Detailed spatiotemporal impacts of El Ni?o on phytoplankton biomass in the        <fc xmlns='http://www.wiley.com/namespaces/wiley'>S</fc>S        outh        <fc xmlns='http://www.wiley.com/namespaces/wiley'>C</fc>C        hina        <fc xmlns='http://www.wiley.com/namespaces/wiley'>S</fc>S        ea

Siswanto Eko; Ye Haijun; Yamazaki Dai; Tang DanLing

摘要

Abstract > The lagging and leading correlations among satellite observations, reanalyzed biogeophysical data, and the Nino3.4 El Ni?o index were investigated to reveal the impacts of El Ni?o on the phytoplankton biomass (chlorophyll a [Chl a ]) in the South China Sea (SCS), in an attempt to identify the probable responsible factors in greater spatiotemporal detail. A basin‐scale high Chl a concentration during the developing phase of El Ni?o changed to basin‐scale low Chl a during the weakening phase. Cyclonic wind circulation in the northern basin, increased wind speed in the southern basin, and strengthened upwelling off the Vietnamese coast likely caused a basin‐scale nutrient increase during the developing phase of an El Ni?o event; the opposite conditions led to low nutrient levels during the weakening phase. Decreases in Chl a east of the Vietnamese coast and northwest of Borneo Island were due to decreases in nutrients supplied by rivers. These spatiotemporal changes are considered biogeophysical responses to a variety of types of El Ni?o. Regardless of the El Ni?o type, reanalyzing biogeophysical data sets during central Pacific warming separately from those during eastern Pacific warming is recommended for a more robust understanding of the detailed spatiotemporal impacts of different El Ni?o types on the biogeophysical environment of the SCS. </abstract> </span> <span class="z_kbtn z_kbtnclass hoverxs" style="display: none;">展开▼</span> </div> <div class="translation abstracttxt"> <span class="zhankaihshouqi fivelineshidden" id="abstract"> <span>机译：</span><abstract xmlns =“http://www.wiley.com/namespaces/wiley”type =“main”> <标题类型=“main”>抽象</ title> > 研究了卫星观察结果，重新分析的生物果质数据和Nino3.4 El Niβ0指数之间的滞留和主要相关性，揭示了El Ni-O对浮游植物生物量（叶绿素）的影响（叶绿素） a </ i> [CHL. a </ i> ]）在南海（SCS）中，试图以更大的时空细节确定可能的负责因素。盆地高CHL a </ i> El Ni的显影阶段浓度变为盆地低CHL a </ i> 在弱化阶段。北部盆地的旋风风循环，南部盆地的风速增加，加强了越南海岸的升温可能导致EL NI的发展阶段的盆地营养增加;相反的条件导致弱化相期间的营养水平低。 CHL下降 a </ i> 越南海岸和婆罗洲岛西北部的东部是由于河流提供的营养素减少。这些时尚的变化被认为是对各种类型的EL NI o的生物果实响应。无论El Ni吗？O类型，建议在中央太平洋中加热中的重共生物格格理数据集，以便更加强大地了解不同EL NIΔO类型对SCS的生物果实环境的详细时尚影响。 </ p> </摘要> </span> <span class="z_kbtn z_kbtnclass hoverxs" style="display: none;">展开▼</span> </div> </div> <div class="record"> <h2 class="all_title" id="enpatent33" > 著录项</h2> <ul> <li> <span class="lefttit">来源</span> <div style="width: 86%;vertical-align: text-top;display: inline-block;"> <a href='/journal-foreign-34643/'>《Journal of Geophysical Research, C. Oceans: JGR 》</a> <b style="margin: 0 2px;">|</b><span>2017年第4期</span><b style="margin: 0 2px;">|</b> <span>共15页</span> </div> </li> <li> <div class="author"> <span class="lefttit">作者</span> <p id="fAuthorthree" class="threelineshidden zhankaihshouqi"> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Siswanto Eko&option=202" target="_blank" rel="nofollow">Siswanto Eko;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Ye Haijun&option=202" target="_blank" rel="nofollow">Ye Haijun;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Yamazaki Dai&option=202" target="_blank" rel="nofollow">Yamazaki Dai;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Tang DanLing&option=202" target="_blank" rel="nofollow">Tang DanLing;</a> </p> <span class="z_kbtnclass z_kbtnclassall hoverxs" id="zkzz" style="display: none;">展开▼</span> </div> </li> <li> <div style="display: flex;"> <span class="lefttit">作者单位</span> <div style="position: relative;margin-left: 3px;max-width: 639px;"> <div class="threelineshidden zhankaihshouqi" id="fOrgthree"> <p>Department of Environmental and Geochemical Cycle ResearchJapan Agency for Marine‐Earth Science and TechnologyYokohama Japan;</p> <p>State Key Laboratory of Tropical OceanographySouth China Sea Institute of Oceanology Chinese Academy of SciencesGuangzhou China;</p> <p>Department of Integrated Climate Change Projection ResearchJapan Agency for Marine‐Earth Science and TechnologyYokohama Japan;</p> <p>State Key Laboratory of Tropical OceanographySouth China Sea Institute of Oceanology Chinese Academy of SciencesGuangzhou China;</p> </div> <span class="z_kbtnclass z_kbtnclassall hoverxs" id="zhdw" style="display: none;">展开▼</span> </div> </div> </li> <li> <span class="lefttit">收录信息</span> <span style="width: 86%;vertical-align: text-top;display: inline-block;"></span> </li> <li> <span class="lefttit">原文格式</span> <span>PDF</span> </li> <li> <span class="lefttit">正文语种</span> <span>eng</span> </li> <li> <span class="lefttit">中图分类</span> <span> <a href="https://www.zhangqiaokeyan.com/clc/163.html" title="地球物理学">地球物理学 ;</a></span> </li> <li class="antistop"> <span class="lefttit">关键词</span> <p style="width: 86%;vertical-align: text-top;"> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=chlorophyll a&option=203" rel="nofollow">chlorophyll a;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=El Ni?o&option=203" rel="nofollow">El Ni?o;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=nutrient sources&option=203" rel="nofollow">nutrient sources;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=ocean color&option=203" rel="nofollow">ocean color;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=upwelling/downwelling&option=203" rel="nofollow">upwelling/downwelling;</a> </p> <div class="translation"> 机译：叶绿素a;el ni？o;营养来源;海洋颜色;上升/贫困; 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Detailed spatiotemporal impacts of El Ni?o on phytoplankton biomass in the SS outh CC hina SS ea

摘要