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首页> 外文期刊>Revista de Biologia Marina y Oceanografia >Seasonal variability of chlorophyll a and their response to El Nino and La Nina conditions in the Northern Gulf of California
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Seasonal variability of chlorophyll a and their response to El Nino and La Nina conditions in the Northern Gulf of California

机译:加利福尼亚湾北部叶绿素a的季节性变化及其对厄尔尼诺和拉尼娜条件的响应

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In order to determinate the seasonal variability concentrations of chlorophyll-a (Clo-a) derived from satellite observations, and their responses to El Nino and La Nina conditions in the northern Gulf of California (NGC), we used monthly sea color composites from January 1997 to December 2011 from the OCTS and SeaWiFS sensor. The Clo-a seasonality indicate in winter-spring maxima and summer-autumn minimum, with a predominance of the annual signal During El Nino 1997-1998 Clo-a showed low concentrations. During El Nino 2002-2003 the Clo-a show low influence. In La Nina 2007 Clo-a response was positive with high values. In 2011 where registered the highest Clo-a concentration of the entire study period, as result of La Nina phase. From 2003 to 2007 conditions were considered 'normal' in the system. The average pattern of time series suggests that NGC is eutrophic and the interannual variability of Chl-a is influenced by adjacent Pacific Ocean forcing, suggested by a significant inverse relationship of Chl-a and the Multivariate ENOA index (MEI; ENOA: El Nino Austral Oscillation). We propose that shifts from a strong El Nino (1997-1998) to La Nina conditions (1999), the phytoplankton biomass response was low because a great oceanography conditions changes (wind, stability, etc.), however with the shifts from El Nino weak (2009-2010) to La Nina (2011), these conditions represent less stress with a suitable phytoplankton response and the biomass increases.
机译:为了确定卫星观测得出的叶绿素-a(Clo-a)的季节性变化浓度,以及它们对加利福尼亚湾北部(NGC)厄尔尼诺和拉尼娜条件的响应,我们使用了1997年1月至2011年12月来自OCTS和SeaWiFS传感器的月度海色复合材料。1997-1998年厄尔尼诺现象期间,Clo-a的季节性变化表明冬春季最大值和夏秋季最小值,以年度信号为主。在2002-2003年厄尔尼诺现象期间,克洛-阿的影响很小。在2007年拉尼娜现象中,Clo-a响应为正值,值很高。2011年,由于拉尼娜阶段,Clo-a浓度是整个研究期间最高的。从2003年到2007年,系统中的条件被认为是“正常”的。时间序列的平均模式表明NGC是富营养化的,Chl-a的年际变率受到邻近太平洋强迫的影响,Chl-a与多变量ENOA指数(MEI;ENOA:厄尔尼诺南方振荡)。本文认为,从强厄尔尼诺(1997-1998)到拉尼娜条件(1999)的转变,浮游植物生物量响应较低,因为海洋学条件发生了变化(风、稳定性等),但随着厄尔尼诺(2009-2010)向拉尼娜(2011)的转变,这些条件代表了压力较小,浮游植物响应合适,生物量增加。

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