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Marine phytoplankton biomass responses to typhoon events in the South China Sea based on physical-biogeochemical model

机译:基于物理生物地球化学模型的海洋浮游植物的生物质响应南海的台风活动

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摘要

Most previous studies confirmed that marine phytoplankton biomass can increased dramatically and then formed blooms along the typhoon track after typhoon passage. However, many events of no significant responses to typhoons were neglected. In order to figure out the most important factor for bloom formation, a coupled physical-biogeochemical model was used to study the biogeochemical phytoplankton responses to all 79 typhoon events that affected the South China Sea (SCS) during 2000-2009. The major factors investigated included typhoon intensity and translation speed, Chlorophyll a concentration (Chl-a) and vertical nitrate transport in the euphotic zone before and after typhoon passage. The results revealed that phytoplankton blooms were triggered after 43 typhoon events, but no significant blooms were found after 36 other typhoons. Of the 43 typhoon events that triggered blooms, 24 were in the open ocean and 19 were on the coast. Subsurface blooms were detected after five typhoon events that did not trigger surface blooms. Over half of the typhoons that affect the oligotrophic SCS can trigger phytoplankton blooms, and contribute to the marine primary productivity. The mechanism of the above results were surveyed, we found that (1) an increased nitrate concentration is the basic and key precondition for phytoplankton blooming in the oligotrophic SCS; (2) typhoon intensity, and translation speed control the upward flux of nitrates together, and translation speed has more effect than intensity; (3) uplifted nitrates could trigger phytoplankton bloom, and Chl-a levels reached a peak 3 days later than nitrate levels; (4) mesoscale eddies and the nutricline depth before a typhoon's arrival also affects bloom genesis; and (5) the composition of phytoplankton functional groups in the coast was adjusted by typhoon, which have more complex mechanism of bloom formation than that in the open ocean. In summary, the physical driving force that modulates blooms is vertical nutrient transportation in the SCS. (C) 2017 Elsevier B.V. All rights reserved.
机译:最先前的研究证实,海洋浮游植物生物质可以急剧增加,然后在台风通道后沿着台风轨道形成绽放。然而,许多对台风没有重大反应的事件被忽视了。为了弄清楚盛开形成的最重要因素,耦合的物理生物地球化学模型用于研究生物地球化学浮游植物对2000 - 2009年期间南海(SCS)影响的所有79个台风事件。调查的主要因素包括台风通道前后Euphone区中叶绿素强度和翻译速度,叶绿素浓度(CHL-A)和垂直硝酸盐转运。结果表明,在43台台风活动后触发了浮游植物盛开,但在其他36个其他台风后没有发现显着的绽放。在触发绽放的43个台风活动中,24次在开阔的海洋中,19岁的是在海岸。在没有触发表面绽放的五个台风事件之后检测到地下绽放。超过影响寡营养的SCS的一半的台风可以触发浮游植物盛开,并有助于海洋初级生产力。调查了上述结果的机制,我们发现(1)增加硝酸盐浓度是植物浮游植物中浮游植物的基本和关键前提; (2)台风强度,翻译速度控制硝酸盐的向上通量,而翻译速度比强度更多; (3)升高的硝酸盐可以引发浮游植物绽放,CHL-A水平比硝酸水平晚3天达到峰值; (4)台风到达前的Messcale Eddies和Nutricline深度也会影响盛开的创世纪; (5)沿着海岸的浮游植物官能团的组成由台风调节,其具有比开阔的海洋的更复杂的绽放形成机制。总之,调制盛开的物理驱动力是SCS中的垂直营养运输。 (c)2017 Elsevier B.v.保留所有权利。

著录项

  • 来源
    《Ecological Modelling》 |2017年第2017期|共10页
  • 作者单位

    Chinese Acad Sci South China Sea Inst Oceanol State Key Lab Trop Oceanog LTO Guangzhou 510301 Guangdong Peoples R China;

    Univ Maine Sch Marine Sci Orono ME 04469 USA;

    Chinese Acad Sci South China Sea Inst Oceanol State Key Lab Trop Oceanog LTO Guangzhou 510301 Guangdong Peoples R China;

    Chinese Acad Sci South China Sea Inst Oceanol State Key Lab Trop Oceanog LTO Guangzhou 510301 Guangdong Peoples R China;

  • 收录信息
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 环境生物学;
  • 关键词

    Typhoon; Phytoplankton bloom; Primary productivity; South China sea; ROMS-CoSiNE model;

    机译:台风;Phytoplankton Bloom;初级生产力;南海;罗姆斯 - 余弦模型;
  • 入库时间 2022-08-20 02:28:02

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