Quantifying the surface energy fluxes in South Greenland during the 2012 high melt episodes using in-situ observations

Frontiers in Earth Science

Dirk van As²  Robert S. Fausto²  Jason Eric Box²  Peter L. Langen³  William Colgan⁴ 

[1] Danish Meteorological Institute;Geological Survey of Denmark and Greenland (GEUS);University of Copenhagen;York University;

关键词: Surface mass balance;    In situ observation;    Automatic weather stations;    turbulent heat fluxes;    South Greenland melt;    Daily melt rates;   

DOI  :  10.3389/feart.2016.00082

来源: DOAJ

【 摘 要 】

Two high melt episodes occurred on the Greenland ice sheet in July 2012, during which nearly the entire ice sheet surface experienced melting. Observations from an automatic weather station (AWS) in the lower ablation area in South Greenland reveal the largest daily melt rates (up to 28 cm d-1 ice equivalent) ever recorded on the ice sheet. The two melt episodes lasted 6 days, equivalent to 6% of the June-August melt period, but contributed 14 % to the total annual ablation of 8.5 m ice equivalent. We employ a surface energy balance model driven by AWS data to quantify the relative importance of the energy budget components contributing to melt through the melt season. During the days with largest daily melt rates, surface turbulent heat input peaked at 552 Wm-2, 77 % of the surface melt energy, which is otherwise typically dominated by absorbed solar radiation. We find that rain contributed ca. 7 % to melt during these episodes.

【 授权许可】

Unknown