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首页> 外文期刊>Journal of Hydrology >Satellite-based estimation of watershed groundwater storage dynamics in a freeze-thaw area under intensive agricultural development
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Satellite-based estimation of watershed groundwater storage dynamics in a freeze-thaw area under intensive agricultural development

机译:集约农业发展下冻融区流域地下水储量动态的卫星估算

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Understanding the temporal-spatial characteristics of groundwater storage is critical for agricultural planning and management in the future, thereby causing more challenges in water resource management. However, the special hydrological features of the snow water equivalent, soil moisture, and total canopy water storage in the freeze-thawing agricultural area requires the innovative methods for the water resource analysis. The watershed land cover variation and the expanding pattern of the farmlands over a decade were identified using the TM-Landsat series data. Combined with the traditional measurements of the water resource, the monthly gravity field data from the Gravity Recovery And Climate Experiment (GRACE) was validated and applied. The water resources distribution based on the remotely sensed data demonstrated that the forest in the watershed center had a larger amount of water storage. The inter-annual and seasonal variability of total water storage (TWS) over the agricultural area was analyzed and the higher value appeared in the thawing period of April. The correlations of the TWS stream flow, soil moisture and snow water equivalent with precipitation were all identified. The precipitation was the dominant factor for the watershed TWS and the groundwater dynamics. Under the similar precipitation condition, the lower groundwater storage in recent years was the consequence of the expanding of farmland. The watershed averaged decrease rate of groundwater level from 2003 to 2012 was 1.06 mm/year, which was much lower than the rates in other agricultural areas. The freeze-thawing process with smelt snow and rainfall in summer had more time and chance to recharge the groundwater resource and provided the sustainable water resource. This study proved that the application of GRACE was an effective method for the temporal-spatial estimation of the TWS anomalies in the freeze thawing agricultural area. (C) 2016 Elsevier B.V. All rights reserved.
机译:了解地下水储量的时空特征对于未来的农业规划和管理至关重要,因此给水资源管理带来了更多挑战。但是,冻融农业地区的雪水当量,土壤湿度和冠层总储水量的特殊水文特征要求采用新颖的水资源分析方法。使用TM-Landsat系列数据确定了十年来流域的土地覆盖变化和农田的扩展格局。结合传统的水资源测量方法,对重力恢复和气候实验(GRACE)的月重力场数据进行了验证和应用。基于遥感数据的水资源分配表明,流域中心的森林蓄水量较大。分析了农业地区总储水量(TWS)的年际和季节变化,在四月的解冻期出现了较高的储水量。都确定了TWS流量,土壤水分和雪水当量与降水的相关性。降水是影响分水岭水位和地下水动力学的主要因素。在相似的降水条件下,近年来地下水蓄水量减少是农田扩张的结果。 2003年至2012年,流域平均地下水位下降速度为1.06毫米/年,远低于其他农业地区的下降速度。夏季融雪和降雨的冻融过程有更多的时间和机会来补充地下水资源并提供可持续的水资源。这项研究证明了GRACE的应用是一种有效的时空估算冻融农业地区TWS异常的时空方法。 (C)2016 Elsevier B.V.保留所有权利。

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