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Inter-annual and decadal sea level variations in the north-western Pacific marginal seas

机译:西北太平洋边缘海的年际和年代际海平面变化

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摘要

Long term sea level changes in the Okhotsk, Japan/East, East China and Yellow Seas have been explored based on mean monthly values of sea level from tide gauge and altimetry measurements. The analysis of low frequency sea level variability reveals clearly differentiated areas: the Okhotsk Sea and the northern sector of the Japan/East Sea display lower sea level variances and no sea level rise. The southern Japan/ East Sea presents larger sea level variability associated with the circulation regime of the warm current entering through the Tsushima Strait and inter-annual sea level variations that are driven by steric and atmospheric changes. The largest sea level variances are found in the Yellow Sea due to the effect of atmospheric forcing over the continental shelf. Inter-annual variability is spatially varying within the Yellow Sea and the East China Sea and is mainly related to the steric sea level changes. Regional mean sea level indices have been synthesized for each area using the longest tide gauge records and have revealed correlations between the southern Japan/East and Yellow Seas with PDO and NP climatic indices. Linear trends at coastal sites in the Japan/East, East China and Yellow Seas show a rather heterogeneous pattern, with values between -1.5 and 5.5 mm/yr for the period 1960-2000. During the period 1993-2008 linear trends derived from coastal tide gauges and from altimetry observations are coherent and reveal a southwards increasing pattern with maximum averaged values reached at the Yellow Sea (4.9 ±1.9 mm/yr) followed by the Japan/East Sea (3.8 ± 0.9 mm/yr). Decadal rates of sea level change show distinct behaviour among basins as well as with the global average. The southern Japan/East Sea, the East China Sea and the Yellow Sea display decadal variability which is out of phase with respect to the global values.
机译:根据潮汐仪和测高仪测得的平均海平面月度值,对鄂霍次克州,日本/东部,中国东部和黄海的长期海平面变化进行了研究。低频海平面变化的分析揭示了明显不同的区域:鄂霍次克海和日本/东海北部地区显示出较低的海平面变化且没有海平面上升。日本南部/东海呈现出较大的海平面变化性,这与通过对马海峡进入的暖流的环流状况以及由空间和大气变化驱动的年际海平面变化有关。由于大陆架上的大气强迫作用,在黄海发现最大的海平面变化。黄海和东中国海的年际变化在空间上是变化的,并且主要与空间海平面的变化有关。利用最长的潮汐记录仪对每个地区的区域平均海平面指数进行了合成,并揭示了日本南部/东海和黄海与PDO和NP气候指数之间的相关性。日本/华东,华东和黄海沿岸站点的线性趋势显示出一种相当不同的模式,在1960-2000年期间,其年值在-1.5至5.5 mm / yr之间。在1993年至2008年期间,来自沿海潮汐仪和测高仪观测的线性趋势是连贯的,并显示出向南增加的格局,黄海的最大值达到最大值(4.9±1.9 mm / yr),其次是日本/东海( 3.8±0.9毫米/年)。十年间海平面变化率显示了各盆地之间以及全球平均水平的不同行为。日本南部/东海,东中国海和黄海显示年代际变化,相对于全球价值而言,年代际变化是不同的。

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  • 来源
    《Progress in Oceanography》 |2012年第10期|p.4-21|共18页
  • 作者单位

    IMEDEA (UIB-CSIC), Miquel Marques, 21, 07190, Balearic Islands, Spain;

    National Oceanography Centre Southampton, SO14 3ZH, United Kingdom;

    College of Marine Science, University of South Florida, St. Petersburg United States;

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