Modeling of rain fields at large scale

N. Jeannin, L. Feral, H. Sauvageot, L. Castanet, J. Lemorton
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引用次数: 3

Abstract

This paper describes the modeling of rain fields at small (size of a rain cell) mid (100times100 km2) and very large scale (4000times4000 km2). The methodology lies on a cellular description of rain fields by HYCELL Mid-scale fields are generated so that they account for local climatology and for spatial repartition of rain cells deduced from radar data. Very large scale fields are generated in two steps. First rainy areas are determined by thresholding a stationary Gaussian random field. In each point of the field, the probability of rain apparition is the one recommended by ITU and the covariance function is determined in order to reproduce the one observed by meteorological radar. Then rain intensity for rainy area is determined by applying mid-scale model to each mid-scale rainy area. Rain fields simulated are turned into attenuation fields and compared with ITU-R recommendations and radar observations
大尺度雨场模拟
本文描述了小尺度(一个雨单体的大小)、中尺度(100 × 100 km2)和超大尺度(4000 × 4000 km2)的雨场模拟。该方法基于HYCELL对雨场的单元描述,生成中尺度场,以便它们考虑当地气候和从雷达数据推断出的雨场的空间重新划分。超大规模的字段分两步生成。首先,通过设定平稳高斯随机场的阈值来确定多雨地区。在场地的每个点上,降雨的概率是ITU建议的概率,并确定协方差函数,以便再现气象雷达观测到的概率。然后对每个中尺度雨区应用中尺度模型,确定雨区降雨强度。模拟的雨场被转换成衰减场,并与ITU-R推荐值和雷达观测值进行比较
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