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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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 |
work_keys_str_mv |
AT lutang seismicimpactoflargeearthquakesonestimatingglobalmeanoceanmasschangefromgrace AT jinli seismicimpactoflargeearthquakesonestimatingglobalmeanoceanmasschangefromgrace AT jianlichen seismicimpactoflargeearthquakesonestimatingglobalmeanoceanmasschangefromgrace AT songyunwang seismicimpactoflargeearthquakesonestimatingglobalmeanoceanmasschangefromgrace AT ruiwang seismicimpactoflargeearthquakesonestimatingglobalmeanoceanmasschangefromgrace AT xiaogonghu seismicimpactoflargeearthquakesonestimatingglobalmeanoceanmasschangefromgrace |
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