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Estimating the influence of precipitation variability by considering effect of middle atmosphere parameters on lower atmosphere over upper Blue Nile basin in Ethiopia

机译:估算沉淀变异性对埃塞俄比亚上蓝尼罗河盆地较低大气影响的影响

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Precipitation over upper Blue Nile basin (UBNB) exhibits complex variability because of topographical features and the variability in tropopause temperature. The factors affecting its temporal and spatial distribution are not well known over the UBNB.Since precipitation is influenced by middle and lower atmosphere parameters such as greenhouse gases (carbon dioxide and methane), ozone concentration, incident solar radiation, gravity wave dispersion, cloud cover, and temperature. There is no study conducted to estimate precipitation variability using these parameters. In this study, we investigated the influence of precipitation variability by considering the effect of the middle atmosphere on lower atmospheres over UBNB in Ethiopia. Most of the data sets used in this study are derived from the European Centre for Medium-range Weather Forecast (ECMWF), in situ measurements and the Global monitoring division of National Oceanic and Atmospheric Administration. The results indicate that the correlation between ECMWF and in situ precipitation and temperature data is 0.82 and 0.32, respectively. The maximum ozone concentration is found during the summer season (6.2 x 10~(-3) kg m~(-2)). In this season, precipitation and cloud cover has positive correlations and both are negative correlations with temperature and incident solar radiation. The observed positive trend in temperature is associated with the enhancement of greenhouse gases. Cloud cover and ozone is quite useful for reduced incident solar radiation. Ozone is increased with temperature for all seasons except winter. Gravity wave dispersion affects the spatial distributions of temperature. Finally, we conclude that precipitation is directly influenced by temperature and incident solar radiation and indirectly affected by gravity waves, ozone concentration, and greenhouse gases. To draw a better conclusion, further study is needed with water vapor nuclei on precipitation variability in addition to middle atmospheric parameters.
机译:上蓝尼罗河盆地(UBNB)上的降水,由于地形特征和对流度温度的可变性,具有复杂的变化。影响其时间和空间分布的因素在UBNB中没有公知。沉淀因温室气体(二氧化碳和甲烷),臭氧浓度,入射太阳辐射,重力波分散,云盖,云覆盖而受到中下大气层的影响和温度。使用这些参数估计降水变异性没有研究。在这项研究中,我们通过考虑中间大气在埃塞俄比亚UBNB的较低气氛上的影响来调查降水变异性的影响。本研究中使用的大多数数据集源自欧洲中等地区天气预报(ECMWF)中心,原位测量和国家海洋和大气管理局的全球监测划分。结果表明,ECMWF与原位沉淀和温度数据之间的相关性分别为0.82和0.32。在夏季发现最大臭氧浓度(6.2×10〜(-3)kg m〜(-2))。在本赛季中,降水和云盖具有正相关性,两者都是与温度和事件太阳辐射的负相关性。观察到的温度阳性趋势与温室气体的增强有关。云盖和臭氧对于减少事件太阳辐射非常有用。除了冬季外,臭氧增加了所有季节的温度。重力波色散影响温度的空间分布。最后,我们得出结论,降水直接受温度和事件太阳辐射的影响,并受重力波,臭氧浓度和温室气体间接影响。为了得出更好的结论,除了中部大气参数外,还需要进一步研究水蒸气沉淀可变性。

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