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Satellite and ship studies of phytopiankton in the Northeastern Arabian during 2000 - 2006 period

机译:2000 - 2006年东北阿拉伯植物卫星和潮汐研究

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Sequence of the images from IRS P4 / OCM satellite and extensive shipboard sampling programme are used to understand the seasonal variation of phytopiankton abundance and types in the Northeastern (NE) Arabian Sea and Lakshadweep Sea. An appreciable degree of spatial and temporal variability is observed in chlorophyll a distribution from November to April months, as well as coastal and offshore stations, indicating marked seasonality in phytopiankton distribution in NE Arabian Sea. During November month (fall intermonsoon) average chlorophyll a (Chi a) by fluorometer was (0.799 mgm-3) and by OCM it was 0.584 mgm-3. The higher chlorophyll a observed was due to Trichodesmium (cyanobacteria) blooms. During December the average chlorophyll a was 0.34 mgm-3 also due to Trichodesmium filaments in water column. During January onwards winter cooling led to increase in nutrients which enhanced chlorophyll a value to 0.64 mgm-3 due to growth of flagellates (as seen by high chlorophyll b besides chlorophyll a) in water column. February, March and April supported moderately high chlorophyll value (0. 3 to 0.5 mgm"3) due to growth of prasinophytes (as seen by pigment prasinoxanthin) and blooms of the Noctiluca miliaris. Time series monitoring of Noctiluca bloom was also conducted using OCM based chlorophyll images in NE Arabian Sea. During February chlorophyll a retrieved by OCM was 0.3 to 0.9 mgm-3. Pigment analysis of water samples indicated the equal important of accessory pigment like zeaxanthin, prasinoxanthin, P-carotene. The relevance of these pigments estimated by HPLC like zeaxanthin (cyanobacteria), fucoxanthin (diatoms), peridinin (dinoflagellates) is presented and discussed. Similarly, exercise is conducted in Lakshadweep waters where Trichodesmium related peak in chlorophyll a was observed during March onwards in OCM data. The average chlorophyll a in NE Arabian Sea at surface during November was (0.726 mgm-3), December (0.34 mgm-3), January (0.723 mgm-3), February (0.344 mgm-3), March (0.963 mgm-3) and April 0.665 mgm-3. Similar trend was observed in primary productivity estimates. The attempt is made to work out seasonality in the productivity of the Arabian Sea using OCM derived chlorophyll and relation of enhancement in productivity due to development of winter blooms in the Arabian Sea. The environmental conditions (temperature, wind, nutrients and mixed layer depth) affecting these blooms responsible for year to year variation in bloom biomass and productivity is also presented in detail.
机译:来自IRS P4 / OCM卫星和广泛的船役采样计划的图像序列用于了解植物北非(Ne)阿拉伯海和Lakshadweep海中的植物普通和类型的季节变化。从11月到4月的叶绿素和近海站,在叶绿素的分布中观察到可明显的空间和时间变异程度,以及沿海和近海站,表明在奈伊阿拉伯海的植物科技分布中标志着季节性。 11月月份(崩溃晶体)荧光计的平均叶绿素A(Chi A)是(0.799mgm-3)和OCM,它为0.584mgm-3。观察到的叶绿素A较高是由于芽孢杆菌(蓝藻)绽放。 12月期间,由于水柱中的吡咯丝,平均叶绿素A也为0.34mgm-3。在1月份,冬季冷却导致营养素增加,由于鞭毛酸盐的生长,增强叶绿素的值为0.64mgm-3(如叶绿素A)在水柱中的高叶绿素B. 2月,3月和4月支持中度高叶绿素值(0.3至0.5mgm“3)由于血糖体的生长(如色素普拉西氏菌素所见)和Noctiluca Miliaris的盛开。使用OCM的时间序列监测夜间绽放的监测基于Ne阿拉伯海的基础叶绿素图像。2月份的叶绿素A通过OCM检索为0.3至0.9mgm-3。水样的颜料分析表明了Zeaxanthin,Prasinoxanthin,p-Carotene等附件颜料的相同重要性。这些颜料的相关性估计通过HPLC如玉米蛋白(蓝藻),呈现和讨论了植物黄嘌呤(硅藻),植物黄素(胆碱),赤素蛋白(Dinoflageates)。类似地,在Lakshadweep水域中进行锻炼,其中在3月在OCM数据中向后观察到叶绿素A中的相关峰值。平均叶绿素A.在11月份的地面上的NE阿拉伯海(0.726 MGM-3),12月(0.34 MGM-3),1月(0.723 MGM-3),2月(0.344 MGM-3),3月(0.963米 - 3)和4月0.665 mgm-3。在初级生产力估算中观察到类似的趋势。使用OCM衍生的叶绿素和由于阿拉伯海的冬季盛开的发展,在阿拉伯海的生产力下,在阿拉伯海的生产力下,试图锻炼阿拉伯海的生产力。还详细介绍了影响盛开生物质和生产率的年度变化的这些绽放的环境条件(温度,风,营养物质和混合层深度)。

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