Linking scales of sea ice surface topography: evaluation of ICESat-2 measurements with coincident helicopter laser scanning during MOSAiC

被引:8
|
作者
Ricker, Robert [1 ]
Fons, Steven [2 ,3 ]
Jutila, Arttu [4 ]
Hutter, Nils [4 ,5 ]
Duncan, Kyle [6 ]
Farrell, Sinead L. [2 ,7 ]
Kurtz, Nathan T. [3 ]
Fredensborg Hansen, Renee Mie [8 ,9 ,10 ]
机构
[1] NORCE Norwegian Res Ctr, Tromso, Norway
[2] Univ Maryland, Dept Atmospher & Ocean Sci, College Pk, MD USA
[3] NASA Goddard Space Flight Ctr, Cryospher Sci Lab, Greenbelt, MD USA
[4] Helmholtz Ctr Polar & Marine Res, Alfred Wegener Inst, Bremerhaven, Germany
[5] Univ Washington, Cooperat Inst Climate Ocean & Ecosyst Studies, Seattle, WA USA
[6] Univ Maryland, Earth Syst Sci Interdisciplinary Ctr, College Pk, MD USA
[7] Univ Maryland, Dept Geog Sci, College Pk, MD USA
[8] DTU Space, Dept Geodesy & Earth Observat, Kongens Lyngby, Denmark
[9] NTNU, Dept Civil & Environm Engn, Trondheim, Norway
[10] Univ Ctr Svalbard UNIS, Arctic Geophys, Longyearbyen, Norway
来源
CRYOSPHERE | 2023年 / 17卷 / 03期
基金
美国国家航空航天局;
关键词
FREEBOARD; IMPACT;
D O I
10.5194/tc-17-1411-2023
中图分类号
P9 [自然地理学];
学科分类号
0705 ; 070501 ;
摘要
Information about sea ice surface topography and related deformation is crucial for studies of sea ice mass balance, sea ice modeling, and ship navigation through the ice pack. The Ice, Cloud, and land Elevation Satellite-2 (ICESat-2), part of the National Aeronautics and Space Administration (NASA) Earth Observing System, has been on orbit for over 4 years, sensing the sea ice surface topography with six laser beams capable of capturing individual features such as pressure ridges. To assess the capabilities and uncertainties of ICESat-2 products, coincident high-resolution measurements of sea ice surface topography are required. During the yearlong Multidisciplinary drifting Observatory for the Study of Arctic Climate (MOSAiC) expedition in the Arctic Ocean, we successfully carried out a coincident underflight of ICESat-2 with a helicopter-based airborne laser scanner (ALS), achieving an overlap of more than 100 km. Despite the comparably short data set, the high-resolution centimeter-scale measurements of the ALS can be used to evaluate the performance of ICESat-2 products. Our goal is to investigate how the sea ice surface roughness and topography are represented in different ICESat-2 products as well as how sensitive ICESat-2 products are to leads and small cracks in the ice cover. Here, we compare the ALS measurements with ICESat-2's primary sea ice height product, ATL07, and the high-fidelity surface elevation product developed by the University of Maryland (UMD). By applying a ridge-detection algorithm, we find that 16 % (4 %) of the number of obstacles in the ALS data set are found using the strong (weak) center beam in ATL07. Significantly higher detection rates of 42 % (30 %) are achieved when using the UMD product. While only one lead is indicated in ATL07 for the underflight, the ALS reveals many small, narrow, and only partly open cracks that appear to be overlooked by ATL07.
引用
收藏
页码:1411 / 1429
页数:19
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