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Estimation of Precipitation Evolution from Desert to Oasis Using Information Entropy Theory: A Case Study in Tarim Basin of Northwestern China

机译:基于信息熵理论的沙漠到绿洲降水演变估算-以西北塔里木盆地为例

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The cold-wet effect of oasis improves the extreme natural conditions of the desert areas significantly. However, the relationship between precipitation and the width of oasis is challenged by the shortage of observed data. In this study, the evolution of annual precipitation from desert to oasis was explored by the model establishment and simulation in Tarim Basin of northwestern China. The model was developed from the principle of maximum information entropy, and was calibrated by the China Meteorological Forcing Dataset with a high spatial resolution of 0.1° from 1990 to 2010. The model performs well in describing the evolution of annual precipitation from the desert to oasis when the oasis is wide enough, and the R 2 is generally more than 0.90 and can be up to 0.99. However, it fails to simulate the seasonal precipitation evolution because of the non-convergence solved by nonlinear fitting and the unfixed upper boundary condition solved by the least square method. Through the simulation with the parameters obtained from the nonlinear fitting, the basic patterns, four stages of precipitation evolution with the oasis width increasing, are revealed at annual scale, and the current stages of these oases are also uncovered. Therefore, the establishment of the model and the simulated results provide a deeper insight from the perspective of informatics to understand the regional precipitation evolution of the desert–oasis system. These results are not only helpful in desertification prevention, but also helpful in fusing multisource data, especially in extreme drought desert areas.
机译:绿洲的冷湿效应显着改善了沙漠地区的极端自然条件。然而,降水和绿洲宽度之间的关系受到观测数据缺乏的挑战。通过建立和模拟中国西北塔里木盆地的模式,探索了从沙漠到绿洲的年降水量演变。该模型是根据最大信息熵原理开发的,并通过1990年至2010年的中国气象强迫数据集进行了校准,具有0.1°的高空间分辨率。该模型在描述从沙漠到绿洲的年降水量变化方面表现出色当绿洲足够宽时,R 2通常大于0.90且可以高达0.99。然而,由于非线性拟合求解的非收敛性和最小二乘法求解的不固定上限边界条件,因此无法模拟季节性降水的演变。通过利用非线性拟合得到的参数进行模拟,以年尺度揭示了随着绿洲宽度增加而降水演变的四个基本阶段,并且也揭示了这些绿洲的当前阶段。因此,模型的建立和模拟结果从信息学的角度提供了更深入的了解,以了解荒漠-绿洲系统的区域降水演变。这些结果不仅有助于防治荒漠化,而且有助于融合多源数据,尤其是在极端干旱的沙漠地区。

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