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MONITORING THE EFFECT OF SEASONAL VARIATION ON THE OCEAN PRODUCTIVITY: A CASE STUDY IN THE BAY OF BENGAL

机译:监测季节变化对海洋生产力的影响:以孟加拉湾为例

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The productivity of the ocean is crucial and can be represented by several oceanic parameters. However, the major indicator for ocean productivity monitoring is phytoplankton (Chlorophyll-a) concentration. The productivity of the ocean is now decreasing due to several factors and the rate of declination is even higher in some part of the ocean such as in the Bay of Bengal. Therefore, long-term monitoring of ocean productivity is important, thus the primary goal of this study is to monitor the changes in ocean productivity in the Bay of Bengal due to the seasonal variation. The observation was made based on two seasons i.e. northeast monsoon (November to February) and southwest monsoon (May to September) over a long-term period. The ten-year (from 2001 to 2010) products of Chlorophyll-a concentration from SeaWiFS were used to analyze the spatial and temporal analysis of ocean productivity at the Bay of Bengal. The finding of this study indicates a long-term variation of ocean productivity at the Bay of Bengal for different seasons. It is found that Chlorophyll-a concentration started to increase in the month of October/November and decreased after January, and this trend of Chlorophyll-a concentration change remains the same for over the past ten years. However, no constant rate of change of Chlorophyll-a concentration from year to year has been observed in this study. This study also observed that ocean productivity is highly varied in the Northwestern region of the Bay of Bengal during the northeast monsoon as compared to other regions. In contrary, ocean productivity was found high at Northeastern part of the Bay during the southwest monsoon period. The probable reason for this variation is the monsoon wind that blows in certain directions (e.g. from Southwestern part to Northeastern during southwest) which reduces the water surface temperature, resulting in an increasead productivity.
机译:海洋的生产力至关重要,可以用几个海洋参数来表示。但是,监测海洋生产力的主要指标是浮游植物(叶绿素-a)的浓度。由于多种因素,海洋的生产力现在正在下降,并且在海洋的某些部分(例如,孟加拉湾)中,磁偏角的发生率甚至更高。因此,长期监测海洋生产力很重要,因此,本研究的主要目标是监测由于季节变化而导致的孟加拉湾海洋生产力的变化。观测是根据长期的两个季节进行的,即东北季风(11月至2月)和西南季风(5月至9月)。 SeaWiFS的叶绿素a浓度的十年(从2001年到2010年)产物用于分析孟加拉湾海洋生产力的时空分析。这项研究的发现表明孟加拉湾不同季节海洋生产力的长期变化。发现叶绿素a的浓度在10月/ 11月开始增加,而在1月后降低,并且在过去的十年中,叶绿素a的浓度变化趋势保持不变。然而,在这项研究中,没有观察到年复一年叶绿素a浓度的恒定变化率。这项研究还观察到,与其他地区相比,东北季风期间孟加拉湾西北地区的海洋生产力差异很大。相反,在西南季风时期,在海湾东北部发现海洋生产力较高。这种变化的可能原因是季风向某些方向吹(例如,在西南期间从西南部向东北部吹来),从而降低了水面温度,从而提高了生产率。

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