TY - JOUR
T1 - Revisiting the Cause of the 1989–2009 Arctic Surface Warming Using the Surface Energy Budget
T2 - Downward Infrared Radiation Dominates the Surface Fluxes
AU - Lee, Sukyoung
AU - Gong, Tingting
AU - Feldstein, Steven B.
AU - Screen, James A.
AU - Simmonds, Ian
N1 - Publisher Copyright:
©2017. American Geophysical Union. All Rights Reserved.
PY - 2017/10/28
Y1 - 2017/10/28
N2 - The Arctic has been warming faster than elsewhere, especially during the cold season. According to the leading theory, ice-albedo feedback warms the Arctic Ocean during the summer, and the heat gained by the ocean is released during the winter, causing the cold-season warming. Screen and Simmonds (2010; SS10) concluded that the theory is correct by comparing trend patterns in surface air temperature (SAT), surface turbulence heat flux (HF), and net surface infrared radiation (IR). However, in this comparison, downward IR is more appropriate to use. By analyzing the same data used in SS10 using the surface energy budget, it is shown here that over most of the Arctic the skin temperature trend, which closely resembles the SAT trend, is largely accounted for by the downward IR, not the HF, trend.
AB - The Arctic has been warming faster than elsewhere, especially during the cold season. According to the leading theory, ice-albedo feedback warms the Arctic Ocean during the summer, and the heat gained by the ocean is released during the winter, causing the cold-season warming. Screen and Simmonds (2010; SS10) concluded that the theory is correct by comparing trend patterns in surface air temperature (SAT), surface turbulence heat flux (HF), and net surface infrared radiation (IR). However, in this comparison, downward IR is more appropriate to use. By analyzing the same data used in SS10 using the surface energy budget, it is shown here that over most of the Arctic the skin temperature trend, which closely resembles the SAT trend, is largely accounted for by the downward IR, not the HF, trend.
UR - https://www.scopus.com/pages/publications/85032303320
UR - https://www.scopus.com/pages/publications/85032303320#tab=citedBy
U2 - 10.1002/2017GL075375
DO - 10.1002/2017GL075375
M3 - Article
AN - SCOPUS:85032303320
SN - 0094-8276
VL - 44
SP - 10,654-10,661
JO - Geophysical Research Letters
JF - Geophysical Research Letters
IS - 20
ER -