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首页> 外文期刊>Journal of Geophysical Research, C. Oceans: JGR >The great 2012 Arctic Ocean summer cyclone enhanced biological productivity on the shelves
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The great 2012 Arctic Ocean summer cyclone enhanced biological productivity on the shelves

机译:2012年极好的北冰洋夏季气旋提高了货架的生物生产力

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[1] A coupled biophysical model is used to examine the impact of the great Arctic cyclone of early August 2012 on the marine planktonic ecosystem in the Pacific sector of the Arctic Ocean (PSA). Model results indicate that the cyclone influences the marine planktonic ecosystem by enhancing productivity on the shelves of the Chukchi, East Siberian, and Laptev seas during the storm. Although the cyclone's passage in the PSA lasted only a few days, the simulated biological effects on the shelves last 1 month or longer. At some locations on the shelves, primary productivity (PP) increases by up to 90% and phytoplankton biomass by up to 40% in the wake of the cyclone. The increase in zooplankton biomass is up to 18% on 31 August and remains 10% on 15 September, more than 1 month after the storm. In the central PSA, however, model simulations indicate a decrease in PP and plankton biomass. The biological gain on the shelves and loss in the central PSA are linked to two factors. (1) The cyclone enhances mixing in the upper ocean, which increases nutrient availability in the surface waters of the shelves; enhanced mixing in the central PSA does not increase productivity because nutrients there are mostly depleted through summer draw down by the time of the cyclone's passage. (2) The cyclone also induces divergence, resulting from the cyclone's low-pressure system that drives cyclonic sea ice and upper ocean circulation, which transports more plankton biomass onto the shelves from the central PSA. The simulated biological gain on the shelves is greater than the loss in the central PSA, and therefore, the production on average over the entire PSA is increased by the cyclone. Because the gain on the shelves is offset by the loss in the central PSA, the average increase over the entire PSA is moderate and lasts only about 10 days. The generally positive impact of cyclones on the marine ecosystem in the Arctic, particularly on the shelves, is likely to grow with increasing summer cyclone activity if the Arctic continues to warm and the ice cover continues to shrink.
机译:[1]一种耦合的生物物理模型用于检验2012年8月上旬的北极大旋风对北冰洋太平洋地区(PSA)海洋浮游生态系统的影响。模型结果表明,飓风在风暴期间通过增加楚科奇海,东西伯利亚海和拉普捷夫海陆架的生产力来影响海洋浮游生态系统。尽管气旋在PSA中的通过仅持续了几天,但在架子上模拟的生物效应却持续了1个月或更长时间。在架子上的某些位置,在飓风过后,初级生产力(PP)增长高达90%,浮游植物生物量增长高达40%。风暴过后一个多月,浮游动物生物量的增加在8月31日达到18%,并在9月15日保持10%。然而,在中央PSA中,模型模拟表明PP和浮游生物量减少。货架上的生物收获和中央PSA的损失与两个因素有关。 (1)旋风增强了上层海洋的混合,增加了架子地表水的养分利用率;中央PSA中增强的混合不会提高生产率,因为在旋风通过之前,那里的养分大部分都在夏季被消耗掉了。 (2)气旋还引起发散,这是由于气旋的低压系统驱动气旋海冰和上层海洋环流,从而将更多的浮游生物质从中央PSA运到架子上。货架上模拟的生物增益大于中央PSA的损耗,因此,旋风分离器可提高整个PSA的平均产量。由于货架上的收益被中央PSA的损失所抵消,因此整个PSA的平均增长是适度的,仅持续约10天。如果北极继续变暖且冰盖继续缩小,随着夏季气旋活动的增加,气旋对北极海洋生态系统(特别是在架子上)的总体积极影响可能会增加。

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