ocean.html

New research by an international team of scientists explains what's behind a stalled trend in Arctic Ocean sea ice loss since 2007. The findings indicate that stronger declines in sea ice will occur when an atmospheric feature known as the Arctic dipole reverses itself in its recurring cycle.

The many environmental responses to the Arctic dipole are described in a paper published online today in the journal Science. This analysis helps explain how North Atlantic water influences Arctic Ocean climate. Scientists call it Atlantification.

... "This is a multidisciplinary view on what's going on in the Arctic and beyond," Polyakov said of the new research. "Our analysis covered the atmosphere, ocean, ice, changing continents and changing biology in response to climate change."

A wealth of data, including direct instrumental observations, reanalysis products and satellite information going back several decades, shows that the Arctic dipole alternates in an approximately 15-year cycle and that the system is probably at the end of the present regime.

In the Arctic dipole's present "positive" regime, which scientists say has been in place since 2007, high pressure is centered over the Canadian sector of the Arctic and produces clockwise winds. Low pressure is centered over the Siberian Arctic and features counterclockwise winds.

This wind pattern drives upper ocean currents, with year-round effects on regional air temperatures, atmosphere-ice-ocean heat exchanges, sea-ice drift and exports, and ecological consequences.

The authors write that, "Water exchanges between the Nordic seas and the Arctic Ocean are critically important for the state of the Arctic climate system" and that sea ice decline is "a true indicator of climate change."



In analyzing oceanic responses to the wind pattern since 2007, the researchers found decreased flow from the Atlantic Ocean into the Arctic Ocean through the Fram Strait east of Greenland, along with increased Atlantic flow into the Barents Sea, located north of Norway and western Russia.

The new research refers to these alternating changes in the Fram Strait and the Barents Sea as a "switchgear mechanism" caused by the Arctic dipole regimes.

The researchers also found that counterclockwise winds from the low-pressure region under the current positive Arctic dipole regime drive freshwater from Siberian rivers into the Canadian sector of the Arctic Ocean.

This westward movement of freshwater from 2007 to 2021 helped slow the overall loss of sea ice in the Arctic compared to 1992 through 2006. The freshwater layer's depth increased, making it too thick and stable to mix with the heavier saltwater below. The thick layer of freshwater prevents the warmer saltwater from melting sea ice from the bottom.

The authors write that the switchgear mechanism regulating inflows of sub-Arctic waters has "profound" impacts on marine life. It can lead to potentially more suitable living conditions for sub-Arctic boreal species near the eastern part of the Eurasian Basin, relative to its western part.

Quote
... "We are beyond the peak of the currently positive Arctic dipole regime, and at any moment it could switch back again," ... "This could have significant climatological repercussions, including a potentially faster pace of sea-ice loss across the entire Arctic and sub-Arctic climate systems."

Igor V. Polyakov et al, Fluctuating Atlantic inflows modulate Arctic atlantification, Science (2023).
https://www.science.org/doi/10.1126/science.adh5158

Sheldon Bacon, Arctic sea ice, ocean, and climate evolution, Science (2023)
https://www.science.org/doi/10.1126/science.adj8469

Abstract

Enhanced warm, salty subarctic inflows drive high-latitude atlantification, which weakens oceanic stratification, amplifies heat fluxes, and reduces sea ice. In this work, we show that the atmospheric Arctic Dipole (AD) associated with anticyclonic winds over North America and cyclonic winds over Eurasia modulates inflows from the North Atlantic across the Nordic Seas. The alternating AD phases create a “switchgear mechanism.” From 2007 to 2021, this switchgear mechanism weakened northward inflows and enhanced sea-ice export across Fram Strait and increased inflows throughout the Barents Sea. By favoring stronger Arctic Ocean circulation, transferring freshwater into the Amerasian Basin, boosting stratification, and lowering oceanic heat fluxes there after 2007, AD+ contributed to slowing sea-ice loss. A transition to an AD− phase may accelerate the Arctic sea-ice decline, which would further change the Arctic climate system.
« Last Edit: September 02, 2023, 02:44:15 AM by vox_mundi »
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Sublime_Rime

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Re: What's new in the Arctic ?
« Reply #871 on: September 02, 2023, 04:57:16 AM »
Wow, I don't have the expertise to interpret the credibility of this publication, but seems to be quite a major finding to explain many observations made on this forum for the past 10 years or so (at least the past 8 years that I've been lurking). Also with major implications for the next few years. Would the El Nino increase the odds of a tip into the new regime?
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binntho

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Re: What's new in the Arctic ?
« Reply #872 on: September 02, 2023, 12:22:27 PM »
This is a very interesting article, and of course time will tell if they are right or not.

BUT I am very suspicious about their claim of a stall since 2007, and a 15 year cycle in rate of extent loss and was hoping to see some discussion justifying this. The papers are behind a paywall and I am unable to read them. It may very well be that their climatological data supports a change around 2007, and a 15 year cycle, but it is not at all evident that this has a direct effect on the rate of sea ice loss at minimum.

The image below is highly suspicious and I am surprised that it gets published in a scientific journal, with the red lines placed totally without any justification, other than placing them to support a supposed 15 year cycle.

With every year, it does seem more and more likely that a the last decade or so has seen a statistically significant slowdown, but the jury is still very much out (and arguing and getting drunk and roomjumping) when it comes to explaining the apparent decadal changes in rate of sea ice extent during the satellite era. Any attempt at explanation has to cover all the 43+ years of satellite measurements, and no attempt has even come close to providing a quantitative or qualitative explanation of any decadal rate changes.

Not to say that this couldn't be the one of the better attempts (i.e. 15 year dipole cyclus), but again - time will tell.
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Richard Rathbone

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Re: What's new in the Arctic ?
« Reply #873 on: September 02, 2023, 07:49:37 PM »
This.
This is a very interesting article, and of course time will tell if they are right or not.

BUT I am very suspicious about their claim of a stall since 2007, and a 15 year cycle in rate of extent loss and was hoping to see some discussion justifying this. The papers are behind a paywall and I am unable to read them. It may very well be that their climatological data supports a change around 2007, and a 15 year cycle, but it is not at all evident that this has a direct effect on the rate of sea ice loss at minimum.

The image below is highly suspicious and I am surprised that it gets published in a scientific journal, with the red lines placed totally without any justification, other than placing them to support a supposed 15 year cycle.

With every year, it does seem more and more likely that a the last decade or so has seen a statistically significant slowdown, but the jury is still very much out (and arguing and getting drunk and roomjumping) when it comes to explaining the apparent decadal changes in rate of sea ice extent during the satellite era. Any attempt at explanation has to cover all the 43+ years of satellite measurements, and no attempt has even come close to providing a quantitative or qualitative explanation of any decadal rate changes.

Not to say that this couldn't be the one of the better attempts (i.e. 15 year dipole cyclus), but again - time will tell.

Glen Koehler

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Re: What's new in the Arctic ?
« Reply #874 on: September 08, 2023, 04:05:25 AM »
      Interesting (though not always technically spot on) press article about two important 2023 ASI research articles at Southern atmospheric rivers drive irreversible melting of Arctic sea ice: Study by Alec Luhn on 23 March 2023  https://news.mongabay.com/2023/03/southern-atmospheric-rivers-are-melting-the-arctic-sea-ice-it-may-never-recover-study/#Echobox=1678901808-1

     The two studies discussed are:
Hiroshi Sumata, Laura de Steur, Dmitry V. Divine, Mats A. Granskog & Sebastian Gerland. March, 2023. Regime shift in Arctic Ocean sea ice thickness. Nature.

Pengfei Zhang, Gang Chen, Mingfang Ting, L. Ruby Leung, Bin Guan & Laifang Li. February, 2023. More frequent atmospheric rivers slow the seasonal recovery of Arctic sea ice. Nature Climate Change.

Excerpts from figure legends for attached graphics from Sumata et al. 2023:
Fig. 3.  "Time series of residence time of ice floes in the Arctic Basin"

Fig. 4. TPB = Transpoloar Drift
"a,b, Difference of September sea ice concentration (a) and ice drift speed (b) between the two periods: 1990–2006 and 2007–2019.
c,d, Time series of mean sea ice concentration in September (c) and mean sea ice drift speed in selected regions (d).

a, The positive (negative) values indicate increase (decrease) in the latter period.
b, The difference in sea ice drift vector is shown by the arrows, while its magnitude is shown by the colour. The difference in sea ice drift field in b was calculated from ice drift vectors from December to May.

The time series in c are the areal average of the Alaskan (A) and Siberian sectors (B) shown by the solid black polygon in a, while those in d are the areal average of A, B and C: the TPD Stream is shown by the rectangular box labelled C. The ice drift speed of the TPD in d shows the annual mean ice drift speed in box C (vector component parallel to the main axis of box C, positive value oriented to the Fram Strait), whereas those in A and B are calculated without three summer months (August to October) to exclude under-represented ice motion due to very low spatial coverage in recent years."
« Last Edit: September 08, 2023, 09:59:10 AM by Glen Koehler »
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gerontocrat

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Re: What's new in the Arctic ?
« Reply #875 on: September 14, 2023, 09:35:09 PM »
What's new in the Arctic ? A lot more rainy days. But I think we knew that.

paywalled - so summary only.

https://journals.ametsoc.org/view/journals/clim/36/19/JCLI-D-22-0428.1.xml
Quote
Rainy Days in the Arctic
Abstract

The Arctic is warming faster than anywhere on Earth, and with these warming temperatures, there is likely to be more precipitation falling as rain. This precipitation phase change will have profound impacts on the hydrologic cycle, energy balance, and snow and sea ice mass budgets.

Here, we examine the number of rainfall days in the Arctic from three reanalyses, ERA-Interim, ERA5, and MERRA-2, over 1980–2016. We show that the number of rainfall days has increased over this period, predominantly in the autumn and in the North Atlantic and peripheral seas, and the length of the rain season has increased in all reanalyses. This is positively correlated to the number of days with above freezing air temperatures and a lengthening of the warm season.

ERA-Interim produces significantly more rainfall days than other reanalyses and CloudSat observations, as well as significantly more rainfall when temperatures are below freezing. Investigation into the cloud microphysics schemes revealed that the scheme employed by ERA-Interim allowed for mixed-phase clouds to form rain at temperatures below freezing following a temperature-dependent phase partitioning function between 250 and 273 K. This simple diagnostic treatment erroneously overestimates rain at temperatures below 273 K and produces unrealistic rainfall compared to ERA5 and MERRA-2. This work highlights the importance of having accurate physics and improving microphysical schemes in models for simulating precipitation in the Arctic and the caution that is warranted for interpreting reanalysis trends.
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vox_mundi

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Re: What's new in the Arctic ?
« Reply #876 on: September 21, 2023, 05:33:18 PM »
Riddle of Varying Warm Water Inflow In the Arctic Now Solved
https://phys.org/news/2023-09-riddle-varying-inflow-arctic.html



In the "weather kitchen," the interplay between the Azores High and Icelandic Low has a substantial effect on how much warm water the Atlantic transports to the Arctic along the Norwegian coast. But this rhythm can be thrown off for years at a time.

Experts from the Alfred Wegener Institute finally have an explanation for why: Due to unusual atmospheric pressure conditions over the North Atlantic, low-pressure areas are diverted from their usual track, which disrupts the coupling between the Azores High, the Icelandic Low and the winds off the Norwegian coast. This finding is an important step toward refining climate models.

... A team led by oceanographer Finn Heukamp from the Alfred Wegener Institute, Helmholtz Center for Polar and Marine Research (AWI) has just published a study in the journal Communications Earth & Environment, in which he and his colleagues investigated ocean currents along the Norwegian coast and into the Barents Sea. Their focus was on the atmospheric pressure difference between the Azores High and the Icelandic Low, also known as the North Atlantic Oscillation (NAO), which shapes the currents off of Norway.

They were particularly interested in the question of why there are (in some cases, extreme) deviations from the typical interplay between the NAO and weather conditions. Normally, the intensity of the winds and therefore the ocean currents is predominantly determined by the atmospheric pressure difference in the NAO.

When the NAO is more pronounced, it creates powerful air currents, which drive low-pressure areas across the North Atlantic and past Norway on their way north. When the atmospheric pressure difference lessens, both the winds and the low-pressure areas run out of momentum.

As such, the NAO, the low-pressure areas' track, and the intensity of the ocean currents off the coast of Norway are normally closely interconnected. However, a decoupling of the NAO and ocean currents was observed in the Barents Sea as far back as the late 1990s.

"This unusual decoupling frequently manifested in winter between the years 1995 and 2005," says Heukamp. "But the cause of these changes was unclear." Thanks to a mathematical ocean model that simulates the Arctic Ocean at very high resolution, the experts now have the answer.

Apparently, the phenomenon is caused by an unusual change in the low-pressure areas' track. Heukamp has now determined that the stream of low-pressure areas that pass by Norway, moving from the southwest to the north, is at times disrupted by powerful, nearly stationary high-pressure areas, also known as blocking highs. The latter push the fast-moving low-pressure areas out of their normal track. As a result, the NAO and the northward flow of warm water are temporarily decoupled.

"Global climate models simulate on a comparatively broad scale," the researcher explains. "With the latest results from our high-resolution analysis for the North Atlantic and the Arctic, we've now added an important detail for making climate modeling for the Arctic even more accurate." They also show that, in future, the NAO, the low-pressure areas over the Atlantic, and the ocean currents need to increasingly be viewed together.

Given that both the transport of warm water and the track of lows over the Atlantic affect our weather in the middle latitudes, the results are also interesting in terms of more accurately predicting the future climate and weather in Central Europe.

Finn Ole Heukamp et al, Cyclones modulate the control of the North Atlantic Oscillation on transports into the Barents Sea, Communications Earth & Environment (2023)
https://www.nature.com/articles/s43247-023-00985-1



Composite maps of 850 hPa geopotential height anomalies and associated wind anomalies (DJFM) during strong (a) and weak (b) net transport through Barents Sea Opening (BSO) based on JRA55.
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kassy

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Re: What's new in the Arctic ?
« Reply #877 on: September 26, 2023, 08:58:31 PM »
In Arctic Lakes, Scientists Watch For a Shifting Carbon Cycle

...

Lake SS85 is one of hundreds of lakes dotting this 90-mile-wide fringe of land between the towering Greenland Ice Sheet and the Labrador Sea. For centuries, 85 and its aquatic neighbors have been ice-covered most of the year. But as the climate has warmed, high-latitude lakes — from the northern United States and Canada to Scandinavia and Siberia — have started to thaw, on average, a week earlier and freeze 11 days later than they did a century ago, according to Sapna Sharma, a biologist at York University in Toronto. The rate of ice loss has sextupled over the past 25 years. Northern lake temperatures are rising more than twice as fast as the global lake average, Sharma says. And nowhere is the climate changing faster than in the Arctic.

The boreal forests and unglaciated polar lowlands are Earth’s most lake-rich biome, hosting nearly half of the planet’s lakes by surface area. While precise data are sparse, a 2015 satellite-based inventory estimates some 3.5 million lakes cover a total of around 150,000 square miles in the Arctic. But due to the difficulty of conducting research in the remote north, relatively little is known about how these vast freshwater ecosystems are responding to the sweeping changes underway.

One of scientists’ key questions is how rising temperatures, shrinking ice seasons, and the increasing precipitation projected for many parts of the Arctic might affect lakes’ carbon cycles. Put simply, this cycle describes the actions of aquatic microbes that break down organic material — exhaling carbon dioxide and other greenhouse gases — and phytoplankton that take up carbon dioxide to build their skeletons — releasing oxygen. Lakes that breathe out more carbon dioxide than they take in are net carbon sources, while those that on balance remove carbon dioxide from the atmosphere are sinks.

...

“We are trying to understand the carbon budget in the Arctic,” says Hazuková. The stakes are high: That ledger of sinks and sources informs the models that scientists use to project the Earth’s future climate. Currently, however, the estimate “pretty much only focuses on soils and vegetation,” she says. “Freshwaters are just not included at all.”

Some of those freshwater systems are changing “very, very quickly,” says John Smol, a paleolimnologist at Queens University in Kingston, Ontario. Earlier thaws and later freezes expose lakes to more light, heat, and contact with the outside world. The impacts compound at high latitudes, such as the lakes on Canada’s Ellesmere Island that Smol has studied for decades. The summer ice-free period up there used to be six weeks at most, he says. With 24-hour daylight during the Arctic summer, less time under ice cover opens lakes to significantly more time under the sun.

Arctic lakes are diverse, however, and climate change is manifesting differently across regions. In areas where rapidly thawing permafrost releases once-frozen stores of plants and other organic material into lakes, microbes are feasting on those extra helpings of carbon and belching out carbon dioxide and methane. Thermokarst lakes such as Alaska’s Big Trail Lake visibly boil with escaping greenhouse gases. Across the boreal region, the total annual carbon dioxide emissions from lakes is equivalent to that of forest fires, according to a study conducted in 2017 (before the recent extreme wildfire seasons).

But those amped-up emissions may be offset, at least in part, by lakes that emit little or even sponge up carbon. In a 2019 survey of Alaska’s Yukon River Basin, biogeochemist Matthew Bogard found lakes in that flat, dry region produce “negligible” CO2 emissions. That’s because those lakes have little hydrologic connection to the surrounding landscape, which means almost no organic material is delivered to the lakes through outside water flowing in, explains Bogard, who is now at the University of Lethbridge in Alberta.

Data on Arctic emissions are patchy overall, Bogard acknowledges. “We need more data from understudied regions.”

...

Except this summer isn’t normal. Across the Northern Hemisphere, 2023 will turn out to be the hottest summer on record, according to the European Union’s Copernicus Climate Change Service. In West Greenland, we see day after day of rain. Everyone in Kangerlussuaq is talking about the extraordinary weather. Longtime resident Vivi Grønvald tells me she’s never seen a summer this wet. “It’s like we haven’t had a summer at all,” she laments. The period from May to July ends up breaking West Greenland precipitation records dating back to 1940, climatologist Sean Birkel, developer of the University of Maine’s Climate Reanalyzer, found in an August analysis. Birkel linked the season’s extreme precipitation to large circulation anomalies, including unusually weak North Atlantic winds, likely related to the 2023 El Niño.

For lake scientists, all that rain makes for murky work. Usually, these lakes are crystal clear, says project co-lead Jasmine Saros, a University of Maine ecologist who has worked in the area for more than a decade. But this year, the water is the color of coffee. “This is the first time I’ve seen these lakes like this,” Saros says. “So dark.”

...

“The data that we got so far from the carbon sensors shows all the lakes were carbon sources,” Hazuková says, leaning over a computer screen filled with numbers. “Between April and now, they were carbon sources the whole time.”

That’s the opposite of what the researchers expected. “The reason why we started this study is that we thought these lakes were going to be sinks of carbon, at least during the summer … because they are not receiving organic matter to fuel respiration,” Hazuková reflects. “But what we saw this year was just unprecedented.”

So unprecedented, in fact, that Hazuková and Saros return to Kangerlussuaq in August for another look. They speed-hike the same route, covering around 60 miles in a week. The West Greenland weather has returned to its usual rainless days of long summer sun. The lakes are still brown, but their carbon dioxide levels have dropped, and several are once again behaving like sinks, says Hazuková.

...

https://undark.org/2023/09/26/arctic-lakes-carbon/

A couple of years ago there was a paper looking at the output in Alaskan lakes and the balance of CO2 and CH4 plus they sampled the waters to see what was involved. It was complicated.

In the grand scheme of things this is the time when the northern forest burn and the lakes thaw but it is interesting to find out more about what is going on.
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vox_mundi

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Re: What's new in the Arctic ?
« Reply #878 on: October 06, 2023, 05:30:14 PM »
Confirmed: Salmon are spawning in Arctic rivers
https://www.uaf.edu/news/confirmed-salmon-are-spawning-in-arctic-rivers.php

Researchers have confirmed that salmon are spawning in an Arctic Ocean watershed, suggesting that at least some salmon species could be expanding to new territory as climate change reshapes their habitat.

The University of Alaska Fairbanks-led project found about 100 chum salmon in the Anaktuvuk and Itkillik rivers on Alaska's North Slope. Both rivers flow into the Colville River, which empties into the Arctic Ocean. All the fish that researchers caught in mid-September 2023 were either actively spawning or had finished spawning at sites where groundwater appeared to be flowing to the surface. Similar conditions have supported chum salmon reproduction throughout their typical range.

... "Throughout most parts of the salmon's range, things have gotten too warm and they're starting to blink off," said Westley, an associate professor at UAF's College of Fisheries and Ocean Sciences. "In the Arctic, the water is getting warm enough and they're starting to blink on."

Westley, who has studied potential shifts in salmon habitat for the past decade, credited a December 2022 workshop for shaping the goals of this research. Scientists, community members and Indigenous fishermen met in Anchorage to discuss the increasing number of salmon being observed in the Arctic Ocean and their possible origin.

The workshop helped steer researchers toward the Colville River watershed, approximately 60 miles southwest of Prudhoe Bay.

"One major theme was that salmon have always been on the North Slope, but they're also increasing in recent years," said Elizabeth Mik'aq Lindley, a UAF graduate student who helped organize the meeting. "I don't want to portray our discovery as the first ever. That assumes no one has ever seen this before, and people have been there for thousands of years."

"Straying is part of the biological story of salmon—it's what they do," he said. "It's a fundamental part of their biology and evolution. In the Arctic, we can see it playing out before our eyes."

It's still unknown whether attempts by salmon to reproduce in the region have been successful. Researchers have left temperature sensors in some of the chum salmon nests to determine whether the rivers completely freeze during the winter, destroying any developing embryos. A return trip is planned in fall 2024 to look for smolt or a new wave of spawning adults. Salmon bones and tissue will also undergo analyses to help determine whether the fish lived their entire lives in Arctic waters.
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vox_mundi

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Re: What's new in the Arctic ?
« Reply #879 on: October 24, 2023, 03:19:57 PM »
Declining Bering Sea Ice Linked to Increasing Wildfire Hazard In Northeast China
https://phys.org/news/2023-10-declining-bering-sea-ice-linked.html



The northeast of China (120°E–135°E and 40°N–50°N) has experienced an upsurge in polluting emissions from natural and anthropogenic-induced wildfires and the resulting biomass burning over the last decade, accounting for approximately 60% of total burned area in the country. This region possesses some of the greatest and most diverse tree coverage in China, meaning it is a critical natural ecosystem and resource under threat.

The cause of these wildfires is the focus of new research published in Geophysical Research Letters, which links a decline in sea ice moving from the Arctic to the Bering Sea, north Pacific Ocean (160°E–158°W, 53°N–66°N), to increased occurrence of fires during boreal spring (March, April and May).

Guanyu Liu and colleagues from Peking University, China, used climate model simulations alongside real observational data to understand this link and identify fire hazard intensification as this pattern amplifies with continued global warming. The research team used meteorological data from the past 40 years to understand weather changes conducive to wildfire events, alongside data of smoke concentrations and fire radiative power.

Modeling identified a one-month lag between disruption to Bering Sea ice and the presence of wildfires, which the scientists suggest may be impacted by ice albedo feedbacks. This occurs when radiative forcing from the sun is either reflected by "white" ice, or absorbed by the surrounding comparatively "dark" sea water. In the latter case, this causes the ambient environment to warm, resulting in further melting of sea ice and absorption of solar radiation, generating a feedback loop that continuously progresses the decline of sea ice.



A weakened temperature gradient between the Arctic and lower latitudes encourages a reduced polar and subtropical jet stream and consequently weakened wind shear (the change in horizontal wind direction/speed with height). Thus, this reduces vertical atmospheric convection above northeast China, making the formation of clouds less likely, and therefore the possibility of precipitation. (... sounds like Canada)

In the computed experiments, Liu and colleagues found that sea ice decline during winter leads to decreased precipitation and warmer temperatures in northeast China, affected by unusual higher-speed northwesterly wind patterns and the formation of high-pressure centers with downward-directed airflow. As such, they suggest this creates a tinderbox of hot, dry conditions ready to ignite at any moment and spread rapidly via strong wind regimes.

Such conditions are further exacerbated by global-scale climate patterns, such as the El-Niño Southern Oscillation and Pacific Decadal Oscillation, atmosphere-ocean interactions impacted by sea surface temperature in the Pacific Ocean. Both of these climate oscillations encourage drought during their warm positive phases and therefore heighten the potential for wildfire occurrence.

Translating this knowledge to future predictions under the most extreme climate scenario of Shared Socioeconomic Pathway 8.5 (SSP585), where radiative forcing increases by 8.5W/m2 by 2100, the research team identified a clear pattern of continued Bering Sea ice decline and the occurrence of more wildfires in northeast China. For the lower radiative forcing of 7W/m2 (SSP370), wildfire occurrence was still higher than what has occurred over historical measurements, but the pattern is less distinct for the lowest radiative forcings of 2.67W/m2 (SSP126) and 4.57W/m2 (SSP245).

With Arctic sea ice concentration predicted to disappear entirely during summer months by the 2050s, the likelihood of more frequent and damaging wildfires is an ever-pressing issue that requires management strategies to be implemented as soon as possible, no matter the level of climate change forcing.

Guanyu Liu et al, Increasing Fire Weather Potential Over Northeast China Linked to Declining Bering Sea Ice, Geophysical Research Letters (2023).
https://agupubs.onlinelibrary.wiley.com/doi/10.1029/2023GL105931
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kassy

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Re: What's new in the Arctic ?
« Reply #880 on: November 07, 2023, 02:25:01 PM »
New research explains "Atlantification" of the Arctic Ocean

What's behind a stalled trend in Arctic Ocean sea-ice loss

New research by an international team of scientists describes the causes for the stalled trend in Arctic Ocean sea-ice loss since 2007. The findings indicate that stronger declines in sea ice will occur when an atmospheric feature known as the Arctic dipole reverses itself in its recurring cycle.

Environmental responses to the Arctic dipole are described in a paper published in the journal Science. The analysis helps explain how North Atlantic water influences the Arctic Ocean climate. Scientists refer to this phenomenon as Atlantification.

The U.S. National Science Foundation-supported research is led by Igor Polyakov of the University of Alaska Fairbanks. "This is a multidisciplinary view on what's going on in the Arctic and beyond," Polyakov said. "Our analysis covered the atmosphere, ocean, ice, changing continents and changing biology in response to climate change."

A wealth of data, including direct instrumental observations, reanalysis products and satellite information going back several decades, show that the Arctic dipole alternates in an approximately 15-year cycle and that the system is probably at the end of the present period.

"Evidence of Atlantification in the Arctic demonstrates that local to regional changes in atmospheric processes and ocean properties have implications for understanding and forecasting Earth climate systems arising from a changing Arctic," said Roberto Delgado, a program director in NSF's Office of Polar Programs.

In the Arctic dipole's present "positive" state, which scientists say has been in place since 2007, high pressure is centered over the Canadian sector of the Arctic and produces clockwise winds. Low pressure is centered over the Siberian Arctic and features counterclockwise winds.

This wind pattern drives upper ocean currents, with year-round effects on regional air temperatures, atmosphere-ice-ocean heat exchanges, sea-ice drift and exports, and ecological consequences.

The authors write that "water exchanges between the Nordic seas and the Arctic Ocean are critically important for the state of the Arctic climate system" and that sea-ice decline is "a true indicator of climate change."

In analyzing oceanic responses to the wind pattern since 2007, the researchers found decreased flow from the Atlantic Ocean into the Arctic Ocean through the Fram Strait, east of Greenland, along with increased Atlantic flow into the Barents Sea, located north of Norway and western Russia.

The new research refers to these alternating changes in the Fram Strait and the Barents Sea as a "switchgear mechanism" caused by the Arctic dipole cycles.

The scientists state that the switchgear mechanism regulating inflows of sub-Arctic waters has profound impacts on marine life. It could lead to more suitable living conditions for sub-Arctic boreal species near the eastern part of the Eurasian Basin, relative to its western part.

"We are beyond the peak of the currently positive Arctic dipole regime, and at any moment it could switch back again," Polyakov said. "This could have significant climatological repercussions, including a potentially faster pace of sea-ice loss across the entire Arctic and sub-Arctic climate systems."

https://new.nsf.gov/news/new-research-explains-atlantification-arctic-ocean
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vox_mundi

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Re: What's new in the Arctic ?
« Reply #881 on: November 07, 2023, 04:39:26 PM »
There are 3 classes of people: those who see. Those who see when they are shown. Those who do not see

Insensible before the wave so soon released by callous fate. Affected most, they understand the least, and understanding, when it comes, invariably arrives too late

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vox_mundi

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Re: What's new in the Arctic ?
« Reply #882 on: November 07, 2023, 04:48:18 PM »
First Assimilation of CryoSat-2 Summer Observations Provides Accurate Estimates of Arctic Sea Ice Thickness
https://phys.org/news/2023-11-assimilation-cryosat-summer-accurate-arctic.html



Scientists have improved a data assimilation system for better estimating Arctic summer sea ice thickness (SIT) by assimilating satellite-based summer SIT and ice concentration data with an incremental analysis update (IAU) approach. Their study shows promising results for the improved estimations of Arctic SIT by assimilating the latest breakthrough of satellite-retrieved SIT for summer in the Arctic.

Their work was published in the journal Ocean-Land-Atmosphere Research.

"To date, there are no studies focusing on the assimilation of satellite-based SIT observations during summer. In this study, we assimilate the latest biweekly summer SIT and daily sea ice concentration data from satellite observations into a coupled ice-ocean model to improve the model estimates," said Dr. Chao Min at Sun Yat-sen University, and Southern Marine Science and Engineering Guangdong Laboratory (Zhuhai), China; and the Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Germany.

Prior to this study, satellite-derived summer SIT had not been assimilated into numerical models since SIT observations were limited in summer. Recent progresses on SIT observations based on CryoSat-2, a satellite dedicated to the study of ice, have provided scientists with reliable year-round sea ice data. With CryoSat-2 summer SIT, the team delved into the proper approach to assimilate CryoSat-2 data. Their study marks the first successful instance in which satellite-based summer SIT data has been assimilated into a coupled ice-ocean model.

Directly assimilating the rather infrequent CryoSat-2 observations would introduce discontinuities in the development of sea ice volume and thickness estimates. The team overcame this challenge by implementing an incremental analysis update (IAU) approach in their data assimilation system. The IAU method provides a gradual development of the sea ice fields over time while allowing the assimilation of infrequent summer SIT data, which are only available on the biweekly basis, in conjunction with daily sea ice concentration data.

The team's efforts have led to improved estimates of Arctic SIT, which exhibit stronger correlations with independent SIT observations when compared to a sea ice reanalysis (CMST) that does not incorporate CryoSat-2 summer observations. By combining CryoSat-2 summer observations and model dynamics, the team obtained significant improvements in sea ice estimates.

They noted significant improvements in the SIT field in the areas where the sea ice is roughest and experiences strong deformation, such as around the Fram Strait and the northern coast of the Canadian Arctic Archipelago and Greenland.

... "A continuous long-term ice thickness record with a finer temporal-spatial resolution that assimilates both the year-round sea ice concentration and thickness will be reconstructed in the future. In addition, with the improved sea ice initial states, our data assimilation system has the potential to improve sea ice forecasts, particularly in summer," said Prof. Qinghua Yang, a professor at the School of Atmospheric Sciences, Sun Yat-sen University, and Southern Marine Science and Engineering Guangdong Laboratory (Zhuhai), China.

Chao Min et al, Improving Arctic sea-ice thickness estimates with the assimilation of CryoSat-2 summer observations, Ocean-Land-Atmosphere Research (2023)
https://spj.science.org/doi/10.34133/olar.0025
There are 3 classes of people: those who see. Those who see when they are shown. Those who do not see

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Glen Koehler

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Re: What's new in the Arctic ?
« Reply #883 on: November 29, 2023, 11:59:20 PM »



     The 2nd graph summarizes the 2023 melt-season quite well: cool start in May with reduced melt pond preconditioning.  Then a late summer catchup with heat in July and August.  The 2023 melt season was not as warm as the blistering summer of 2020 yet still went below the 2020 minimum Area.

     The high but not record-breaking temperature rankings for the 2012 melt-season months show that more than temperature is involved in driving the September Extent/Area/Volume measures.
« Last Edit: December 01, 2023, 10:43:20 AM by Glen Koehler »
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Glen Koehler

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Re: What's new in the Arctic ?
« Reply #884 on: December 12, 2023, 06:41:44 AM »
Excerpts from the "Sea Ice*" chapter in: State of the Cryosphere 2023.  Two Degrees Is Too High
© 2023 International Cryosphere Climate Initiative
https://iccinet.org/statecryo23/
"*In previous State of the Cryosphere reports, this chapter was actually titled “Arctic sea ice” and touched only briefly on Antarctic sea ice, because there was little to report: Antarctic sea ice extent had not fluctuated much despite global warming. However, the past two-three years – and 2023 in particular – has shown a striking shift also in the Antarctic sea ice response to warming; so this chapter is now re-titled “Sea Ice” and covers both."
 
     "... any Arctic sea ice recovery may take many decades, even with a subsequent return to lower atmospheric temperatures, because the water will hold that heat far longer. More open water, for longer periods may also absorb more carbon dioxide (CO2), increasing Arctic Ocean acidification rates"

"Preserved at 1.5°C: Studies consistently indicate that Arctic sea ice will still melt almost
completely some summers even at 1.5°C, but not each year and only for a brief period
(days to a few weeks) when it does."

"2023 Updates
• Arctic sea ice is more sensitive to greenhouse gas emissions than predicted by the IPCC AR6 report; and 90% of Arctic sea ice loss can be directly attributed to anthropogenic emissions."

     "Under current policies, the Arctic will experience ice-free summers in the 2030s, and the
length of time that the Arctic is ice-free will expand into August and October by 2080."

     "A typical sea ice floe now spends one-third less time in the Arctic Ocean compared to two decades ago."

     "Global warming has slowed the re-growth of Arctic sea ice in fall and winter following the melt season.  The frequency of atmospheric rivers – narrow corridors of warmer, moist air – has increased over the central Arctic, causing slower refreezing of the fragile ice attempting to recover after the summer melt season."

     "...the first ice-free summer will be an event that the Arctic likely has not experienced since at least the spike in warming that occurred at the end of the last ice age 8,000 years ago, and
possibly not since the warm Eemian period 125,000 years ago."

     "Like many impacts of climate change, Arctic sea ice loss over the past three decades has not occurred gradually, but rather in abrupt loss events when combinations of wind and warmer temperatures drove lower ice extents."

     "It is likely that a near-complete loss of summer sea ice (defined as dipping below 15% of the Arctic Ocean’s area, or 1 million km2) will occur with one of these sudden events, but perhaps not occur again for several years.  Eventually total-loss summers will become more frequent, and if temperatures continue to rise past a threshold of about 1.7°C, they will become the norm for some portion of each summer, with ice-free conditions ultimately extending into spring and autumn." (bolding added).

     "The occurrence of the first sea ice-free Arctic summer is therefore unpredictable, but  scientists now believe it is inevitable, and likely to occur at least once before 2050 even under a “very low” emissions scenario.  However, under both very low and low emissions scenarios, summer sea ice extent would likely stabilize, with occasional ice-free years, but remain generally above the threshold for ice-free conditions.  Greater amounts of sea ice may then form, slowly increasing as atmospheric temperatures decline below 1.5°C, but with multi-year ice nevertheless taking many decades to re-form due to a warmer Arctic Ocean.

     In contrast, continuing on the current emissions trajectory may lead to the Arctic becoming ice-free in the summer as soon as the 2030s.  Even moderate emissions will lead to ice-free conditions most summers once global mean temperature rise reaches about 1.7°C.  The length of
this ice-free state would increase in lock-step with emissions and temperature eventually stretching from July–October at 2°C.  The effects of amplifying feedbacks will be widespread, ranging from accelerated loss of ice and associated sea-level rise from Greenland; to losses of ice-dependent species; to greater permafrost  thaw, leading to even larger carbon emissions and infrastructure damage."

     "Given the greater absorption of solar heat into open water, it will lead to higher autumn
and winter temperatures in the Arctic that are expected to affect weather patterns around the Northern Hemisphere.  Unusual weather patterns likely will involve persistent conditions (drought, heatwaves, cold spells, or stormy periods),..."

     "The 2°C of global warming above pre-industrial levels that will cause summer ice-free conditions and allow exploitation of Arctic resources will also amplify the risks and societal disruptions noted elsewhere in this report, such as 6–20 meters committed long-term sea-level rise, fisheries loss from acidification, and extensive coastal damage from more intense storms and coastal permafrost thaw, including in the coastal Russian High North.  Such profound adverse impacts almost certainly will eclipse any temporary economic benefits brought by an ice-free summer Arctic."
   
     "Sea ice has served a cooling role in the climate system almost continuously for at least the past 125,000 years."

     "The former “ecosystem of ice” no longer exists."

     "The unprecedented reduction in Antarctic sea ice extent since 2016 represents a regime shift to a new state of inevitable decline caused by ocean warming."

(2 page discussion of Antarctic sea ice in the report)
« Last Edit: December 12, 2023, 10:55:52 PM by Glen Koehler »
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binntho

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Re: What's new in the Arctic ?
« Reply #885 on: December 30, 2023, 07:15:41 AM »
Stumbled across this paper in the American journal of Biological Anthropology. It is a very interesting discussion on the origin of the population of the Americas using dental morphological comparison. Of interest to this forum is the map below, which shows the state of the Bering Strait, Nares Strait and the CAA towards the end of the last glacial period. Sea levels were much lower than they are today, due to the massive continental glaciers that reached as far south as Northern Germany in Europe and the Great Lakes in the Americas. But at the same time, extensive areas in Northern Asia and possibly Alaska were free of glaciation, primarily due to lack of precipitation.

According to the current study, humans settled on the Arctic coast more than 20.000 years ago, during the height of the last glacial, and stayed there for at least 5000 years. Around 15.000 years ago they started moving south into both continents, coinciding neatly with the onset of significant warming during the Bølling-Allerød interstatial period (Late Glacial Interstadial in Wikipedia).

The paper can be downloaded from ResarchGate:

Scott, G. & Navega, David & Vlemincq-Mendieta, Tatiana & Dern, Laresa & O'Rourke, Dennis & Hlusko, Leslea & Hoffecker, John. (2023). Peopling of the Americas: A new approach to assessing dental morphological variation in Asian and Native American populations. American Journal of Biological Anthropology. 10.1002/ajpa.24878.
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binntho

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Re: What's new in the Arctic ?
« Reply #886 on: January 12, 2024, 07:03:18 AM »
An article in phys.org is very interesting. The article is named Chasing the light: Study finds new clues about warming in the Arctic and tells of research into changes in albedo over the Arctic ocean.

Being able to access radiometer data from GPS satellites, that give near constant full-time coverage, they find that while albedo decreased by 20-35%, sea ice coverage decreased by 7-9% over the same period (data from 2014-2019, looking at 40 days on either side of the summer solstice).

In other words - during a 5 year period, Albedo decreased significantly, and mostly because of changes to the surface of the ice and only one third of the decrease was because of ice being replaced by open water.

The paper itself is also available at nature.com. 
Broadband radiometric measurements from GPS satellites reveal summertime Arctic Ocean Albedo decreases more rapidly than sea ice recedes
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binntho

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Re: What's new in the Arctic ?
« Reply #887 on: January 16, 2024, 08:54:21 AM »
Last week I saw an article claiming that when average temperatures (not sure if it is annual or only winter months) rise above a threshold of -8C, annual snowcover decreases significantly. Unfortunately I was unable to find the article again, but I wonder if anybody else has seen this?
because a thing is eloquently expressed it should not be taken to be as necessarily true
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Glen Koehler

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Re: What's new in the Arctic ?
« Reply #888 on: January 16, 2024, 02:50:01 PM »
     From NY Times article on a recent study about decline in snow cover when average winter temperature goes above -8C (~17F):   
https://www.nytimes.com/2024/01/10/climate/climate-change-snowpack-decline.html#:~:text=Even%20as%20temperatures%20warm%2C%20places,Fahrenheit%2C%20the%20losses%20accelerate%20exponentially.

"The Northeast and Southwest of the United States are among the regions losing snowpack the fastest, along with much of Europe.

These changes haven’t been even or linear around the world. Even as temperatures warm, places that were colder to begin with may not exceed the freezing point of water (32 degrees Fahrenheit, or 0 degrees Celsius) enough during the winter to lose much snowpack.

But after an area hits a winter average of 17 degrees Fahrenheit, the losses accelerate exponentially.
"

     The source journal article is in Nature
Gottlieb, A.R., Mankin, J.S. Evidence of human influence on Northern Hemisphere snow loss. Nature 625, 293–300 (2024). https://doi.org/10.1038/s41586-023-06794-y https://www.nature.com/articles/s41586-023-06794-y
"Abstract
     Documenting the rate, magnitude and causes of snow loss is essential to benchmark the pace of climate change and to manage the differential water security risks of snowpack declines.  So far, however, observational uncertainties in snow mass have made the detection and attribution of human-forced snow losses elusive, undermining societal preparedness.  Here we show that human-caused warming has caused declines in Northern Hemisphere-scale March snowpack over the 1981–2020 period.  Using an ensemble of snowpack reconstructions, we identify robust snow trends in 82 out of 169 major Northern Hemisphere river basins, 31 of which we can confidently attribute to human influence.  Most crucially,  we show a generalizable and highly nonlinear temperature sensitivity of snowpack, in which snow becomes marginally more sensitive to one degree Celsius of warming as climatological winter temperatures exceed minus eight degrees Celsius.  Such nonlinearity explains the lack of widespread snow loss so far and augurs much sharper declines and water security risks in the most populous basins.  Together, our results emphasize that human-forced snow losses and their water consequences are attributable—even absent their clear detection in individual snow products—and will accelerate and homogenize with near-term warming, posing risks to water resources in the absence of substantial climate mitigation."
« Last Edit: January 16, 2024, 03:33:21 PM by Glen Koehler »
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binntho

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Re: What's new in the Arctic ?
« Reply #889 on: January 17, 2024, 07:27:19 AM »
Thanks Glen!
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gerontocrat

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Re: What's new in the Arctic ?
« Reply #890 on: January 19, 2024, 04:57:52 PM »
Maybe a SSW on the horizon? (We did have a minor one recently)
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El Cid

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Re: What's new in the Arctic ?
« Reply #891 on: January 19, 2024, 08:20:15 PM »
Not if you can believe the GFS forecast. It has the vortex back and running in about a week

vox_mundi

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Re: What's new in the Arctic ?
« Reply #892 on: January 20, 2024, 04:45:03 PM »
There are 3 classes of people: those who see. Those who see when they are shown. Those who do not see

Insensible before the wave so soon released by callous fate. Affected most, they understand the least, and understanding, when it comes, invariably arrives too late

Fiat iustitia, et pereat mundus

vox_mundi

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Re: What's new in the Arctic ?
« Reply #893 on: February 06, 2024, 02:35:56 PM »
Frequent Marine Heat Waves In the Arctic Ocean Will Be the Norm, Says New Study
https://phys.org/news/2024-02-frequent-marine-arctic-ocean-norm.html



Since 2007, conditions in the Arctic have shifted, as confirmed by data recently published in the journal Communications Earth & Environment. Between 2007 and 2021, the marginal zones of the Arctic Ocean experienced 11 marine heat waves, producing an average temperature rise of 2.2 degrees Celsius above seasonal norm and lasting an average of 37 days. Since 2015, there have been Arctic marine heat waves every year.

The most powerful heat wave to date in the Arctic Ocean was in 2020; it continued for 103 days, with peak temperatures that were four degrees Celsius over the long-term average. The probability of such a heat wave occurring without the influence of anthropogenic greenhouse gases is less than 1%, as calculated by Barkhordarian's team at the Cluster of Excellence CLICCS. By doing so, they have narrowed down the number of plausible climate scenarios in the Arctic. According to the study, annual marine heat waves will be the norm.

In the study, Barkhordarian also proves for the first time that heat waves are produced when sea ice melts early and rapidly after the winter. When this happens, considerable heat energy can accumulate in the water by the time maximum solar radiation is reached in July.

Officially, it is considered to be a marine heat wave when temperatures at the water's surface are higher than 95% of the values from the past 30 years for at least five consecutive days.

"Not just the constant loss of sea ice but also warmer waters can have dramatic negative effects on the Arctic ecosystem," says Barkhordarian. Food chains could collapse, fish stocks could be reduced, and overall biodiversity could decline

Arctic marine heatwaves forced by greenhouse gases and triggered by abrupt sea-ice melt, Communications Earth & Environment (2024)
https://dx.doi.org/10.1038/s43247-024-01215-y
There are 3 classes of people: those who see. Those who see when they are shown. Those who do not see

Insensible before the wave so soon released by callous fate. Affected most, they understand the least, and understanding, when it comes, invariably arrives too late

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vox_mundi

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Re: What's new in the Arctic ?
« Reply #894 on: February 10, 2024, 03:12:15 PM »
Melting Ice Roads Cut Off Indigenous Communities In Northern Canada
https://phys.org/news/2024-02-ice-roads-indigenous-communities-northern.html

Melting ice roads cut off Indigenous communities in Canada's far north as unseasonably warm weather on Friday also saw its largest city, Toronto, break a winter heat record.

Communities in Ontario and neighboring Manitoba provinces declared a state of emergency as the warm spell made the network of ice roads—which across Canada spans more than 8,000 kilometers (5,000 miles) between dispersed populations—unpassable.

Many remote communities in Canada's north depend on ice roads—compacted snow and ice atop frozen ground, lakes and rivers—for deliveries of essentials including fuel, equipment, non-perishable goods, as well as construction materials to build housing and infrastructure.

They allow trucks to reach areas in winter that are inaccessible at other times of the year.

"We're very concerned," Raymond Flett, chief of the Saint Theresa Point First Nation in northern Manitoba, told AFP.

The ice roads, he said, "are our lifeline. It's our only access."

The Nishnawbe Aski Nation said 30 Indigenous communities in northern Ontario were cut off and in desperate need of federal help.

"Winter temperatures have been significantly warmer than normal, exacerbated by the effects of climate change," it said in a statement, adding that many winter roads have become impassable for large loads and critical supplies.

Indigenous Services Minister Patricia Hajdu's office did not immediately reply to a request for comment.

Saint Theresa Point First Nation councilor Victor Walker warned that his community is "running out of supplies and fuel" and needs some 300 truckloads of gas, food and other essentials to get through the rest of the winter.

The community of about 5,000 people, he said, is considering flying in supplies but that comes with a hefty price tag that it can ill afford.

Environment Canada meteorologist Peter Kimbell said a cold blast could sweep across Manitoba and Ontario as early as next week.

He noted that winter warm spells are not unusual in Canada but "it is unusual to see this continued trend that we've seen all winter long."

Toronto on Friday broke a winter heat record as temperatures soared to 14.4 degrees Celsius (58 Fahrenheit). Its previous high was 10.6 degrees Celsius in 1938.

Several other cities in Ontario province were also flirting with new temperature highs including the nation's capital Ottawa.

Temperatures in December and January, he said, have been about four degrees Celsius warmer than normal and so far February appears to be moving in that direction too.
There are 3 classes of people: those who see. Those who see when they are shown. Those who do not see

Insensible before the wave so soon released by callous fate. Affected most, they understand the least, and understanding, when it comes, invariably arrives too late

Fiat iustitia, et pereat mundus

vox_mundi

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Re: What's new in the Arctic ?
« Reply #895 on: February 16, 2024, 07:58:10 PM »


From ESA/Copernicus
There are 3 classes of people: those who see. Those who see when they are shown. Those who do not see

Insensible before the wave so soon released by callous fate. Affected most, they understand the least, and understanding, when it comes, invariably arrives too late

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kassy

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Re: What's new in the Arctic ?
« Reply #896 on: February 20, 2024, 08:04:35 PM »
Long range weather forecast:

Frequent marine heatwaves in the Arctic Ocean will be the norm

Marine heatwaves will become a regular occurrence in the Arctic in the near future and are a product of higher anthropogenic greenhouse-gas emissions -- as shown in a study just released by Dr. Armineh Barkhordarian from Universität Hamburg's Cluster of Excellence for climate research CLICCS.

Since 2007, conditions in the Arctic have shifted, as confirmed by data recently published in the journal Nature Communications Earth & Environment. Between 2007 and 2021, the marginal zones of the Arctic Ocean experienced 11 marine heatwaves, producing an average temperature rise of 2.2 degrees Celsius above seasonal norm and lasting an average of 37 days.

Since 2015, there have been Arctic marine heatwaves every year.

The most powerful heatwave to date in the Arctic Ocean was in 2020; it continued for 103 days, with peak temperatures intensity that were four degrees Celsius over the long-term average.

The probability of such a heatwave occurring without the influence of anthropogenic greenhouse gases is less than one percent, as calculated by Barkhordarian's team at the Cluster of Excellence CLICCS.

...

In the study, Barkhordarian also proves for the first time that heatwaves are produced when sea ice melts early and rapidly after the winter.

When this happens, considerable heat energy can accumulate in the water by the time maximum solar radiation is reached in July.

"In 2007, a new phase began in the Arctic," says Barkhordarian, an expert on climate statistics.

"There is less and less of the thicker, several-year-old ice, while the percentage of thin, seasonal ice is consistently increasing." However, the thin ice is less durable and melts more quickly, allowing incoming solar radiation to warm the water's surface.

Officially, it is considered to be a marine heatwave when temperatures at the water's surface are higher than 95 percent of the values from the past 30 years for at least five consecutive days.

...

https://www.sciencedaily.com/releases/2024/02/240213130452.htm

oh and rain:

Rain Comes to the Arctic, With a Cascade of Troubling Changes

In August of 2021, rain fell atop the 10,551-foot summit of the Greenland ice cap, triggering an epic meltdown and a more-than-2,000-foot retreat of the snowline. The unprecedented event reminded Joel Harper, a University of Montana glaciologist who works on the Greenland ice sheet, of a strange anomaly in his data, one that suggested that in 2008 it might have rained much later in the season — in the fall, when the region is typically in deep freeze and dark for almost 24 hours a day.

When Harper and his colleagues closely examined the measurements they’d collected from sensors on the ice sheet those many years ago, they were astonished. Not only had it rained, but it had rained for four days as the air temperature rose by 30 degrees C (54 degrees F), close to and above the freezing point. It had warmed the summit’s firn layer — snow that is in transition to becoming ice — by between 11 and 42 degrees F (6 and 23 degrees C). The rainwater and surface melt that followed penetrated the firn by as much as 20 feet before refreezing, creating a barrier that would alter the flow of meltwater the following year.

...

Twenty years ago, annual precipitation in the Arctic ranged from about 10 inches in southern areas to as few as 2 inches or less in the far north. But as Arctic temperatures continue to warm three times faster than the planet as a whole, melting sea ice and more open water will, according to a recent study, bring up to 60 percent more precipitation in coming decades, with more rain falling than snow in many places.

Such changes will have a profound impact on sea ice, glaciers, and Greenland’s ice cap —

...

https://e360.yale.edu/features/arctic-rainfall-climate-change
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binntho

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Re: What's new in the Arctic ?
« Reply #897 on: March 12, 2024, 09:43:02 AM »
Trees are expanding north in Alaska’s Arctic as a result of sea ice loss

The causal chain seems to be: More open water leads to more moisture which causes more snowfall which helps protect young saplings during winter.

Increased snowfall is also insulating the ground and thus speeding up the melt of permafrost, helping the saplings to gain rootage.

And of course, tree cover lowers albedo significantly and has other effects that lead to milder climatic conditions.
because a thing is eloquently expressed it should not be taken to be as necessarily true
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KenB

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Re: What's new in the Arctic ?
« Reply #898 on: March 12, 2024, 04:42:31 PM »
Trees are expanding north in Alaska’s Arctic as a result of sea ice loss

...

Even without trees, working just with arctic shrubs, beavers are making inroads into the arctic.  Having trees around may accelerate this.  A-BON is the Arctic Beaver Observation Network:
 https://sites.google.com/alaska.edu/a-bon/
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vox_mundi

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Re: What's new in the Arctic ?
« Reply #899 on: March 21, 2024, 01:45:43 AM »
The Polar Vortex Is Spinning Backwards
https://www.climate.gov/news-features/blogs/polar-vortex/welcome-polar-vortex-blog

Earlier this month, atmospheric scientists noticed something unusual in the Arctic stratosphere. The polar vortex was spinning backward.

"The vortex changed direction around March 4th," reports Dr. Amy Butler, author of NOAA's Polar Vortex Blog. "It was a substantial reversal, reaching -20.5 m/s a few days ago, which puts it in the top 6 strongest such events since 1979."



Two weeks later, it is still spinning backwards. What's going on?

"Atmospheric planetary waves have been breaking in the polar stratosphere, increasing its temperature," says Butler. "We call this a 'Sudden Stratospheric Warming' event, and it can cause the vortex to change direction.'"

In recent years, many people have heard the phrase "polar vortex" because of the effect it can have on winter weather. When the polar vortex is strong and stable, it helps confine cold air to polar regions. When the vortex weakens or becomes disturbed, cold air spills out to lower latitudes.

This month's backward vortex has *not* caused an outbreak of winter weather. Instead, it has produced a very strong increase in polar ozone.



"Sudden Stratospheric Warming events accelerate the transport of ozone from the tropics to the poles," explains Butler. "Also, warming air helps prevent chemical ozone loss."

The current 'ozone spike' -- the opposite of an ozone hole -- is the biggest in the month of March since record-keeping began in 1979.

Soon, things could return to normal. The vortex's backward-spin is slowing, and "could become westerly again in about 10 days," says Butler. If so, the ozone spike will subside.

There are 3 classes of people: those who see. Those who see when they are shown. Those who do not see

Insensible before the wave so soon released by callous fate. Affected most, they understand the least, and understanding, when it comes, invariably arrives too late

Fiat iustitia, et pereat mundus