共 50 条
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
相关论文
共 50 条