Global S&T Development Trend Analysis Platform of Resources and Environment
DOI | 10.1175/JCLI-D-17-0447.1 |
Greenland Ice Sheet Surface Melt and Its Relation to Daily Atmospheric Conditions | |
Cullather, Richard I.1,2; Nowicki, Sophie M. J.3 | |
2018-03-01 | |
发表期刊 | JOURNAL OF CLIMATE
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ISSN | 0894-8755 |
EISSN | 1520-0442 |
出版年 | 2018 |
卷号 | 31期号:5页码:1897-1919 |
文章类型 | Article |
语种 | 英语 |
国家 | USA |
英文摘要 | Melt area is one of the most reliably monitored variables associated with surface conditions over the full Greenland Ice Sheet (GrIS). Surface melt is also an important indicator of surface mass balance and has potential relevance to the ice sheet's global sea level contribution. Melt events are known to be spatially heterogeneous and have varying time scales. To understand the forcing mechanisms, it is necessary to examine the relation between the existing conditions and melt area on the time scales that melt is observed. Here, the authors conduct a regression analysis of atmospheric reanalysis variables including sea level pressure, near-surface winds, and components of the surface energy budget with surface melt. The regression analysis finds spatial heterogeneity in the associated atmospheric circulation conditions. For basins in the southern GrIS, there is an association between melt area and high pressure located south of the Denmark Strait, which allows for southerly flow over the western half of the GrIS. Instantaneous surface melt over northern basins is also associated with low pressure over the central Arctic. Basins associated with persistent summer melt in the southern and western GrIS are associated with the presence of an enhanced cloud cover, a resulting decreased downwelling solar radiative flux, and an enhanced downwelling long wave radiative flux. This contrasts with basins to the north and east, where an increased downwelling solar radiative flux plays a more important role in the onset of a melt event. The analysis emphasizes the importance of daily variability in synoptic conditions and their preferred association with melt events. |
领域 | 气候变化 |
收录类别 | SCI-E |
WOS记录号 | WOS:000427438100013 |
WOS关键词 | REGIONAL CLIMATE MODEL ; MASS-BALANCE ; TEMPERATURE ; VARIABILITY ; REANALYSIS ; CLOUDS ; BLOCKING ; DRIVERS ; TRENDS ; COVER |
WOS类目 | Meteorology & Atmospheric Sciences |
WOS研究方向 | Meteorology & Atmospheric Sciences |
引用统计 | |
文献类型 | 期刊论文 |
条目标识符 | http://119.78.100.173/C666/handle/2XK7JSWQ/20532 |
专题 | 气候变化 |
作者单位 | 1.Univ Maryland, Earth Syst Sci Interdisciplinary Ctr, College Pk, MD 20742 USA; 2.NASA, Global Modeling & Assimilat Off, Goddard Space Flight Ctr, Greenbelt, MD 20771 USA; 3.NASA, Cryospher Sci Lab, Goddard Space Flight Ctr, Greenbelt, MD USA |
推荐引用方式 GB/T 7714 | Cullather, Richard I.,Nowicki, Sophie M. J.. Greenland Ice Sheet Surface Melt and Its Relation to Daily Atmospheric Conditions[J]. JOURNAL OF CLIMATE,2018,31(5):1897-1919. |
APA | Cullather, Richard I.,&Nowicki, Sophie M. J..(2018).Greenland Ice Sheet Surface Melt and Its Relation to Daily Atmospheric Conditions.JOURNAL OF CLIMATE,31(5),1897-1919. |
MLA | Cullather, Richard I.,et al."Greenland Ice Sheet Surface Melt and Its Relation to Daily Atmospheric Conditions".JOURNAL OF CLIMATE 31.5(2018):1897-1919. |
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