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首页> 外文期刊>Australian geographical studies >An Assessment of the Influence of the Inter-Tropical Discontinuity on Inter-Annual Rainfall Characteristics in Nigeria
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An Assessment of the Influence of the Inter-Tropical Discontinuity on Inter-Annual Rainfall Characteristics in Nigeria

机译:尼日利亚热带间断性对年度降水特征的影响评估

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This study assessed the influence of the Inter-Tropical Discontinuity (ITD) on inter-annual rainfall characteristics in Nigeria between 1970 and 2000. This involved determining the strength and direction of the relationships between the total annual rainfalls in the extreme southern and northern parts of the country and the total annual rainfalls during the period of the Little Dry Season in southwestern Nigeria, and the surface locations of the ITD over Nigeria and some other factors that may impact ITD characteristics (such as the pressure differences between Azores, Libyan and St. Helena anticyclones and the sea surface temperature of the Gulf of Guinea). Results indicate that although the surface location of the ITD significantly accounts for rainfall inter-annual variability in Nigeria, it does so in the northern part of the country only. Pressure differences between the various anticyclones were observed to be another significant factor influencing inter-annual rainfall variability in the north. However, the influence of the sea surface temperature of the Gulf of Guinea on the rainfall characteristics in the northern region is ill-defined. It was also noted that the only factor influencing inter-annual variability in the Little Dry Season rainfall in the southwest and the total annual rainfalls in the south is the sea surface temperature of the Gulf of Guinea. The results obtained indicate that the total annual rainfalls in the north have significant positive relationships with the surface location of the ITD but significant negative relationships with the pressure differences between the Azores, Libyan and St. Helena anticyclones. The Little Dry Season rainfalls and total annual rainfalls in the south have significant positive relationships with the sea surface temperature of the Gulf of Guinea.
机译:这项研究评估了热带间断性(ITD)对1970年至2000年尼日利亚年间降雨特征的影响。这涉及确定该国南部和北部极端地区总年降雨量之间关系的强度和方向。该国以及尼日利亚西南部小旱季期间的年降雨量总量,以及尼日利亚境内ITD的地表位置和其他可能影响ITD特征的其他因素(例如亚速尔群岛,利比亚和圣约翰群岛之间的压力差)。海伦娜反气旋和几内亚湾的海面温度。结果表明,尽管ITD的地表位置显着说明了尼日利亚的降雨年际变化,但仅在该国北部确实如此。观测到各种反气旋之间的压力差是影响北部年际降水变化的另一个重要因素。然而,几内亚湾海面温度对北部地区降雨特征的影响尚不清楚。还注意到,影响西南小旱季降雨量和南部总年降雨量的年际变化的唯一因素是几内亚湾的海面温度。获得的结果表明,北部的年度总降雨量与ITD的表面位置具有显着的正相关关系,而与亚速尔群岛,利比亚和圣海伦娜反气旋之间的压力差具有显着的负相关关系。南部的小旱季降雨量和年总降雨量与几内亚湾的海面温度有着显着的正相关关系。

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