坦桑尼亚桑给巴尔地区10 - 12月季节降雨变率及其季节开始和结束日期的测定

Riziki Ali Suleiman, Wang Wen, Jonah Kazora, Elias Julius Lipiki
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引用次数: 0

摘要

本研究旨在确定坦桑尼亚桑给巴尔的10月至12月(OND)降雨变异性、季节性开始和停止日期。该研究使用了从六个气象站获得的10年日降雨量(2012-2021年)和30年月度降雨量数据集。其他气候参数包括海温(SST)、风、相对湿度和垂直速度,时间分辨率为30年(1992-2021)。利用气候平均值和经验正交函数(EOF)分析降水季节变异,利用累积百分比异常计算降水开始和停止日期。采用复合分析方法研究了大气环流异常与冬季降水的关系。研究表明;OND季的特点是地区间降水呈正常到中等的变化,峰值出现在11月(季中)。尽管两个岛屿略有不同,平均开始日期发生在10月的第三个十年(22日至25日),结束日期发生在12月的第二个十年(即10日至12日),表明最长持续时间为55- 60天,形成了一个短雨周期。湿润年海温、风、相对湿度和垂直速度的大气环流异常与源自刚果盆地的低层不稳定湿风有关。这些异常是有组织的,并与来自印度洋的海洋东北风(主要在坦桑尼亚北部海岸,包括桑给巴尔)汇合,成为该季节降雨的潜在原因,而在干旱年份,由于该地区的干燥,风会偏离。结果表明,西北向西风、东风和东南气流的辐合(辐散)对桑给巴尔及其周边早(晚)湿(干)的形成有重要影响。研究结果将有助于改进短雨季节起停预报,改善桑给巴尔和整个坦桑尼亚的社会经济活动。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Determination of October to December Seasonal Rainfall Variability, its Seasonal Onset and Cessation Dates in Zanzibar, Tanzania
This study aimed in determining the October to December (OND) rainfall variability, seasonal onset and cessation dates in Zanzibar, Tanzania. The study used 10 years daily rainfall (2012–2021) and 30 years monthly rainfall datasets obtained from six meteorological stations. Other climate parameters of Sea Surface Temperature (SST), Winds, Relative Humidity and Vertical Velocity having temporal resolution of 30 years (1992-2021) were also used. Rainfall seasonal variability was analyzed using Climatological mean and Empirical Orthogonal Function (EOF) analysis, onset and cessation dates was calculated using Cumulative percentage anomalies. The composite analysis was taken to examine the atmospheric circulation anomalies associated with OND seasonal rainfall. The study revealed that; OND season is characterized by normal to moderate rainfall variations from region to region with its peak marked at November (mid-season). Despite the slight differences over both Islands, average onset dates occur on third dekade of October (22nd – 25th) and cessation dates on the second dekade of December (i.e.10th -12th), indicating a maximum duration of 55- 60 days and makes a cycle of the short rains. The atmospheric circulation anomalies of SST, Winds, Relative Humidity and Vertical Velocity during wet years are linked with low level unstable moist winds originated from Congo basin. These anomalies are organized and converges with maritime north easterly winds from the Indian Ocean (mostly over the northern coast of Tanzania, including Zanzibar) and becoming a potential cause for rainfall during the season, while during dry years, the winds diverge as a result of dryness over the region. Therefore the results indicates that convergence (divergence) of the northwesterly to westerly, easterly and southeasterly flow contributed to the early(late) wetness (dryness) over Zanzibar and its surroundings. The study results will help to enhance the improvement of short rains seasonal onsets and cessations forecasts and improve the socio - economic activities over Zanzibar and Tanzanian at large.
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