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首页> 外文期刊>Remote Sensing of Environment: An Interdisciplinary Journal >Coccolithophore bloom detection in the north east Atlantic using SeaWiFS: Algorithm description, application and sensitivity analysis
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Coccolithophore bloom detection in the north east Atlantic using SeaWiFS: Algorithm description, application and sensitivity analysis

机译:使用SeaWiFS探测东北大西洋的球石藻水华:算法描述,应用和敏感性分析

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摘要

Coccolithophores are the largest source of calcium carbonate in the oceans and are considered to play an important role in oceanic carbon cycles. Current methods to detect the presence of coccolithophore blooms from Earth observation data often produce high numbers of false positives in shelf seas and coastal zones due to the spectral similarity between coccolithophores and other suspended particulates. Current methods are therefore unable to characterise the bloom events in shelf seas and coastal zones, despite the importance of these phytoplankton in the global carbon cycle. A novel approach to detect the presence of coccolithophore blooms from Earth observation data is presented. The method builds upon previous optical work and uses a statistical framework to combine spectral, spatial and temporal information to produce maps of coccolithophore bloom extent. Validation and verification results for an area of the north east Atlantic are presented using an in situ database (N=432) and all available SeaWiFS data for 2003 and 2004. Verification results show that the approach produces a temporal seasonal signal consistent with biological studies of these phytoplankton. Validation using the in situ coccolithophore cell count database shows a high correct recognition rate of 80% and a low false-positive rate of 0.14 (in comparison to 63% and 0.34 respectively for the established, purely spectral approach). To guide its broader use, a full sensitivity analysis for the algorithm parameters is presented.
机译:球墨镜是海洋中碳酸钙的最大来源,被认为在海洋碳循环中起着重要的作用。由于球墨镜与其他悬浮颗粒之间的光谱相似性,目前从地球观测数据中检测出球石藻水华的方法通常会在架子海和沿海地区产生大量假阳性。因此,尽管这些浮游植物在全球碳循环中非常重要,但目前的方法无法表征架子海和沿海地区的水华事件。提出了一种从地球观测数据中发现球石藻水华的新方法。该方法以先前的光学工作为基础,并使用统计框架将光谱,空间和时间信息相结合,以生成球石藻开花程度的图。使用原位数据库(N = 432)以及2003年和2004年所有可用的SeaWiFS数据提供了东北大西洋地区的验证和验证结果。验证结果表明,该方法产生的时间季节性信号与墨西哥的生物学研究一致。这些浮游植物。使用原位球墨石细胞计数数据库进行的验证显示,正确率高达80%,假阳性率只有0.14(相比之下,已建立的纯光谱方法分别为63%和0.34)。为了指导其更广泛的使用,对算法参数进行了全面的灵敏度分析。

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