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Remote Sensing of Chlorophyll Concentration in a Bay from Landsat TM Data

机译:LANDSAT TM数据遥感湾叶绿素浓度

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Major inner bays in Japan are in chronic eutrophication and suffering from so-called red tide and blue tide or anoxia in summer, which often cause serious damages to coastal fisheries and environments. In order to improve the water quality and reduce the damage, various kinds of countermeasure have been carried out, which include reducing inflow load of nitrogen and phosphorus, removing organic bottom mud and covering the bottom mud with sand etc. Continuous monitoring of water quality is very important to grasp the effects of these countermeasures and to take proper procedures. Mikawa Bay (area = 604km~2, mean water depth = 9.2m) is a shallow and closed inner bay connected to Ise Bay, where the water quality problems have increasingly been serious due to eutrophication. The prefectural government has continued water quality measurement every month at about 20 locations in the bay. More frequent measurements at more locations are however necessary to understand the dynamic behavior of water quality in the bay In the ocean, satellite images have been used for analyzing distributions of water surface temperature, chlorophyll concentration (Chl-a) and turbidity etc. The remote sensing of water quality in inner bays are also expected because satellite images regularly supply simultaneous information of wide area. Water quality of inner bays is usually evaluated through various indices such as COD, SS and Chl-a etc. Among these, Chl-a is the most important index for eutrophic waters. Estimate of Chl-a in the ocean from satellite images has been tackled by many researchers. In particular, various types of algorithm has been developed and verified for the CZCS sensor on NIMBUS7. Most of them relate Chl-a to a ratio between radiance values of two different bands (Gordon et al., 1983). These algorithms are however applicable only to relatively clear water in the ocean where Chl-a is around several mg/m~3. On the other hand, eutrophic water in inner bays sometimes shows very high concentration more than 100 mg/m~3 with high SS and dissolved organic compound, where these algorithms cannot be applied. In this paper, an algorithm that enables us to estimate Chl-a from Landsat TM data is proposed based on field data obtained in Mikawa Bay for several years. Atmospheric effects that deteriorate the quality of information of Chl-a are considered in the algorithm.
机译:日本主要内海湾患有慢性富营养化,夏季患有所谓的红潮和蓝潮或缺氧,这往往对沿海渔业和环境造成严重损害。为了提高水质,减少损坏,已经进行了各种对策,包括减少氮气和磷的流入量,除去有机底部泥浆,用砂等覆盖底部泥浆。连续监测水质非常重要,以掌握这些对策的影响并采取适当的程序。 Mikawa Bay(面积= 604km〜2,平均水深= 9.2米)是一个浅层封闭的内部海湾,其与ise湾连接,由于富营养化,水质问题越来越严重。县政府在海湾约20个地点持续水质测量。然而,在更多地点更频繁的测量是必要了解海洋中海湾水质的动态行为,卫星图像已被用于分析水面温度,叶绿素浓度(CHL-A)和浊度等的分布。遥控器还预期了内海湾水质的传感,因为卫星图像定期提供广域的同步信息。内部海湾的水质通常通过各种指数进行评估,例如COD,SS和CHL-A等。中,CHL-A是富营养化水域最重要的指标。许多研究人员都解决了来自卫星图像海洋中的CHL-A的估计。特别地,已经为NIMBUS7上的CZCS传感器开发并验证了各种类型的算法。其中大多数都将CHL-A与两个不同频段的辐射值之间的比率(Gordon等,1983)相关联。然而,这些算法仅适用于海洋中相对清澈的水,其中CHL-A在几毫克/ m〜3周围。另一方面,内海湾的富营养化水有时显示出非常高浓度的高于100mg / m〜3,具有高SS和溶解的有机化合物,其中这些算法不能施加。在本文中,基于在Mikawa湾获得的现场数据几年来提出了一种使我们能够从Landsat TM数据估计CHL-A的算法。在算法中考虑了降低CHL-A信息质量的大气效应。

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