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Influence of Climate Variability on Seasonal Rainfall Patterns in South-Western DR Congo

机译:气候变化对刚果民主共和国西南部季节性降雨方式的影响

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Climate variability in DR Congo in general and in the Kongo Central Province in particular is well established. However, rains related to variables such as frequency of rainy days and duration of the rainy seasons was generally very little studied. This study aims to investigate the influence of the climate event on rainfall patterns in the south-western of the DRC. This is firstly to characterize the climate event from the analysis of the air temperature, the frequency of rainy days and duration of the rainy seasons. Furthermore compare the normal monthly rainfall over the period 1962- 2012 to clear the behavior of seasonal rainfall patterns. Climate variability is manifested by temporal dynamic regressive temperatures, annual rainfall and a decrease in the number of rainy days. A temperature increase of around 1℃?was observed fr om 1992 and the thermal peak was recorded in 1994 (>28℃). The highest rainfall was recorded in 2006 (>2400 mm). These variabilities cause short periods of intense rainfall leading to early droughts of the end of season.
机译:刚果民主共和国总体而言,特别是金戈中央省的气候变异性已得到充分证实。但是,与变数有关的降雨,例如雨天的频率和雨季的持续时间,通常很少进行研究。这项研究旨在调查气候事件对刚果(金)西南部降雨模式的影响。首先,这是通过分析气温,雨天的频率和雨季的持续时间来表征气候事件的。此外,比较1962-2012年期间的正常月降雨量以清除季节性降雨模式的行为。气候变化表现为时间动态回归温度,年降水量和雨天数的减少。 1992年前后观测到温度升高了1℃左右,并在1994年创下了热峰值(> 28℃)。 2006年的降雨量最高(> 2400 mm)。这些变化会导致短时强降雨,从而导致季末早期干旱。

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