Below is a complete copy of a post by AbruptSLR, from which I quote
.....50–60% increase in Arctic precipitation over the 21st century. The additional precipitation is diagnosed to fall primarily as rain,..............But then again, Nebraska isn't in the Arctic.
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ps:
North America Snow Cover Extent back down to average (due to melt),
Eurasia Snow Cover Extent still going up strongly,
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https://forum.arctic-sea-ice.net/index.php/topic,2205.msg231856.html#msg231856Quote from: AbruptSLR on October 03, 2019, 10:55:10 PM
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Edit: I note that consensus models project that with continuing global warming, rainfall will increase in the Arctic in coming decades; which will not only impact: Arctic sea ice extent, potential release of excess freshwater from the Arctic Ocean, glacial ice, but also permafrost (which will not only increase CO2 emissions, but also methane emissions from thermal karst lakes).
Imagine what Bintanja (2018) would project if it had used a model with ECS greater than 5C:
R. Bintanja (2018), "The impact of Arctic warming on increased rainfall", Scientific Reports, 8, Article number: 16001, DOI:
https://doi.org/10.1038/s41598-018-34450-3https://www.nature.com/articles/s41598-018-34450-3Abstract: "The Arctic region is warming two to three times faster than the global mean, intensifying the hydrological cycle in the high north. Both enhanced regional evaporation and poleward moisture transport contribute to a 50–60% increase in Arctic precipitation over the 21st century. The additional precipitation is diagnosed to fall primarily as rain, but the physical and dynamical constraints governing the transition to a rain-dominated Arctic are unknown. Here we use actual precipitation, snowfall, rainfall output of 37 global climate models in standardised 21st-century simulations to demonstrate that, on average, the main contributor to additional Arctic (70–90°N) rainfall is local warming (~70%), whereas non-local (thermo)dynamical processes associated with precipitation changes contribute only 30%. Surprisingly, the effect of local warming peaks in the frigid high Arctic, where modest summer temperature changes exert a much larger effect on rainfall changes than strong wintertime warming. This counterintuitive seasonality exhibits steep geographical gradients, however, governed by non-linear changes in the temperature-dependent snowfall fraction, thereby obscuring regional-scale attribution of enhanced Arctic rainfall to climate warming. Detailed knowledge of the underlying causes behind Arctic snow/rainfall changes will contribute to more accurate assessments of the (possibly irreversible) impacts on hydrology/run-off, permafrost thawing, ecosystems, sea ice retreat, and glacier melt."