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Temporal variability of chromophoric dissolved organic matter in the Pearl River Estuary, China from 2003 to 2009

机译:Temporal variability of chromophoric dissolved organic matter in the pearl River Estuary, China from 2003 to 2009

摘要

The present study aims to investigate the temporal variability of chromophoric dissolved organic matter through remote sensing and to determine its influence factors in the Pearl River Estuary. A medium resolution imaging spectrometer, chromophoric dissolved organic matter product was evaluated with in situ absorption coefficient (R-2 = 0.9605, RMS = 0.1672 and MRE = 0.3930). L2 daily products were then averaged into monthly data to analyze variability in the specified area from January 2003 to December 2009. Accumulated anomaly analysis and the wavelet analysis showed that the variability had a significant period of one year from 2003 to 2009, accompanied with 3 and 6 month periods in 2004 and 2008 separately. Cross wavelet transform was used to analyze the relationships between chromophoric dissolved organic matter and its influence factors including rainfall and phytoplankton in time frequency space. Relationships with salinity and light were also analyzed. It was found that photobleaching induces lower dissolved organic matter in summer even though there is greater discharge due to large rainfall intensity during this season. However, the anomalous strong precipitation may cause significantly higher findings in the study area. An example was a heavy flood caused by strong precipitation in 2008 induced higher findings for the period for less than half a year.
机译:本研究旨在通过遥感调查发色溶解性有机物的时变性,并确定其在珠江口的影响因素。用原位吸收系数(R-2 = 0.9605,RMS = 0.1672和MRE = 0.3930)评估了中分辨率成像光谱仪发色溶解的有机物产物。然后将L2日产品平均为月度数据,以分析2003年1月至2009年12月指定区域内的变异性。累积异常分析和小波分析表明,该变异性从2003年至2009年具有显着的一年,其中3和3 2004年和2008年分别为6个月。利用交叉小波变换分析了发色溶解有机物与时频空间中降雨和浮游植物的影响因素之间的关系。还分析了与盐度和光照的关系。研究发现,即使由于本季节降雨强度大而排放量增加,光漂白在夏季仍会导致较低的溶解有机物含量。但是,异常强降水可能会在研究区域引起更高的发现。一个例子是2008年强降雨造成的大洪灾,导致在不到半年的时间内获得了更高的调查结果。

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    Liu FF; Tang SL; Chen CQ;

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  • 年度 2014
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