塞内加尔雨季起始条件的特点:突出作物生长的制约因素。

Mame Balla Ndiaye, B. Sine, Diariétou Sambakhé, Amadou Oury Diallo, Bertrand Muller, Modou Sene, Sousssou Sambou
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引用次数: 0

摘要

塞内加尔雨季开始时的气候多变,导致播种后长期干旱,许多作物歉收。本研究的目的是分析塞内加尔不同地区雨季开始时的条件与早期作物成活率的关系。研究分析了从 1950 年到 2015 年 95 个站点的日降雨量数据库中确定的四个季节成分。这些季节成分是播种日期(Sowing)、雨季开始日期(Onset)、最长干旱期(DryMax)和播种后 30 天内的总降雨量(TotRain)。应用时间序列同质性测定的统计方法,如 Pettitt 检验、Buishand 检验、Von Newmann 检验和分段法来确定实际的断点,并获得最近的同质性时期来定义各站点的组成部分。结果表明,自 1950 年以来,这些成分在统计上没有发生显著变化。事实上,3%的站点显示了播种期断点,4%的站点显示了雨量断点,2%的站点显示了雨季开始期断点。雨季的开始呈东南-西北梯度。从 6 月下旬开始,播种期从该国最东南部地区开始,而第一波播种期则从 6 月下旬开始在东南部的中部地区进行。北部地区仍有可能出现具有重要季节性的 "假开始 "现象。在北部和中部地区,播种的早晚更多取决于干旱指数(DryMax)而非降雨指数(TotRain)。为了更好地控制雨季作物产量,有必要阐明早期降雨机制对雨季概况的影响。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Characterization of the starting conditions of the rainy season in Senegal: Highlighting the constraints of crop establishment.
The start of the rainy season in Senegal is characterized by critical variability, resulting in many crop failures after seed planting when a long dry spell occurs. The objective of this study is to characterize the starting conditions of the rainy season in different areas of Senegal in relation to crop success at the early stage. An analysis of four seasonal components determined from a daily rainfall database of 95 stations from 1950 to 2015. These seasonal components are the sowing date (Sowing), the Onset of the rainy season date (Onset), the length of the longest dry spell (DryMax), and the total rainfall (TotRain) during the 30 days after sowing. Statistical methods of time series homogeneity determination such as the Pettitt test, the Buishand test, the Von Newmann test, and the segmentation method have been applied to determine actual breakpoints and to obtain the most recent and homogeneous period to define the component in each site. The results indicate that these components have not exhibited statistically significant changes since 1950. Indeed, 3% of the stations show breakpoints for the Sowing, 4% for the TotRain, and 2% for the Onset. The start of the season follows a South East-North West gradient. It begins in the extreme South-East part of the country in the second decade of June while the first waves of sowing take place in the South-East center part from the second half of June. The north zone remains exposed to false start events with important seasonality. In the Northern and Central zones, the early or late character of the sowing passes more on the DryMax than the TotRain. It would be interesting to elucidate the effects of the rainfall regime at the early stage on the rainy season profile to gain better control of the pluvial crop yields.
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