globalchange  > 气候变化与战略
DOI: 10.1073/pnas.1519132113
论文题名:
Revisiting the contemporary sea-level budget on global and regional scales
作者: Rietbroek R.; Brunnabend S.-E.; Kusche J.; Schröter J.; Dahle C.
刊名: Proceedings of the National Academy of Sciences of the United States of America
ISSN: 0027-8424
出版年: 2016
卷: 113, 期:6
起始页码: 1504
结束页码: 1509
语种: 英语
英文关键词: Altimetry ; Budget ; GRACE ; Sea level ; Steric
英文摘要: Dividing the sea-level budget into contributions from ice sheets and glaciers, the water cycle, steric expansion, and crustal movement is challenging, especially on regional scales. Here, Gravity Recovery And Climate Experiment (GRACE) gravity observations and sea-level anomalies from altimetry are used in a joint inversion, ensuring a consistent decomposition of the global and regional sea-level rise budget. Over the years 2002-2014, we find a global mean steric trend of 1.38 ± 0.16 mm/y, compared with a total trend of 2.74 ± 0.58 mm/y. This is significantly larger than steric trends derived from in situ temperature/salinity profiles and models which range from 0.66 ± 0.2 to 0.94 ± 0.1 mm/y. Mass contributions from ice sheets and glaciers (1.37 ± 0.09 mm/y, accelerating with 0.03 ± 0.02 mm/y2) are offset by a negative hydrological component (-0.29 ± 0.26 mm/y). The combined mass rate (1.08 ± 0.3 mm/y) is smaller than previous GRACE estimates (up to 2 mm/y), but it is consistent with the sum of individual contributions (ice sheets, glaciers, and hydrology) found in literature. The altimetric sea-level budget is closed by coestimating a remaining component of 0.22 ± 0.26 mm/y. Well above average sea-level rise is found regionally near the Philippines (14.7 ±4.39 mm/y) and Indonesia (8.3 ± 4.7 mm/y) which is dominated by steric components (11.2 ± 3.58 mm/y and 6.4 ± 3.18 mm/y, respectively). In contrast, in the central and Eastern part of the Pacific, negative steric trends (down to -2.8 ± 1.53 mm/y) are detected. Significant regional components are found, up to 5.3 ± 2.6 mm/y in the northwest Atlantic, which are likely due to ocean bottom pressure variations.
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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/162126
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作者单位: Rietbroek, R., Institute of Geodesy and Geoinformation, University of Bonn, Bonn, D-53115, Germany; Brunnabend, S.-E., Institute of Geodesy and Geoinformation, University of Bonn, Bonn, D-53115, Germany, Alfred Wegener Institute for Polar and Marine Research, Bremerhaven, D-27570, Germany; Kusche, J., Institute of Geodesy and Geoinformation, University of Bonn, Bonn, D-53115, Germany; Schröter, J., Alfred Wegener Institute for Polar and Marine Research, Bremerhaven, D-27570, Germany; Dahle, C., GFZ German Research Centre for Geosciences, Potsdam, D-14473, Germany

Recommended Citation:
Rietbroek R.,Brunnabend S.-E.,Kusche J.,et al. Revisiting the contemporary sea-level budget on global and regional scales[J]. Proceedings of the National Academy of Sciences of the United States of America,2016-01-01,113(6)
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