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首页> 外文期刊>Hydrology and Earth System Sciences >A new dense 18-year time series of surface water fraction estimates from MODIS for the Mediterranean region
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A new dense 18-year time series of surface water fraction estimates from MODIS for the Mediterranean region

机译:来自地中海地区的MODIS的新密集18岁的地表水分分数估算

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摘要

Detailed knowledge on surface water distribution and its changes is of high importance for water management and biodiversity conservation. Landsat-based assessments of surface water, such as the Global Surface Water (GSW) dataset developed by the European Commission Joint Research Centre (JRC), may not capture important changes in surface water during months with considerable cloud cover. This results in large temporal gaps in the Landsat record that prevent the accurate assessment of surface water dynamics. Here we show that the frequent global acquisitions by the Moderate Resolution Imaging Spectrometer (MODIS) sensors can compensate for this shortcoming, and in addition allow for the examination of surface water changes at fine temporal resolution. To account for water bodies smaller than a MODIS cell, we developed a global rule-based regression model for estimating the surface water fraction from a 500m nadir reflectance product from MODIS (MCD43A4). The model was trained and evaluated with the GSW monthly water history dataset. A high estimation accuracy (R-2 = 0.91, RMSE = 11.41 %, and MAE = 6.39 %) was achieved. We then applied the algorithm to 18 years of MODIS data (2000-2017) to generate a time series of surface water fraction maps at an 8 d interval for the Mediterranean. From these maps we derived metrics including the mean annual maximum, the standard deviation, and the seasonality of surface water. The dynamic surface water extent estimates from MODIS were compared with the results from GSW and water level data measured in situ or by satellite altimetry, yielding similar temporal patterns. Our dataset complements surface water products at a fine spatial resolution by adding more temporal detail, which permits the effective monitoring and assessment of the seasonal, inter-annual, and long-term variability of water resources, inclusive of small water bodies.
机译:关于地表水分布的详细知识及其变化对水管理和生物多样性保护具有很高的重要性。欧洲委员会联合研究中心(JRC)开发的全球地表水(GSW)的地表水(如全球地表水(GSW)数据集)的土地上的评估可能不会在具有相当大的云覆盖期间在几个月内捕获地表水的重要变化。这导致Landsat记录中的大型时间间隙,以防止对地表水动态的准确评估。在这里,我们表明,中等分辨率成像光谱仪(MODIS)传感器的频繁全球采集可以补偿这种缺点,另外还可以在细时分辨率下进行表面水的变化。为了考虑比MODIS细胞小的水体,我们开发了一种基于规则的基于规则的回归模型,用于从MODIS(MCD43A4)估计从500m Nadir反射产品的表面水分。该模型受到GSW每月水历史数据集进行培训和评估。达到了高估计精度(R-2 = 0.91,RMSE = 11.41%和MAE = 6.39%)。然后,我们将算法应用于18年的MODIS数据(2000-2017),以在8 d间隔为地中海的8 d间隔产生一系列表面水分分数图。来自这些地图,我们派生了指标,包括平均年度最大值,标准偏差和地表水的季节性。将Modis的动态表面水范围估计与原位测量的GSW和水位数据的结果进行比较,或者通过卫星高度测量,产生类似的时间图案。我们的数据集通过添加更多临时细节来补充表面水产品,允许有效监测和评估水资源的季节性,年度年度和长期变异性,包括小水体。

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