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- W4364374619 abstract "Abstract We investigated the interannual variations in the annual mean and seasonal cycle of upward shortwave radiation at the top of the atmosphere (TOA SW ↑ ) over the Arctic using the Clouds and the Earth’s Radiant Energy System (CERES) observation data during 2001–20. The annual mean TOA SW ↑ over the Arctic showed a decreasing trend from 2001 to 2012 (−2.5 W m −2 decade −1 ) and had a large interannual variability after 2012. The standard deviation of detrended TOA SW ↑ increased from 0.4 W m −2 in 2001–12 to 1.1 W m −2 in 2012–20. Over land, TOA SW ↑ variation was related to snow cover in May; snow cover, cloud fraction, and cloud optical depth (COD) in June; and cloud fraction and COD in July. Over ocean, TOA SW ↑ variation in June and July was linked to sea ice cover. TOA SW ↑ variation over ocean in June and July after 2012 was highly related to the North Atlantic Oscillation (NAO). This study suggests that changes in the large annual mean TOA SW ↑ variability after 2012 are explained by the timing of land snow and sea ice melt in spring and summer and cloud variability over land in summer." @default.
- W4364374619 created "2023-04-12" @default.
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- W4364374619 date "2023-08-01" @default.
- W4364374619 modified "2023-10-18" @default.
- W4364374619 title "Interannual Variation in Top-of-Atmosphere Upward Shortwave Flux over the Arctic Related to Sea Ice, Snow Cover, and Land Cloud Cover in Spring and Summer" @default.
- W4364374619 doi "https://doi.org/10.1175/jcli-d-22-0440.1" @default.
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