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Seasonally in sub-surface chlorophyll maxima in the Arabian Sea: Detection by IRS-P4/OCM and implication of it to primary productivity

机译:在阿拉伯海中的亚表面叶绿素最大值中季节性:通过IRS-P4 / OCM检测并对初级生产力的含义

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Arabian Sea is highly influenced by monsoon systems like SW monsoon (June -September) and NE monsoon (December-February). This affects distribution pattern of phytoplankton, availability of nutrients and changing temperature specially during winter cooling period (February-March). These and other conditions like quality and quantity of light influence phytoplankton (type and concentration) in the Arabian Sea. In our study we have observed monsoon related peaks in phytoplankton and chlorophyll a in the Arabian Sea. These chlorophyll a (Chi a) concentrations detected by OCM sensor onboard IRS-P4 satellite is helping us to work out seasonality of phytoplankton in the Arabian Sea, which is of the great importance in the field of biology and biogeochemistry of this region. However, during these study subsurface chlorophyll a maxima (SCM) was observed as characteristics feature of chlorophyll a distribution in the Arabian Sea. The subsurface chlorophyll a maxima varies from 30m to 55m in the Arabian Sea during various seasons. During November at St. 1 surface chlorophyll a was 1.503 mgm3and subsurface chlorophyll maxima was 12.692 mgm-3. Similarly, at St. 13 surface chlorophyll a was 0.584 mgm-3and surface chlorophyll maxima was 8.517 mgm-3. During upwelling, nutrients remained unused at sub surface due to shortage of light which may lead to subsurface blooms, detection of which is critical for precise estimation of chlorophyll a from ocean colour sensor. During our 5 year study (covering all the seasons) in northeastern (NE) Arabian Sea, we have observed more than 50 % stations were with subsurface chlorophyll a maxima where chlorophyll a was approximately 10 times higher compared to surface value. The high chlorophyll some time detected by OCM is mainly because of detection of subsurface chlorophyll maxima by the satellite but may not actually sampled during ship studies. The satellite penetration depth (ze), subsurface chlorophyll maxima depth, OCM derived chlorophyll a for different seasons in NE Arabian Sea is presented and discussed in this paper.
机译:阿拉伯海受到SW季风(六月 - 京日)和Ne Monsoon(12月至2月)的季风系统受到高度影响。这影响了冬季冷却期间(2月至3月)在冬季冷却期间植物的分布模式,营养素的可用性和变化温度。这些和其他条件,如质量和光线影响在阿拉伯海中的浮游植物(类型和浓度)。在我们的研究中,我们观察了阿拉伯海中浮游植物和叶绿素A中的季风相关峰。这些叶绿素A(ChI A)由OCM传感器船上检测到的浓度IRS-P4卫星正在帮助我们在阿拉伯海中植物季节性,这在该地区的生物学和生物地球化学领域具有重要意义。然而,在这些研究期间,地下叶绿素叶绿素(SCM)被观察到作为阿拉伯海中叶绿素A分布的特征特征。在各个季节,地下叶绿素最大值在阿拉伯海中的30米到55米。 11月在圣1表面叶绿素A为1.503 mgm3和地下叶绿素最大值为12.692 mgm-3。类似地,在圣13表面叶绿素A为0.584mgm-3和表面叶绿素最大值为8.517mgm-3。在上升期间,由于光线缺乏可能导致地下盛开的缺点,营养物质在子表面上保持未使用,检测到来自海洋颜色传感器的叶绿素A的精确估计至关重要。在我们的5年的学习(覆盖所有季节)在东北(NE)阿拉伯海,我们观察到超过50%的站点是叶绿素的最大值,而叶绿素A与表面值相比大约10倍。 OCM检测到的高叶绿素主要是由于卫星检测到地下叶绿素最大值,但在船舶研究期间可能无法实际采样。本文提出并讨论了卫星渗透深度(ZE),地下叶绿素最大值深度,OCM衍生出不同季节的叶绿素A.

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