气候变化领域集成服务门户(CCPortal): Brief communication: Improved simulation of the present-day Greenland firn layer (1960-2016)

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DOI	10.5194/tc-12-1643-2018
	Brief communication: Improved simulation of the present-day Greenland firn layer (1960-2016)
	Ligtenberg S.R.M.; Munneke P.K.; Noël B.P.Y.; Van Den Broeke M.R.
发表日期	2018
ISSN	19940416
卷号	12 期号:5
英文摘要	By providing pore space for storage or refreezing of meltwater, the Greenland ice sheet firn layer strongly modulates runoff. Correctly representing the firn layer is therefore crucial for Greenland (surface) mass balance studies. Here, we present a simulation of the Greenland firn layer with the firn model IMAU-FDM forced by the latest output of the regional climate model RACMO2, version 2.3p2. In the percolation zone, much improved agreement is found with firn density and temperature observations. A full simulation of Greenland firn at high temporal (10 days) and spatial (11 km) resolution is available for the period 1960-2016. © Author(s) 2018. This work is distributed under the Creative Commons Attribution 4.0 License.
学科领域	climate modeling; density; firn; mass balance; model; regional climate; runoff; simulation; temperature; Arctic; Greenland; Greenland Ice Sheet
语种	英语
scopus关键词	climate modeling; density; firn; mass balance; model; regional climate; runoff; simulation; temperature; Arctic; Greenland; Greenland Ice Sheet
来源期刊	Cryosphere
文献类型	期刊论文
条目标识符	http://gcip.llas.ac.cn/handle/2XKMVOVA/119152
作者单位	Institute for Marine and Atmospheric Research Utrecht (IMAU), Utrecht University, Utrecht, Netherlands
推荐引用方式 GB/T 7714	Ligtenberg S.R.M.,Munneke P.K.,Noël B.P.Y.,et al. Brief communication: Improved simulation of the present-day Greenland firn layer (1960-2016)[J],2018,12(5).
APA	Ligtenberg S.R.M.,Munneke P.K.,Noël B.P.Y.,&Van Den Broeke M.R..(2018).Brief communication: Improved simulation of the present-day Greenland firn layer (1960-2016).Cryosphere,12(5).
MLA	Ligtenberg S.R.M.,et al."Brief communication: Improved simulation of the present-day Greenland firn layer (1960-2016)".Cryosphere 12.5(2018).