使用测高法从欧洲遥感卫星(ERS-2)获取北极海冰雷达干舷:面向1995年至2021年的海冰厚度观测

IF 4.4 2区 地球科学 Q1 GEOGRAPHY, PHYSICAL
Cryosphere Pub Date : 2023-07-25 DOI:10.5194/tc-17-3013-2023
M. Bocquet, S. Fleury, F. Piras, E. Rinne, Heidi Sallila, F. Garnier, F. Rémy
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引用次数: 1

摘要

摘要海冰量的显著年际变化需要长期的一系列观测来确定其演变趋势。尽管在过去几年中,由于CryoSat-2和ICESat-2,通过测高技术估算海冰厚度有所改善,但欧洲航天局以前的雷达测高任务,如环境卫星(Envisat),特别是欧洲遥感卫星(ERS-1和ERS-2),到目前为止仍未得到充分利用。虽然已经提出了解决方案,以确保CryoSat-2和Envisat之间测量的连续性,但没有时间序列集成ERS。本研究的目的是将北极雷达干舷时间序列延后至1995年。处理ERS测量的困难来自于一个被称为脉冲模糊效应的技术问题,它会改变海冰上的雷达回波和由此产生的地表高度估计值。在这里,我们提出并应用这种脉冲模糊效果的校正。为了确保CryoSat-2、Envisat和ERS-2时间序列的一致性,提出了一种基于多参数神经网络的方法来校准Envisat与CryoSat-2和ERS-2与Envisat的对比。校准是根据在任务重叠期间高度计测量值与表征海冰状态的一组参数之间观察到的差异进行训练的。每月雷达干舷提供基于蒙特卡罗方法的不确定性估计,将不确定性沿处理链传播,包括神经网络。在重叠期间对校正后的雷达干深进行比较,结果显示两项任务之间存在良好的一致性,Envisat和CryoSat-2的平均偏差为0.30 cm,标准差为9.7 cm, ERS-2和Envisat的偏差为0.20 cm,标准差为3.8 cm。从Envisat和ERS-2获得的每月校正雷达干舷,然后通过与几个独立数据集(如机载、系泊、直接测量和其他高度计产品)进行比较来验证。除了两个数据集外,比较结果显示Envisat的相关性为0.41至0.94,ERS-2的相关性为0.60至0.74。该研究最后提供了1995年至2021年冬季(从ERS-2任务到CryoSat-2)的雷达干舷估计。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Arctic sea ice radar freeboard retrieval from the European Remote-Sensing Satellite (ERS-2) using altimetry: toward sea ice thickness observation from 1995 to 2021
Abstract. Sea ice volume's significant interannual variability requires long-term series of observations to identify trends in its evolution. Despite improvements in sea ice thickness estimations from altimetry during the past few years thanks to CryoSat-2 and ICESat-2, former ESA radar altimetry missions such as the Environmental Satellite (Envisat) and especially the European Remote-Sensing Satellite (ERS-1 and ERS-2) have remained under-exploited so far. Although solutions have already been proposed to ensure continuity of measurements between CryoSat-2 and Envisat, there is no time series integrating ERS. The purpose of this study is to extend the Arctic radar freeboard time series back to 1995. The difficulty in handling ERS measurements comes from a technical issue known as the pulse blurring effect, altering the radar echoes over sea ice and the resulting surface height estimates. Here we present and apply a correction for this pulse blurring effect. To ensure consistency of the CryoSat-2, Envisat and ERS-2 time series, a multiparameter neural-network-based method to calibrate Envisat against CryoSat-2 and ERS-2 against Envisat is presented. The calibration is trained on the discrepancies observed between the altimeter measurements during the mission-overlap periods and a set of parameters characterizing the sea ice state. Monthly radar freeboards are provided with uncertainty estimations based on a Monte Carlo approach to propagate the uncertainties all along the processing chain, including the neural network. Comparisons of corrected radar freeboards during overlap periods reveal good agreement between the missions, with a mean bias of 0.30 cm and a standard deviation of 9.7 cm for Envisat and CryoSat-2 and a 0.20 cm bias and a standard deviation of 3.8 cm for ERS-2 and Envisat. The monthly corrected radar freeboards obtained from Envisat and ERS-2 are then validated by comparison with several independent datasets such as airborne, mooring, direct-measurement and other altimeter products. Except for two datasets, comparisons lead to correlations ranging from 0.41 to 0.94 for Envisat and from 0.60 to 0.74 for ERS-2. The study finally provides radar freeboard estimation for winters from 1995 to 2021 (from the ERS-2 mission to CryoSat-2).
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来源期刊
Cryosphere
Cryosphere GEOGRAPHY, PHYSICAL-GEOSCIENCES, MULTIDISCIPLINARY
CiteScore
8.70
自引率
17.30%
发文量
240
审稿时长
4-8 weeks
期刊介绍: The Cryosphere (TC) is a not-for-profit international scientific journal dedicated to the publication and discussion of research articles, short communications, and review papers on all aspects of frozen water and ground on Earth and on other planetary bodies. The main subject areas are the following: ice sheets and glaciers; planetary ice bodies; permafrost and seasonally frozen ground; seasonal snow cover; sea ice; river and lake ice; remote sensing, numerical modelling, in situ and laboratory studies of the above and including studies of the interaction of the cryosphere with the rest of the climate system.
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