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首页> 外文期刊>Geophysical Research Letters >Sea level changes from Topex-Poseidon altimetry and tide gauges, and vertical crustal motions from DORIS
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Sea level changes from Topex-Poseidon altimetry and tide gauges, and vertical crustal motions from DORIS

机译:Topex-Poseidon测高仪和潮汐仪的海平面变化以及DORIS的垂直地壳运动

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摘要

Sea level difference (Topex-Poseidon minus tide gauge) time series have been computed over 1993-1997 at 53 selected gauges sites. Comparison of these sea level differences with vertical crustal motions derived from the DORIS space geodesy system at 6 colocated sites shows good consistency. At one site (the Socorro volcanic island), a striking correlation is reported between sea level differences and DORIS height time series. The observed trend likely reflects a post eruptive deformation associated with a volcanic eruption that occurred in early 1993. At several other gauge sites, the sea level differences present large linear trends possibly bearing evidence of land motion. This may be the case at Rabaul (Papua New Guinea) where a volcanic eruption took place in autumn of 1994. The sea level differences at Rabaul show a negative trend from this date, likely related to the volcanic event.
机译:1993-1997年期间,在53个选定的测量站上计算了海平面差(Topex-Poseidon减潮仪)时间序列。将这些海平面差异与DORIS空间大地测量系统在6个位于同一地点的垂直地壳运动的比较显示出良好的一致性。在一个地点(索科罗火山岛)上,据报道海平面差异与DORIS高度时间序列之间具有惊人的相关性。观测到的趋势可能反映了1993年初发生的与火山喷发有关的喷发后变形。在其他几个规范地点,海平面差异呈现出很大的线性趋势,可能带有陆地运动的证据。 1994年秋季在拉包尔(巴布亚新几内亚)发生火山喷发就是这种情况。拉包尔的海平面差异从那时起就显示出负趋势,可能与火山事件有关。

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