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Spatial and Temporal Analysis of Precipitation over Iran Using Gridded Precipitation Data of APHRODITE

机译:使用APHRODITE的网格降水数据对伊朗降水进行时空分析

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In order to achieve risk management of water-related disasters such as droughts and floods in Iran, it is essential to obtain knowledge of the exact quantities of spatial and temporal precipitation over the long term. In this regard, this paper presents the results of monitoring precipitation on monthly, seasonal and annual timescales during the period of 1986-2006 (21 years) over Iran using a product of 0.5-degree-gridded data sets provided by the Asian Precipitation-Highly-Resolved Observational Data Integration (APHRODITE) Towards Evaluation of the Water Resources project, namely APHRO_ME_V003R1. Spatial distribution of mean seasonal and annual precipitation shows two rainfall peaks that extend from the northwest to the southeast along the Zagros Mountains and along the Caspian Sea and Alborz Mountains in the northern part of the country. With respect to a seasonal spatial analysis of rainfall over Iran, it is concluded that in winter, DJF (December- January- February), and spring, MAM (March-April-May), most precipitation occurs in the west, northwest and southwest along the Zagros Mountains, but in summer. JJA (Jun-July-August), and autumn, SON (September-October-November), most precipitation occurs along the southern Caspian Sea in the north. Annual and seasonal drought condition using APHRODITE data have showed that mean annual precipitation amount were low (drought condition) over Iran in 1989, 1990, 1991, 1992, 1996, 1998, 1999, 2000, 2001 and they are in accordance with Yazdani et al (2011)'s study about drought analysis over Iran.
机译:为了对与水有关的灾害(例如伊朗的干旱和洪水)进行风险管理,必须长期了解确切的时空降水量。在这方面,本文介绍了使用亚洲降水-高度观测资料提供的0.5度网格数据集对伊朗1986-2006年(21年)期间每月,季节性和年度时间尺度上的降水进行监测的结果。 -解析的观测数据集成(APHRODITE),用于水资源项目APHRO_ME_V003R1的评估。平均季节性和年降水量的空间分布表明,有两个降雨峰从西北向东南延伸,沿着Zagros山脉,以及沿着该国北部的里海和Alborz山脉。关于伊朗降水的季节性空间分析,可以得出结论,在冬季,DJF(12月至1月至2月)和春季,MAM(3月至4月至5月),大部分降水发生在西部,西北和西南部。扎格罗斯山脉沿线,但在夏天。 JJA(6月至7月至8月)和秋季SON(9月至10月至11月),大部分降水发生在北部的里海南部。使用APHRODITE数据得出的年度和季节性干旱状况表明,伊朗,1989、1990、1991、1992、1996、1998、1999、2000、2001年的年平均降水量较低(干旱状况),这与Yazdani等人的观点一致。 (2011年)关于伊朗干旱分析的研究。

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