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首页> 外文期刊>Journal of Geology & Geophysics >Bio-physical Changes in the Eastern Arabian Sea due to Ocean-Atmospheric Teleconnections
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Bio-physical Changes in the Eastern Arabian Sea due to Ocean-Atmospheric Teleconnections

机译:海洋-大气遥相关导致阿拉伯东部海域的生物物理变化

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Arabian Sea is in general biologically most productive region in the North Indian Ocean, in particular eastern Arabian Sea. However, there is a lack of pre-existing studies performed to reveal the seasonal and interannual variability of the primary production. The potential role of atmospheric and oceanographic events on promoting the distinct development of phytoplankton in the northern and southern parts of eastern Arabian Sea regions was investigated in this article. In order to study the temporal variability of the bio-physical parameters, we used 12 years (1998-2009) of Sea WiFS chlorophyll-a data and 10 years (2000-2009) of QuickSCAT wind stress data (zonal and meridional) as two important forcing parameters. Relative impacts of the Indian Ocean Dipole (IOD), associated with the global climatic event of El Ni?o Southern Oscillation (ENSO) on biophysical parameters of eastern Arabian Sea during the study period have been analyzed at the two regions. Seasonal and interannual variabilities are clearly observed in both chlorophyll-a and wind stress time series. The overall seasonal variation for chlorophyll-a were 0.17 and 2.29 mg m-3 with a standard deviation of 0.03 and 0.54 mg m-3 for the northern and southern regions, respectively, and the coefficient of variation was 8-65%. The relationship between chlorophyll-a and multivariate ENSO index was negative at northern and southern regions in all seasons, and the IOD also showed negative relation except pre monsoon sea.
机译:一般而言,阿拉伯海是北印度洋,尤其是阿拉伯海东部生物学上生产力最高的地区。但是,缺乏先前的研究来揭示初级生产的季节和年度变化。本文研究了大气和海洋事件对促进阿拉伯海东部和北部地区浮游植物显着发展的潜在作用。为了研究生物物理参数的时间变异性,我们使用了12年(1998-2009年)的Sea WiFS叶绿素a数据和10年(2000-2009年)的QuickSCAT风应力数据(区域和子午线)作为两个重要的强制参数。在研究期间,分析了印度洋偶极子(IOD)与厄尔尼诺南方涛动(ENSO)的全球气候事件对阿拉伯海东部生物物理参数的相对影响。在叶绿素a和风胁迫时间序列中都清楚地观察到季节和年际变化。叶绿素-a的总体季节变化为0.17和2.29 mg m-3,北部和南部区域的标准偏差分别为0.03和0.54 mg m-3,变化系数为8-65%。在所有季节中,北部和南部地区的叶绿素-a与多元ENSO指数之间的关系均为负,除季风海以外,IOD也呈负相关。

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