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- W2023157364 abstract "[1] The sea level trend from1992 to 2006 was estimated by combining satellite altimeter data with in situ hydrographic data along the TOPEX/POSEIDON and Jason-1 subsatellite track south of Japan. The sea level trend estimates from the altimeter data were consistent with those from the coastal tide gauge data. The mean sea level trend along the hydrographic observation line was 4.2 ± 0.8 mm a–1. By assuming that the sea level trend due to large-scale deformation of ocean basins from glacial isostatic adjustment is –0.3 mm a–1, the sea level trend by the ocean mass change was estimated to be 1.3 ± 0.4 mm a–1, and the steric height trend was estimated to be 3.2 ± 0.9 mm a–1 (2.8 ± 0.9 mm a–1 between 0 and 1800 dbar plus 0.4 ± 0.2 mm a–1 between 1800 and 4500 dbar). Steric height estimated from the altimeter data agreed well with that estimated from the conductivity-temperature-depth profiler and expendable bathythermograph data. However, steric height estimated from the Argo float data over year 2004–2006 was significantly biased of about –10 mm on average with respect to that estimated from the altimeter data. A systematic pressure error of about –2 dbar in the Argo float profiles could account for this negative bias in steric height." @default.
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- W2023157364 date "2008-09-30" @default.
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- W2023157364 title "Estimation of the sea level trend south of Japan by combining satellite altimeter data with in situ hydrographic data" @default.
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- W2023157364 doi "https://doi.org/10.1029/2008jc004796" @default.
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