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Characteristics of monsoon precipitation systems in and around Bangladesh

机译:孟加拉国及其周围地区的季风降水系统特征

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摘要

Characteristics of precipitation systems in and around Bangladesh are analysed using 6 years of radar data from the Bangladesh Meteorological Department (BMD). Precipitation systems are classified as arc, line, or scattered types according to their shape; then as small, medium, or large according to their length; and as stationary, slow, or fast according to their propagation speed. Arc-, line-, and scattered-type systems are found 230 (29%), 117 (15%), and 442 (56%) times, respectively, from April to September during the analysis period (2000-2005). These arc-, line-, and scattered-type systems have average speeds of 11.0, 7.1, and 5.8 m/s, horizontal lengths of 185, 184, and 268 km, and approximate lifetimes of 4.3, 4.0, and 4.8 h, respectively. Scattered-type systems dominate in the monsoon period (June, July, August, and September), while arc-type systems dominate in the pre-monsoon period (April and May). Line-type systems occur with nearly equal frequency in both periods. The monsoon systems are large and stationary or slow moving. In contrast, pre-monsoon systems are small and fast moving. Pre-monsoon systems propagate southeastward whereas monsoon systems propagate to the northeast, northwest, or southeast. A large number of systems occur in the southern, eastern, and northern parts of Bangladesh. Of the 442 scattered-type systems, 244 are scattered-type systems having wide areal coverage (SWAC), which extends out of radar range, and speeds too small to calculate. About 97% of SWACs develop during the monsoon period and contribute greatly to monsoon rainfall in this region.
机译:使用来自孟加拉国气象局(BMD)的6年雷达数据分析了孟加拉国及周边地区的降水系统特征。降水系统根据其形状分为弧形,直线形或分散形。然后根据其长度分为小,中或大;并根据它们的传播速度分为固定,慢或快。在分析期间(2000-2005年)从4月到9月,分别发现了弧型,线型和散布型系统230次(29%),117次(15%)和442次(56%)。这些弧形,线形和散布型系统的平均速度分别为11.0、7.1和5.8 m / s,水平长度分别为185、184和268 km,近似寿命分别为4.3、4.0和4.8 h 。散射型系统在季风期(6月,7月,8月和9月)中占主导地位,而弧型系统在季风前期(4月和5月)中占主导地位。线型系统在两个周期中的发生频率几乎相等。季风系统很大,静止或移动缓慢。相反,季风前系统体积小且移动迅速。季风前系统向东南传播,而季风系统向东北,西北或东南传播。孟加拉国的南部,东部和北部有大量系统。在442个分散型系统中,有244个是具有较宽的区域覆盖范围(SWAC)的分散型系统,它超出了雷达范围,并且速度太小而无法计算。季风期间约有97%的西南亚热带气旋形成,并对该地区的季风降雨做出了很大贡献。

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