General
Image
Manipulation
Program. Unfortunate acronym but still makes for a good search term in conjunction with a tutorial topic or mission-critical plugin. ImageJ is far easier to use if just looking for a gif frame or montage viewing tool.
Here is a more uptodate treatment of sea level rise from global (Arctic not tabulated) ice volumes as well. The 2014 article has been cited 364 times, the place to look for 2017-18 updates (see below).
Sea level and global ice volumes from the Last Glacial Maximum to the Holocene
K Lambecka et al
http://www.pnas.org/content/111/43/15296.full.pdf open source
The major cause of sea-level change during ice ages is the exchange of water between ice and ocean and the planet’s dynamic response to the changing surface load. Inversion of ∼1,000 observations for the past 35,000 yr from localities far from former ice margins has provided new constraints on the fluctuation of ice volume in this interval. Key results are:
(i) a rapid final fall in global sea level of ∼40 m in <2,000 y at the onset of the glacial maximum ∼30,000 y before present (30 ka BP)
(ii) a slow fall to −134 m from 29 to 21 ka BP with a maximum grounded ice volume of ∼52 × 106 km3 greater than today
(iii) after an initial short duration rapid rise and a short interval of near-constant sea level, the main phase of deglaciation occurred from ∼16.5 ka BP to ∼8.2 ka BP at an average rate of rise of 12 m·ka−1 punctuated by periods of greater, particularly at 14.5– 14.0 ka BP at ≥40 mm·y−1 (MWP-1A), and lesser, from 12.5 to 11.5 ka BP (Younger Dryas), rates
(iv) no evidence for a global MWP-1B event at ∼11.3 ka BP
(v) a progressive decrease in the rate of rise from 8.2 ka to ∼2.5 ka BP, after which ocean volumes
remained nearly constant until the renewed sea-level rise at 100–150 y ago, with no evidence of oscillations exceeding ∼15–20 cm in time intervals ≥200 y from 6 to 0.15 ka BP
Oceanographic and Climatic Change in the Bering Sea, Last Glacial Maximum to Holocene
BM Pelto, BE Caissie, ST Petsch
Paleoceanography 2018
Post-glacial sea level rise led to a direct connection between the Arctic and Pacific
Oceans via the Bering Strait. Consequently, the Bering Sea experienced changes in
connectivity, size and sediment sources that were among the most drastic of any ocean...
The De Long Trough: a newly discovered glacial trough on the East Siberian continental margin
M O'Regan et al
Climate of the Past 2017
Ice sheets extending over parts of the East Siberian continental shelf have been
proposed for the last glacial period and during the larger Pleistocene glaciations. The
sparse data available over this sector of the Arctic Ocean have left the timing, extent and ...
Deglacial sea level history of the East Siberian Sea and Chukchi Sea margins
TM Cronin et al
Climate of the Past 2017
Deglacial (12.8–10.7 ka) sea level history on the East Siberian continental shelf
and upper continental slope was reconstructed using new geophysical records and
sediment cores taken during Leg 2 of the 2014 SWERUS-C3 expedition.
Younger-Dryas cooling and sea-ice feedbacks were prominent features of the Pleistocene-Holocene transition in Arctic Alaska
BV Gaglioti et al
Quaternary Science 2017
Declining sea-ice extent is currently amplifying climate warming in the Arctic.
Instrumental records at high latitudes are too short-term to provide sufficient historical
context for these trends, so paleoclimate archives are needed to better understand the...
Post-glacial flooding of the Bering Land Bridge dated to 11 cal ka BP based on new geophysical and sediment records
M Jakobsson et al
The Bering Strait connects the Arctic and Pacific oceans and separates the North
American and Asian landmasses. The presently shallow (∼ 53 m) strait was exposed during
the sea level lowstand of the last glacial period, which permitted human migration across ...
Deglaciation of the Laurentide Ice Sheet from the Last Glacial Maximum.
CR Stokes 2017 - dro.dur.ac.uk
The last deglaciation of the Laurentide Ice Sheet (LIS) was associated with major
reorganisations in the ocean-climate system and its retreat also represents a valuable
analogue for understanding the rates and mechanisms of ice sheet collapse...
Caribbean Reef Drowning During Slow Mid-Holocene Sea-Level Rise
P Blanchon et al 2017 osf.io
Predicting if reefs can keep pace with future sea-level (SL) rise is problematic
because accretion occurs over geological timescales. For example, although meltwater
pulses drowned reefs during postglacial SL rise, drowning has also been reported during...