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Sea ice and spring bloom in the East /Japan Sea

机译:东日本海海冰和春暖花开

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摘要

Relation between the spring bloom along the Primorye coast and sea ices of the Tatarskiy Strait in the northern East/Japan Sea were investigated using ten-year SeaWiFS chlorophyll-a concentration data and sea ice concentration data DMSP/SSMI for the period of 1998-2007. Year-to-year variations of chlorophyll-a concentration in spring were positively correlated with those of sea ice concentrations at the Tatarskiy Strait in die previous winter. Abrupt increases of nutrients, indispensable for spring bloom at the upper ocean in spring, were supplied from sea-ice melted waters. The water mass from sea ices provided a preferable condition for the spring bloom through changes in vertical stratification structure of water column. Along-coast ratios of stability parameters between the two neighboring months clearly show rapid progress of generation of shallow thermocline due to the ice-originated fresh waters.
机译:利用十年的SeaWiFS叶绿素a浓度数据和1998-2007年期间海冰浓度数据DMSP / SSMI,研究了滨海边疆区春季开花与东日本北部塔塔斯基海峡海冰之间的关系。 。春季之前的塔塔尔斯基海峡春季的叶绿素a浓度逐年变化与海冰浓度正相关。海冰融化的水提供了营养的突然增加,这是春季高空春季开花不可缺少的。通过改变水柱的垂直分层结构,海冰中的水团为春季开花提供了较好的条件。相邻两个月之间的稳定性参数沿海岸比率清楚地表明,由于冰源的淡水,浅温跃层的产生迅速进展。

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