Towards Mapping Suitable Areas for Weather Modification in East Africa Community

J. Ngaina, N. J. Muthama, Ininda Joseph Mwalichi, Opere Alfred Owuor
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引用次数: 2

Abstract

In order to map suitable areas for weather modification in East Africa Community (EAC), investigations were performed to determine spatio-temporal variability and relationship of aerosol, clouds and precipitation during March- April-May (MAM) and October-November-December (OND). Principal Component Analysis (PCA), Hybrid Single- Particle Lagrangian Integrated Trajectory (HYSPLIT) and Multivariate Regression Analysis (MRA) were used. Identification of near homogeneous zones of Aerosol Optical Depth (AOD), Fine Mode Fraction (FMF), Cloud Top and 3B42 Tropical Rainfall Measuring Mission (TRMM) yielded 13 (14), 20 (18), 11 (10) and 16 (17) significant Principal Components (PCs) for MAM (OND) with explained variance greater than 57%. Aerosols and clouds had positive relationship with precipitation in areas with strong factor loadings. MRA indicated independence of variables used and normality in the model residuals. Backward trajectory analysis indicated differences in origins of transported particles in the atmosphere with strong vertical mixing inlands with mixed aerosols resulting due to mountain blocking systems accounted for enhanced rainfall. Enhanced rainfall was attributed to highly varied AOD and unaffected FMF in the atmosphere. Locations east and west EAC with mean temperatures greater than -10°C were unsuitable for cloud seeding while central EAC region along the great rift-valley and coastal Tanzania exhibited optimal temperatures suitable for cloud seeding. Successful precipitation enhancement will increase available fresh water sources and thus alleviate existing and projected water stress.
东非共同体人工影响天气适宜区域制图研究
为了确定东非共同体(EAC)适宜人工影响天气的区域,对3 - 4 - 5月(MAM)和10 - 11 - 12月(OND)期间气溶胶、云层和降水的时空变化及其关系进行了调查。采用主成分分析(PCA)、混合单粒子拉格朗日积分轨迹分析(HYSPLIT)和多元回归分析(MRA)。对气溶胶光学深度(AOD)、精细模式分数(FMF)、云顶和3B42热带降雨测量任务(TRMM)的近均匀区进行识别,MAM (OND)的显著主成分(pc)分别为13(14)、20(18)、11(10)和16(17),解释方差大于57%。在因子负荷较强的地区,气溶胶和云与降水呈正相关。MRA表示所使用变量的独立性和模型残差的正态性。反向轨迹分析表明,由于山地阻塞系统导致的强垂直混合内陆和混合气溶胶在大气中输送颗粒的来源不同,这是降雨增强的原因。降雨增强归因于大气中高度变化的AOD和未受影响的FMF。东非东部和西部平均气温大于-10℃的地区不适宜人工降雨,东非中部沿大裂谷和坦桑尼亚沿海地区适宜人工降雨。成功地增加降水将增加可用的淡水资源,从而减轻现有的和预计的水压力。
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