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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岁序列的地表水分估计

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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 500 m nadir reflectance product from MODIS (MCD43A4). The model was trained and evaluated with the GSW monthly water history dataset. A high estimation accuracy (R2=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)开发的地表水(如全球地表水(GSW)的地表水评估,可能在几个月内捕捉地表水的重要变化,云覆盖率相当。这导致Landsat记录中的大型时间间隙,以防止对地表水动力学的准确评估。在这里,我们表明,适度分辨率成像光谱仪(MODIS)传感器的频繁全局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。为了考虑小于MODIS细胞的水体,我们开发了一种基于规则的回归模型,用于从MODIS(MCD43A4)从500米NADIR反射产品中估算表面水分。使用GSW每月水历史数据集进行培训和评估该模型。达到高估计精度(R2 = 0.91,RMSE = 11.41%,和MAE = 6.39%)。然后,我们将该算法应用于18岁的MODIS数据(2000-2017),以在地中海的8 d间隔内产生时间序列的表面水分分数图。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。我们的数据集通过加入更多的时间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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