波罗的海卫星海洋颜色数据的云掩蔽方案及其在蓝藻华分析中的应用

A. Banks, F. Mélin
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引用次数: 0

摘要

利用海洋彩色遥感数据的最重要步骤之一是从卫星上的信号中减去大气的贡献,以获得海水留下的辐射。要准确地做到这一点,需要有晴朗的天空条件,即在大气校正之前,需要从数据中排除或掩盖所有的云。在处理美国宇航局全球海洋颜色数据时,常规使用的标准云掩模是基于一个简单的阈值,该阈值应用于瑞利校正的大气顶部辐射。为了确保在全球范围内进行高质量的加工,有目的地将门槛保持在较低的水平。因此,标准方案有时会无意中掩盖极端的光学事件,例如波罗的海的蓝绿藻(蓝藻)大量繁殖。这些水华对流域有重要的生态和环境影响,需要适当的监测。因此,通过系统地测试它们在SeaWiFS、MODIS和MERIS数据时间序列上的应用,对现有的5种可为波罗的海提供有价值的备选方案进行了评估。通过将它们应用于多年的卫星数据,分析了时间和空间影响,并开发了一种新的混合云掩模,并进行了类似的测试。结果表明,通过更换标准的云掩膜,波罗的海的海洋覆盖率在一个季节周期内平均增加22%是可能的。严重的水华可以恢复,同时不会在处理过程中引入任何额外的云。将蓝藻华,甚至是它们最强烈的表现,全面纳入波罗的海数据系列,可以更全面地分析它们的光谱特征,对它们的检测、监测和年际演变具有重要意义。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Cloud masking schemes for satellite ocean colour data in the Baltic sea and applications to cyanobacteria bloom analysis
One of the most important steps in utilizing ocean colour remote sensing data is subtracting the contribution of the atmosphere from the signal at the satellite to obtain marine water leaving radiance. To be done accurately this requires clear sky conditions, i.e. all clouds need to be excluded or masked from the data prior to atmospheric correction. The standard cloud mask used routinely in the processing of NASA's global ocean colour data is based on a simple threshold applied to the Rayleigh-corrected top-of-atmosphere radiance. The threshold is kept purposefully low to ensure high quality processing at a global scale. As a consequence, the standard scheme can sometimes inadvertently mask extreme optical events such as intense blue-green algal (cyanobacteria) blooms in the Baltic Sea. These blooms have important ecological and environmental impacts on the basin and require appropriate monitoring. Therefore, an assessment of 5 existing cloud masking schemes that could provide valuable alternatives for the Baltic Sea was carried out by systematically testing their application to time series of SeaWiFS, MODIS and MERIS data. By applying them to a number of years of satellite data, temporal and spatial implications were analyzed and a new hybrid cloud mask was developed and similarly tested. The results indicate that, by replacing the standard cloud mask, an increase of an average of 22% in ocean coverage over the course of a seasonal cycle in the Baltic Sea may be possible. Major occurrences of intense blooms can be recovered whilst at the same time not introducing any significant extra cloud into the processing. The full inclusion of the cyanobacteria blooms, even their most intense manifestations, into Baltic data series allows a more comprehensive analysis of their spectral characteristics with powerful implications for their detection, monitoring, and interannual evolution.
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