Extending the Arctic sea ice freeboard and sea level record with the Sentinel-3 radar altimeters

被引:16
|
作者
Lawrence, Isobel R. [1 ]
Armitage, Thomas W. K. [2 ]
Tsamados, Michel C. [1 ]
Stroeve, Julienne C. [1 ]
Dinardo, Salvatore [3 ]
Ridout, Andy L. [1 ]
Muir, Alan [1 ]
Tilling, Rachel L. [4 ]
Shepherd, Andrew [4 ]
机构
[1] UCL, Ctr Polar Observat & Modelling, Dept Earth Sci, London WC1E 6BS, England
[2] CALTECH, Jet Prop Lab, Pasadena, CA 91109 USA
[3] HeSpace, Robert Bosch Str 7, D-64293 Darmstadt, Germany
[4] Univ Leeds, Ctr Polar Observat & Modelling, Sch Earth & Environm, Leeds LS2 9JT, W Yorkshire, England
基金
美国国家航空航天局;
关键词
Sea ice; Radar altimetry; CryoSat-2; Sentinel-3; Sea-level anomaly; Radar freeboard; CRYOSAT-2; ENVISAT; VARIABILITY; THICKNESS; RETRIEVAL; MISSION;
D O I
10.1016/j.asr.2019.10.011
中图分类号
V [航空、航天];
学科分类号
08 ; 0825 ;
摘要
In February 2016 and April 2018 the European Space Agency launched the Sentinel-3A and 3B satellites respectively, as part of the European Commission's multi-satellite Copernicus Programme. Here we process Sentinel-3A waveform data to estimate Arctic sea level anomaly and radar freeboard from November 2017 to April 2018. We compare our results to those from the CryoSat-2 satellite, and find an intermission bias on sea-level anomaly of 2 cm. We also find a mean radar freeboard difference of 1 cm, which we attribute to the use of empirical retrackers to retrieve lead and floe elevations. Ahead of Sentinel-3B waveform data being made available, we use orbit files to estimate the improvement in sampling resolution afforded by the addition of Sentinel-3A and 3B data to the CryoSat-2 dataset. By combining data from the three satellites, grid resolution or time-sampling can be almost tripled compared with using CryoSat-2 data alone. (C) 2019 COSPAR. Published by Elsevier Ltd. All rights reserved.
引用
收藏
页码:711 / 723
页数:13
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