2022
DOI: 10.1029/2022gl097899
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The Role of Atmospheric Blocking in Regulating Arctic Warming

Abstract: The near-surface warming in the Arctic is more than twice as fast as the global mean warming in recent decades. This phenomenon, known as Arctic amplification, is a key aspect of climate change (Cohen et al., 2014;Serreze et al., 2006Serreze et al., , 2009Serreze et al., , 2012. However, its exact mechanism is still under debate. A wide range of local and remote processes are considered modulators to Arctic Amplification. Examples of local processes are albedo feedback

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Cited by 14 publications
(10 citation statements)
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References 51 publications
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“…Increased winter warmth, as seen in 2020, reflects changes in circulation that draw more heat and moisture from lower latitudes ( 24 ). Circulation in eastern Siberia draws air and moisture from all directions of the compass ( 25 ) and is not immune to the so-called circulation “blocking” ( 26 ) seen elsewhere across the continent ( 27 ). Nonetheless, most burning occurs during relatively gentle winds blowing from the northeast, indicating that the processes that promote flammability may be distinct from those that promote the subsequent burning.…”
Section: Discussionmentioning
confidence: 99%
“…Increased winter warmth, as seen in 2020, reflects changes in circulation that draw more heat and moisture from lower latitudes ( 24 ). Circulation in eastern Siberia draws air and moisture from all directions of the compass ( 25 ) and is not immune to the so-called circulation “blocking” ( 26 ) seen elsewhere across the continent ( 27 ). Nonetheless, most burning occurs during relatively gentle winds blowing from the northeast, indicating that the processes that promote flammability may be distinct from those that promote the subsequent burning.…”
Section: Discussionmentioning
confidence: 99%
“…Increasing amount of water vapor in the atmosphere at the mid‐latitudes as the climate warms could partly explain this (Gershunov et al., 2017). For the Arctic, changes in circulation, with increasing frequency of blockings also drive the increase in moisture transport (Nygård et al., 2020; You et al., 2022), whereas in Antarctica, trends on the Amundsen Sea Low might explain AR trends in the Amundsen‐Bellinghausen Sea (Turner et al., 2013; Wille et al., 2021). Trends in AR activity across Antarctica are similar with previously observed trends, but are slightly sensitive to the choice of the reanalysis product used for AR detection (Wille et al., 2021).…”
Section: Resultsmentioning
confidence: 99%
“…Variations in the frequency of weather systems further contribute to the formation of extremes on a seasonal timescale (Hartmuth et al., 2022; Papritz, 2020), however their role for Arctic interannual temperature and precipitation variability in a changing climate has only received little attention so far. Several climate models project changes in Arctic weather system frequencies and characteristics such as their intensity and intensification in a warmer climate (Akperov et al., 2019; Rinke et al., 2017; You et al., 2022), with possibly large implications for future T and P variability. We show seasonal‐mean changes in weather system frequencies in CESM1 in Figure S7 in Supporting Information .…”
Section: Resultsmentioning
confidence: 99%