DOI: | 10.1002/2015GL063902
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论文题名: | An increase in the rate of global mean sea level rise since 2010 |
作者: | Yi S.; Sun W.; Heki K.; Qian A.
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刊名: | Geophysical Research Letters
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ISSN: | 0094-9407
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EISSN: | 1944-9138
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出版年: | 2015
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卷: | 42, 期:10 | 起始页码: | 3998
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结束页码: | 4006
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语种: | 英语
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英文关键词: | GMSL
; GRACE
; La Niña
; sea level budget
; sea level rise
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Scopus关键词: | Atmospheric pressure
; Budget control
; Geodetic satellites
; Nickel
; Global mean sea levels
; GMSL
; GRACE
; Land ices
; Land water storage
; Sea level rise
; Southern oscillation
; Sea level
; Argo
; El Nino-Southern Oscillation
; global change
; GRACE
; La Nina
; satellite altimetry
; sea level change
; water storage
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英文摘要: | The global mean sea level (GMSL) was reported to have dropped 5 mm due to the 2010/2011 La Niña and have recovered in 1 year. With longer observations, it is shown that the GMSL went further up to a total amount of 11.6 mm by the end of 2012, excluding the 3.0 mm/yr background trend. A reconciled sea level budget, based on observations by Argo project, altimeter, and gravity satellites, reveals that the true GMSL rise has been masked by El Niño-Southern Oscillation-related fluctuations and its rate has increased since 2010. After extracting the influence of land water storage, it is shown that the GMSL has been rising at a rate of 4.4 ± 0.5 mm/yr for more than 3 years, due to an increase in the rate of both land ice loss and steric change. ©2015. American Geophysical Union. All Rights Reserved. |
URL: | https://www.scopus.com/inward/record.uri?eid=2-s2.0-84931562988&doi=10.1002%2f2015GL063902&partnerID=40&md5=88160579af5edd815d2ef9b5724163d0
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Citation statistics: |
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资源类型: | 期刊论文
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标识符: | http://119.78.100.158/handle/2HF3EXSE/9022
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Appears in Collections: | 科学计划与规划 气候变化与战略
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作者单位: | Key Laboratory of Computational Geodynamics, University of Chinese Academy of Sciences, Beijing, China
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Recommended Citation: |
Yi S.,Sun W.,Heki K.,et al. An increase in the rate of global mean sea level rise since 2010[J]. Geophysical Research Letters,2015-01-01,42(10).
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