Mass-induced sea level change in the northwestern North Pacific and its contribution to total sea level change
Over the period 2003–2011, the Gravity Recovery and Climate Experiment (GRACE) satellite pair revealed a remarkable variability in mass‐induced sea surface height (MSSH) in the northwestern North Pacific. A significant correlation is found between MSSH and observed total sea surface height (SSH), in...
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| Published in | Geophysical research letters Vol. 40; no. 15; pp. 3975 - 3980 |
|---|---|
| Main Authors | , , , , |
| Format | Journal Article |
| Language | English |
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Washington
Blackwell Publishing Ltd
16.08.2013
John Wiley & Sons, Inc |
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| Abstract | Over the period 2003–2011, the Gravity Recovery and Climate Experiment (GRACE) satellite pair revealed a remarkable variability in mass‐induced sea surface height (MSSH) in the northwestern North Pacific. A significant correlation is found between MSSH and observed total sea surface height (SSH), indicative of the importance of barotropic variability in this region. For the period 2003–2011, MSSH rose at a rate of 6.1 ± 0.7 mm/yr, which has a significant contribution to the SSH rise (8.3 ± 0.7 mm/yr). Analysis of the barotropic vorticity equation based on National Centers for Environmental Prediction/National Center for Atmospheric Research reanalysis product, GRACE, and altimetry data suggests that the MSSH signal is primarily caused by negative wind stress curl associated with an anomalous anticyclonic atmospheric circulation. Regression analysis indicates that trends in MSSH and surface wind are related to the Pacific Decadal Oscillation, whose index had a decreasing trend in the last decade.
Key Points
Remarkable variability in MSSH is found in the northwestern North Pacific
For the period 2003‐2011, MSSH has significant contribution to the SSH rise
Trends in MSSH and surface wind are related to the Pacific Decadal Oscillation |
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| AbstractList | Over the period 2003-2011, the Gravity Recovery and Climate Experiment (GRACE) satellite pair revealed a remarkable variability in mass-induced sea surface height (MSSH) in the northwestern North Pacific. A significant correlation is found between MSSH and observed total sea surface height (SSH), indicative of the importance of barotropic variability in this region. For the period 2003-2011, MSSH rose at a rate of 6.1 plus or minus 0.7mm/yr, which has a significant contribution to the SSH rise (8.3 plus or minus 0.7mm/yr). Analysis of the barotropic vorticity equation based on National Centers for Environmental Prediction/National Center for Atmospheric Research reanalysis product, GRACE, and altimetry data suggests that the MSSH signal is primarily caused by negative wind stress curl associated with an anomalous anticyclonic atmospheric circulation. Regression analysis indicates that trends in MSSH and surface wind are related to the Pacific Decadal Oscillation, whose index had a decreasing trend in the last decade. Key Points * Remarkable variability in MSSH is found in the northwestern North Pacific * For the period 2003-2011, MSSH has significant contribution to the SSH rise * Trends in MSSH and surface wind are related to the Pacific Decadal Oscillation Over the period 2003–2011, the Gravity Recovery and Climate Experiment (GRACE) satellite pair revealed a remarkable variability in mass‐induced sea surface height (MSSH) in the northwestern North Pacific. A significant correlation is found between MSSH and observed total sea surface height (SSH), indicative of the importance of barotropic variability in this region. For the period 2003–2011, MSSH rose at a rate of 6.1 ± 0.7 mm/yr, which has a significant contribution to the SSH rise (8.3 ± 0.7 mm/yr). Analysis of the barotropic vorticity equation based on National Centers for Environmental Prediction/National Center for Atmospheric Research reanalysis product, GRACE, and altimetry data suggests that the MSSH signal is primarily caused by negative wind stress curl associated with an anomalous anticyclonic atmospheric circulation. Regression analysis indicates that trends in MSSH and surface wind are related to the Pacific Decadal Oscillation, whose index had a decreasing trend in the last decade. Key Points Remarkable variability in MSSH is found in the northwestern North Pacific For the period 2003‐2011, MSSH has significant contribution to the SSH rise Trends in MSSH and surface wind are related to the Pacific Decadal Oscillation Over the period 2003-2011, the Gravity Recovery and Climate Experiment (GRACE) satellite pair revealed a remarkable variability in mass-induced sea surface height (MSSH) in the northwestern North Pacific. A significant correlation is found between MSSH and observed total sea surface height (SSH), indicative of the importance of barotropic variability in this region. For the period 2003-2011, MSSH rose at a rate of 6.1±0.7mm/yr, which has a significant contribution to the SSH rise (8.3±0.7mm/yr). Analysis of the barotropic vorticity equation based on National Centers for Environmental Prediction/National Center for Atmospheric Research reanalysis product, GRACE, and altimetry data suggests that the MSSH signal is primarily caused by negative wind stress curl associated with an anomalous anticyclonic atmospheric circulation. Regression analysis indicates that trends in MSSH and surface wind are related to the Pacific Decadal Oscillation, whose index had a decreasing trend in the last decade. |
| Author | Li, Lijuan Huang, Rui-Xin Du, Yan Wang, Jing Cheng, Xuhua |
| Author_xml | – sequence: 1 givenname: Xuhua surname: Cheng fullname: Cheng, Xuhua email: xuhuacheng@scsio.ac.cn organization: State Key Laboratory of Tropical Oceanography, South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou, China – sequence: 2 givenname: Lijuan surname: Li fullname: Li, Lijuan organization: State Key Laboratory of Tropical Oceanography, South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou, China – sequence: 3 givenname: Yan surname: Du fullname: Du, Yan organization: State Key Laboratory of Tropical Oceanography, South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou, China – sequence: 4 givenname: Jing surname: Wang fullname: Wang, Jing organization: School of Geography and Planning, Sun Yat-sen University, Guangzhou, China – sequence: 5 givenname: Rui-Xin surname: Huang fullname: Huang, Rui-Xin organization: Woods Hole Oceanographic Institution, Massachusetts, Woods Hole, USA |
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| Snippet | Over the period 2003–2011, the Gravity Recovery and Climate Experiment (GRACE) satellite pair revealed a remarkable variability in mass‐induced sea surface... Over the period 2003-2011, the Gravity Recovery and Climate Experiment (GRACE) satellite pair revealed a remarkable variability in mass-induced sea surface... |
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| SubjectTerms | Altimetry Atmospheric circulation Atmospheric research Atmospherics Geophysics GRACE GRACE (experiment) Marine mass-induced sea surface height northwestern North Pacific Ocean temperature Oscillations Regression analysis Sea level Sea level changes sea surface height Surface wind Trends Wind |
| Title | Mass-induced sea level change in the northwestern North Pacific and its contribution to total sea level change |
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