The Role of the Tropically Excited Arctic Warming Mechanism on the Warm Arctic Cold Continent Surface Air Temperature Trend Pattern

Abstract The December–February surface air temperature (SAT) trend is examined for all consecutive 20‐year time periods between 1979 and 2017, from which a transition from a cold‐Arctic‐warm‐continent toward a warm‐Arctic‐cold‐continent trend pattern is evident. This transition is accompanied by a c...

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Main Authors: Joseph P. Clark, Sukyoung Lee
Format: Article
Language:English
Published: Wiley 2019-07-01
Series:Geophysical Research Letters
Online Access:https://doi.org/10.1029/2019GL082714
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author Joseph P. Clark
Sukyoung Lee
author_facet Joseph P. Clark
Sukyoung Lee
author_sort Joseph P. Clark
collection DOAJ
description Abstract The December–February surface air temperature (SAT) trend is examined for all consecutive 20‐year time periods between 1979 and 2017, from which a transition from a cold‐Arctic‐warm‐continent toward a warm‐Arctic‐cold‐continent trend pattern is evident. This transition is accompanied by a consistent transition in the sea level pressure trend pattern that supports warm air advection over the Arctic and cold air advection over the continents. The regression of the detrended December–February‐average SAT onto a detrended index defined to quantify the east‐west gradient of tropical Pacific sea surface temperature is characterized by a warm‐Arctic‐cold‐continent pattern much like the SAT trend pattern observed in recent decades. A decadal timescale warming of the western tropical Pacific water has increased the east‐west gradient of tropical Pacific sea surface temperature, thus contributing to the observed extratropical SAT trend transition.
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series Geophysical Research Letters
spelling doaj-art-e80a88f1aeed437ab9b0dd2e1397e1e62025-08-20T03:44:57ZengWileyGeophysical Research Letters0094-82761944-80072019-07-0146148490849910.1029/2019GL082714The Role of the Tropically Excited Arctic Warming Mechanism on the Warm Arctic Cold Continent Surface Air Temperature Trend PatternJoseph P. Clark0Sukyoung Lee1Department of Meteorology and Atmospheric Science The Pennsylvania State University University Park PA USADepartment of Meteorology and Atmospheric Science The Pennsylvania State University University Park PA USAAbstract The December–February surface air temperature (SAT) trend is examined for all consecutive 20‐year time periods between 1979 and 2017, from which a transition from a cold‐Arctic‐warm‐continent toward a warm‐Arctic‐cold‐continent trend pattern is evident. This transition is accompanied by a consistent transition in the sea level pressure trend pattern that supports warm air advection over the Arctic and cold air advection over the continents. The regression of the detrended December–February‐average SAT onto a detrended index defined to quantify the east‐west gradient of tropical Pacific sea surface temperature is characterized by a warm‐Arctic‐cold‐continent pattern much like the SAT trend pattern observed in recent decades. A decadal timescale warming of the western tropical Pacific water has increased the east‐west gradient of tropical Pacific sea surface temperature, thus contributing to the observed extratropical SAT trend transition.https://doi.org/10.1029/2019GL082714
spellingShingle Joseph P. Clark
Sukyoung Lee
The Role of the Tropically Excited Arctic Warming Mechanism on the Warm Arctic Cold Continent Surface Air Temperature Trend Pattern
Geophysical Research Letters
title The Role of the Tropically Excited Arctic Warming Mechanism on the Warm Arctic Cold Continent Surface Air Temperature Trend Pattern
title_full The Role of the Tropically Excited Arctic Warming Mechanism on the Warm Arctic Cold Continent Surface Air Temperature Trend Pattern
title_fullStr The Role of the Tropically Excited Arctic Warming Mechanism on the Warm Arctic Cold Continent Surface Air Temperature Trend Pattern
title_full_unstemmed The Role of the Tropically Excited Arctic Warming Mechanism on the Warm Arctic Cold Continent Surface Air Temperature Trend Pattern
title_short The Role of the Tropically Excited Arctic Warming Mechanism on the Warm Arctic Cold Continent Surface Air Temperature Trend Pattern
title_sort role of the tropically excited arctic warming mechanism on the warm arctic cold continent surface air temperature trend pattern
url https://doi.org/10.1029/2019GL082714
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