Seismic Impact of Large Earthquakes on Estimating Global Mean Ocean Mass Change from GRACE

We analyze the impact of large earthquakes on the estimation of the global mean ocean mass (GMOM) change rate over the 13-year period (January 2003 to December 2015) using the Gravity Recovery and Climate Experiment (GRACE) Release-06 (RL06) monthly gravity solutions released by the Center for Space...

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Main Authors: Lu Tang, Jin Li, Jianli Chen, Song-Yun Wang, Rui Wang, Xiaogong Hu
Format: Article
Language:English
Published: MDPI AG 2020-03-01
Series:Remote Sensing
Subjects:
Online Access:https://www.mdpi.com/2072-4292/12/6/935
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spelling doaj-d46841af477442069abbdc930089104d2020-11-25T01:29:02ZengMDPI AGRemote Sensing2072-42922020-03-0112693510.3390/rs12060935rs12060935Seismic Impact of Large Earthquakes on Estimating Global Mean Ocean Mass Change from GRACELu Tang0Jin Li1Jianli Chen2Song-Yun Wang3Rui Wang4Xiaogong Hu5School of Communication and Information Engineering, Shanghai University, Shanghai 200444, ChinaShanghai Astronomical Observatory, Chinese Academy of Sciences, Shanghai 200030, ChinaCenter for Space Research, University of Texas at Austin, TX 78759, USAShanghai Astronomical Observatory, Chinese Academy of Sciences, Shanghai 200030, ChinaSchool of Communication and Information Engineering, Shanghai University, Shanghai 200444, ChinaShanghai Astronomical Observatory, Chinese Academy of Sciences, Shanghai 200030, ChinaWe analyze the impact of large earthquakes on the estimation of the global mean ocean mass (GMOM) change rate over the 13-year period (January 2003 to December 2015) using the Gravity Recovery and Climate Experiment (GRACE) Release-06 (RL06) monthly gravity solutions released by the Center for Space Research (CSR). We take into account the effects of the December 2004 Mw9.1 and April 2012 Mw8.6 Sumatra earthquakes, the March 2011 Mw9.0 Tohoku-Oki earthquake, and the February 2010 Mw8.8 Chile earthquake. After removing the co- and post-seismic effects of these earthquakes in the oceanic areas by least squares fitting, we estimate the GMOM rate from GRACE monthly observations. Results show that GRACE-observed GMOM rate before the seismic correction is 2.12 ± 0.30 mm/year, while after correction the rate is 2.05 ± 0.30 mm/year. Even though the −0.07 ± 0.02 mm/year seismic influence on GRACE GMOM rate is small on a global scale, it is a systematic bias and should be considered for improved quantification and understanding of the global sea level change.https://www.mdpi.com/2072-4292/12/6/935graceglobal mean ocean mass changelarge earthquakesseismic deformation
collection DOAJ
language English
format Article
sources DOAJ
author Lu Tang
Jin Li
Jianli Chen
Song-Yun Wang
Rui Wang
Xiaogong Hu
spellingShingle Lu Tang
Jin Li
Jianli Chen
Song-Yun Wang
Rui Wang
Xiaogong Hu
Seismic Impact of Large Earthquakes on Estimating Global Mean Ocean Mass Change from GRACE
Remote Sensing
grace
global mean ocean mass change
large earthquakes
seismic deformation
author_facet Lu Tang
Jin Li
Jianli Chen
Song-Yun Wang
Rui Wang
Xiaogong Hu
author_sort Lu Tang
title Seismic Impact of Large Earthquakes on Estimating Global Mean Ocean Mass Change from GRACE
title_short Seismic Impact of Large Earthquakes on Estimating Global Mean Ocean Mass Change from GRACE
title_full Seismic Impact of Large Earthquakes on Estimating Global Mean Ocean Mass Change from GRACE
title_fullStr Seismic Impact of Large Earthquakes on Estimating Global Mean Ocean Mass Change from GRACE
title_full_unstemmed Seismic Impact of Large Earthquakes on Estimating Global Mean Ocean Mass Change from GRACE
title_sort seismic impact of large earthquakes on estimating global mean ocean mass change from grace
publisher MDPI AG
series Remote Sensing
issn 2072-4292
publishDate 2020-03-01
description We analyze the impact of large earthquakes on the estimation of the global mean ocean mass (GMOM) change rate over the 13-year period (January 2003 to December 2015) using the Gravity Recovery and Climate Experiment (GRACE) Release-06 (RL06) monthly gravity solutions released by the Center for Space Research (CSR). We take into account the effects of the December 2004 Mw9.1 and April 2012 Mw8.6 Sumatra earthquakes, the March 2011 Mw9.0 Tohoku-Oki earthquake, and the February 2010 Mw8.8 Chile earthquake. After removing the co- and post-seismic effects of these earthquakes in the oceanic areas by least squares fitting, we estimate the GMOM rate from GRACE monthly observations. Results show that GRACE-observed GMOM rate before the seismic correction is 2.12 ± 0.30 mm/year, while after correction the rate is 2.05 ± 0.30 mm/year. Even though the −0.07 ± 0.02 mm/year seismic influence on GRACE GMOM rate is small on a global scale, it is a systematic bias and should be considered for improved quantification and understanding of the global sea level change.
topic grace
global mean ocean mass change
large earthquakes
seismic deformation
url https://www.mdpi.com/2072-4292/12/6/935
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AT songyunwang seismicimpactoflargeearthquakesonestimatingglobalmeanoceanmasschangefromgrace
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