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首页> 外文期刊>Journal of Geophysical Research, D. Atmospheres: JGR >Wind and rainfall regulation of the diffuse attenuation coefficient in large, shallow lakes from long-term MODIS observations using a semianalytical model
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Wind and rainfall regulation of the diffuse attenuation coefficient in large, shallow lakes from long-term MODIS observations using a semianalytical model

机译:风力和降雨对分散的监管衰减系数在大型浅水湖泊从长期MODIS观察使用semianalytical模型

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摘要

Knowledge of the variation and regulation of the diffuse attenuation coefficient is important for management of lake water quality and ecological environments. Data were collected seven times (378 samples) from 2006 to 2011 in Lake Taihu to improve the existing semianalytical model of diffuse attenuation coefficient at 490 nm (K_d(490)) by measuring in situ K_d(490) and remote sensing reflectance (R_(rs)). This semianalytical model was applied to determine the long-term variation of K_d(490) and its driving factors from Moderate Resolution Imaging Spectroradiometer (MODIS) images. Our semianalytical model of K_d(490) improves the retrieval accuracy of K_d(490) from 29.60 to 22.58 (root-mean-square percentage error) and 24.28 ± 18.54 (mean value ± standard deviation) to 19.29 ± 14.34 (mean absolute relative error). The Kd (490) from maps produced from MODIS images clearly present the temporal and spatial variations of K_d(490). This indicates the suitability of using the improved semianalytical model and MODIS to observe K_d(490) in turbid shallow inland waters. Long-term MODIS observation of K_d(490) shows distinct seasonal and spatial variations. Temporally, the highest and the lowest K_d(490) were found in winter and in summer, respectively. Spatially, high K_d(490) values were primarily distributed in the southwestern and northwestern Lake Taihu, and relatively low K_d(490) values were distributed in Meiliang Bay and Gonghu Bay (the eastern part of the lake and East Bay were excluded in this study due to invalid retrieval results of K_d(490)). Many covarying points were found between K_d(490) and maximum wind speed from long-term observations, suggesting that wind-induced sediment resuspension is the principal driver of high K_d(490). Correlation was also observed between K_d(490) and heavy rainfall events, suggesting the regulating effect of heavy rainfall.
机译:知识的变异和监管漫射衰减系数是重要的湖泊水质和生态的管理环境。(378个样本)从2006年到2011年,太湖湖改善现有的semianalytical模型在490 nm漫射衰减系数(K_d(490)通过测量原位K_d(490)和遥感反射率(R_ (rs))。semianalytical模型应用于确定长期变化K_d(490)和它的驱动中等分辨率成像的因素光谱仪(MODIS)的图像。semianalytical K_d模型(490)提高了检索K_d精度从29.60% (490)(均方根误差百分比)和22.58%24.28±18.54%(平均值±标准差)19.29±14.34%(平均绝对相对误差)。Kd(490)从地图生产的MODIS图像显然现在的时间和空间变化的K_d(490)。使用改进的semianalytical的适用性模型和MODIS观察K_d在浑浊的(490)浅内陆水域。观察K_d(490)显示了明显的季节性和空间变化。和最低K_d(490)在冬季和被发现分别在夏天。值主要是分布式的西南和西北湖太湖,相对较低的K_d(490)值分布Meiliang湾和深厚湾(东部湖和东部湾被排除在外研究由于无效的检索结果K_d(490))。K_d之间》(490)和最大风速长期观测,表明风致沉积物再悬浮的高的主要推动力K_d(490)。也观察到K_d之间》(490)和重吗降雨事件,建议调节的效果强降雨。

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