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The Influence of Sea Ice and Snow Cover and Nutrient Availability on the Formation of Massive Under-Ice Phytoplankton Blooms in the Chukchi Sea

机译:楚科奇海海冰雪覆盖和养分供应量对海冰下浮游植物大量开花形成的影响

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摘要

A coupled biophysical model is used to examine the impact of changes in sea ice and snow cover and nutrient availability on the formation of massive under-ice phytoplankton blooms (MUPBs) in the Chukchi Sea of the Arctic Ocean over the period 1988–2013. The model is able to reproduce the basic features of the ICESCAPE (Impacts of Climate on EcoSystems and Chemistry of the Arctic Pacific Environment) observed MUPB during July 2011. The simulated MUPBs occur every year during 1988–2013, mainly in between mid-June and mid-July. While the simulated under-ice blooms of moderate magnitude are widespread in the Chukchi Sea, MUPBs are less so. On average, the area fraction of MUPBs in the ice-covered areas of the Chukchi Sea during June and July is about 8%, which has been increasing at a rate of 2% yr–1 over 1988–2013. The simulated increase in the area fraction as well as primary productivity and chlorophyll a biomass is linked to an increase in light availability, in response to a decrease in sea ice and snow cover, and an increase in nutrient availability in the upper 100 m of the ocean, in conjunction with an intensification of ocean circulation. Simulated MUPBs are temporally sporadic and spatially patchy because of strong spatiotemporal variations of light and nutrient availability. However, as observed during ICESCAPE, there is a high likelihood that MUPBs may form at the shelf break, where the model simulates enhanced nutrient concentration that is seldom depleted between mid-June and mid-July because of generally robust shelf-break upwelling and other dynamic ocean processes. The occurrence of MUPBs at the shelf break is more frequent in the past decade than in the earlier period because of elevated light availability there. It may be even more frequent in the future if the sea ice and snow cover continues to decline such that light is more available at the shelf break to further boost the formation of MUPBs there.
机译:耦合生物物理模型用于检验1988-2013年期间北冰洋楚科奇海中海冰和积雪的变化以及养分的可利用性对北冰洋楚科奇海中大量浮冰下浮游植物水华形成的影响。该模型能够再现2011年7月观测到的MUPB的基本特征(气候对北极太平洋环境的生态系统和化学的影响)。模拟的MUPB每年在1988-2013年期间发生,主要发生在6月中旬至6月中旬之间。七月中旬。尽管在楚科奇海中普遍存在中等程度的冰下大花,但MUPB却很少。在6月和7月,楚科奇海冰雪覆盖地区的MUPB平均面积分数约为8%,在1988-2013年期间,yr-1的年增长率为2%。响应于海冰和积雪减少以及高海拔100 m的养分可利用性增加,模拟的面积分数以及初级生产力和叶绿素a生物量的增加与光可利用性的增加有关。海洋,以及海洋环流的加剧。由于光和养分利用率的强烈时空变化,模拟的MUPB在时间上是零星的,在空间上是零散的。但是,如在ICESCAPE期间观察到的那样,极有可能在货架期形成MUPB,在该模式下,模拟的养分浓度提高了,由于总体上强劲的货架期向上上升和其他原因,该浓度在6月中旬至7月中旬之间很少耗尽。动态的海洋过程。在过去的十年中,由于早些时候的光利用率较高,因此在货架断裂处发生MUPB的频率比在早期时期高。如果将来海冰和积雪继续减少,以便在架子断裂处有更多的光可用,以进一步促进那里的MUPB形成,将来可能会更加频繁。

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