气候变化领域集成服务门户(CCPortal): Representative surface snow density on the East Antarctic Plateau

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DOI	10.5194/tc-14-3663-2020
	Representative surface snow density on the East Antarctic Plateau
	Weinhart A.H.; Freitag J.; Hörhold M.; Kipfstuhl S.; Eisen O.
发表日期	2020
ISSN	19940416
起始页码	3663
结束页码	3685
卷号	14 期号:11
英文摘要	Surface mass balances of polar ice sheets are essential to estimate the contribution of ice sheets to sea level rise. Uncertain snow and firn densities lead to significant uncertainties in surface mass balances, especially in the interior regions of the ice sheets, such as the East Antarctic Plateau (EAP). Robust field measurements of surface snow density are sparse and challenging due to local noise. Here, we present a snow density dataset from an overland traverse in austral summer 2016/17 on the Dronning Maud Land plateau. The sampling strategy using 1m carbon fiber tubes covered various spatial scales, as well as a high-resolution study in a trench at 79° S, 30° E. The 1m snow density has been derived volumetrically, and vertical snow profiles have been measured using a core-scale microfocus X-ray computer tomograph. With an error of less than 2 %, our method provides higher precision than other sampling devices of smaller volume. With four spatially independent snow profiles per location, we reduce the local noise and derive a representative 1m snow density with an error of the mean of less than 1.5 %. Assessing sampling methods used in previous studies, we find the highest horizontal variability in density in the upper 0.3m and therefore recommend the 1m snow density as a robust measure of surface snow density in future studies. The average 1m snow density across the EAP is 355 kgm-3, which we identify as representative surface snow density between Kohnen Station and Dome Fuji. We cannot detect a temporal trend caused by the temperature increase over the last 2 decades. A difference of more than 10% to the density of 320 kgm-3 suggested by a semiempirical firn model for the same region indicates the necessity for further calibration of surface snow density parameterizations. Our data provide a solid baseline for tuning the surface snow density parameterizations for regions with low accumulation and low temperatures like the EAP. © Author(s) 2020.
英文关键词	glacier mass balance; ice sheet; measurement method; precision; sampling; sea level change; snow cover; tomography; uncertainty analysis; Antarctica; East Antarctica; Queen Maud Land
语种	英语
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/202244
作者单位	Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung, Bremerhaven, Germany; Physics of Ice, Climate and Earth, Niels Bohr Institute, University of Copenhagen, Copenhagen, Denmark; Fachbereich Geowissenschaften, Universität Bremen, Bremen, Germany
推荐引用方式 GB/T 7714	Weinhart A.H.,Freitag J.,Hörhold M.,et al. Representative surface snow density on the East Antarctic Plateau[J],2020,14(11).
APA	Weinhart A.H.,Freitag J.,Hörhold M.,Kipfstuhl S.,&Eisen O..(2020).Representative surface snow density on the East Antarctic Plateau.Cryosphere,14(11).
MLA	Weinhart A.H.,et al."Representative surface snow density on the East Antarctic Plateau".Cryosphere 14.11(2020).