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Rainfall variability in Congo-Brazzaville: 1932-2007

机译:刚果布拉柴维尔的降雨变异性:1932-2007年

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摘要

The interannual variability of rainfall amounts and rainy days is analysed from synoptic stations located in different climatic zones of Congo-Brazzaville over the common period 1932-2007. The annual and seasonal rainfall evolution is appreciated using standardized indices. Trends examined were based on the non-parametric Mann-Kendall test (the major synoptic stations point out alternative periods of anomalies-positive and negative). A majority of negative anomalies is recorded during the 1930s and 1940s. The decade 1950 shows mainly positive anomalies with the exception of 1958 which records a general precipitation deficit all across Congo. The decade 1960 is characterized by precipitation excess over the whole Congo. The decades 1980 and 1990 experience the largest rainfall deficit (about 10-20% below the long-term mean). The evolution of the precipitation at Brazzaville is particularly stable, although there are large positive anomalies during the 1990s. The transition between positive and negative anomalies decades is not uniform across Congo. The progressive non-parametric Mann-Kendall trend test shows that there is stability in the annual rainfall and rainy days over the southern area in the period 1932-2007. By contrast, the annual rainfall for the northern stations shows a significant decline since about the 1980s. In the south the decline is observable only in the evolution of the March-May seasonal rainfall. In most of the stations there is a precipitation increase during the September-November rainy season.
机译:从1932-2007年共同时期位于刚果布拉柴维尔不同气候带的天气站分析了降雨量和雨天的年际变化。年度和季节性降水量的变化可以通过标准化指标来体现。检验的趋势基于非参数Mann-Kendall检验(主要的天气观测站指出了异常的正反周期)。在1930年代和1940年代记录了大多数负异常。 1950年的十年主要表现为正异常,但1958年除外,该年记录了整个刚果的普遍降水不足。 1960年代的特征是整个刚果的降水过多。 1980年和1990年这十年是最大的降雨赤字(比长期平均值低约10-20%)。尽管在1990年代期间存在较大的正异常,但布拉柴维尔的降水演变特别稳定。在整个刚果,正异常异常和负异常异常之间的过渡是数十年的。渐进式非参数Mann-Kendall趋势检验表明,在1932-2007年期间,南部地区的年降雨量和雨天是稳定的。相比之下,自1980年代以来,北部气象站的年降雨量显着下降。在南部,下降只有在三月至五月的季节性降雨演变中才能观察到。在大多数气象站,九月至十一月的雨季降雨量增加。

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