首页> 外文会议>American Society for Photogrammetry and Remote Sensing Annual Conference >COMPARISON OF CHANGES IN GROUNDWATER STORAGE USING GRACE DATA AND A HYDROLOGICAL MODEL IN CALIFORNIA'S CENTRAL VALLEY
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COMPARISON OF CHANGES IN GROUNDWATER STORAGE USING GRACE DATA AND A HYDROLOGICAL MODEL IN CALIFORNIA'S CENTRAL VALLEY

机译:利用加州中央山谷的恩典数据和水文模型对地下水储存变化的比较

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The Gravity Recovery and Climate Experiment (GRACE) measures gravity anomalies on earth to estimate changes in total water storage (TWS), and may be a useful tool for calculating changes in groundwater storage for California's agriculturally productive Central Valley region. Under current California law, well owners are not required to report groundwater extraction rates, making estimation of total groundwater extraction difficult. As a result, other groundwater change detection techniques are used to estimate changes in groundwater storage in the Central Valley aquifer. From October 2002 to September 2009, GRACE was used to measure changes in TWS for the Sacramento River Basin, and the San Joaquin River Basin (including the Tulare Lake Basin), which contain the Central Valley aquifer. Net groundwater storage changes were calculated from the changes in TWS by incorporating estimates for additional components of the hydrological budget including soil moisture, snow pack, and surface water storage. The changes in groundwater storage at the river basin and regional level (the two basins combined) were then compared to modeled values calculated using the California Department of Water Resources' Central Valley Groundwater-Surface Water Simulation Model (C2VSIM). At the regional level (the Central Valley aquifer) it was found that GRACE-derived estimates of groundwater change in storage produced comparable results to C2VSIM. However, at the river basin level (Sacramento and San Joaquin), GRACE-derived estimates were significantly different from those modeled by C2VSIM, highlighting the current limit of GRACE'S spatial resolution. This work has the potential to improve California's groundwater resource management at the regional level and in validating existing hydrological models for the Central Valley. The work also underscores the need for higher resolution satellite data that are applicable smaller scale management.
机译:重力恢复和气候实验(Grace)测量地球上的重力异常,以估计总水存储(TWS)的变化,并且可能是计算加州农业生产中央山谷地区地下水储存变化的有用工具。根据目前的加利福尼亚法律,井业主不需要报告地下水提取率,估计地下水的估计困难。结果,其他地下水变化检测技术用于估计中央山谷含水层地下水储存的变化。从2002年10月至2009年9月,恩典被用来衡量萨克拉门托河流域的TWS的变化,以及含有中央山谷含水层的圣Joaquin River盆地(包括Tulare Lake Basin)。通过纳入水文预算包括土壤水分,雪包和地表储存的水文预算的其他组成部分来计算净地下水储存变化。然后将地下水储存的变化与区域水平(两个盆地合并)与使用加利福尼亚水利中央地下水 - 表面水仿真模型(C2VSIM)计算的建模值进行比较。在区域一级(中央山谷含水层),发现储存的地下水变化的恩典衍生估计产生了与C2VSIM的可比结果。然而,在河流域水平(萨克拉门托和圣Joaquin),恩典衍生的估计与C2VSIM建模的估计显着不同,突出了恩典空间分辨率的当前限制。这项工作有可能在区域一级提高加州地下水资源管理,并验证中央山谷的现有水文模型。该工作还强调了对适用更小规模管理的更高分辨率卫星数据的需求。

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