尼日利亚气候区:变异性、趋势和年代中期数据分析(2010-2015 年)

D. Edokpa, P. Ede, Joshua Brown, A. J. Adeyemi, Isaac U Pukiche
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摘要

本研究根据 2010-2015 年期间 0 时、6 时、12 时和 18 时的 Era-Interim 数据,分析了尼日利亚四个气候域低层大气的昼夜天气模式。气候域包括哈科特港(热带海洋型)、埃努古(双模式热带大陆型)、乔斯(山地型)、卡诺(单模式热带大陆型)和迈杜古里(半干旱型)。研究结果表明,各地区的气温显示出较强的纬度位置,向北的天气模式更干燥、更炎热。哈科特港、埃努古、乔斯、卡诺和迈杜古里的昼夜平均气温分别为 23.2-26oC、23-29oC、26-32oC、26-34oC 和 26.6-34oC。平均太阳辐射量在中午 12 点达到峰值,各地区的值分别为 508 W/m2、639 W/m2、830 W/m2、905 W/m2、832 W/m2。平均风速向北增加,分别为 0.9-1.3m/s、2.0-2.5m/s、2.1-2.5m/s、2.4-3.0m/s 和 2.9-3.5m/s。风速的变化与各地区的地表特征有关。西南风主导沿海地区,而东南风/东北风主导干旱地区,雨季高峰期除外。沿海地区和北部地区的平均云量分别为 6-7 和 2-4。相对湿度表明,在任何特定时间,靠近影响源和热带间不连续面(ITD)位置的地区的大气条件较强。湿度值分别为沿海和北部地区的湿度值分别为 67-93% 和 31-71%。降雨量向北减少,为 200-46 毫米。降雨模式受气团来源地区的影响很大。这些地区包括靠近大量水体的地区、靠近撒哈拉沙漠的地区以及山区屏障的影响。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
The Nigeria climate zones: Variability, trends and analysis from era-interim data (2010-2015)
This study analyses diurnal weather patterns in the lower atmosphere across four climate domains in Nigeria from Era-Interim data for synoptic hours of 0000, 0600, 1200 and 1800 hours from 2010-2015. The climate domain includes: Port Harcourt (tropical maritime), Enugu (bi-modal tropical continental), Jos (montane), Kano (mono-modal tropical continental) and Maiduguri (semi-arid). Findings revealed that air temperature across the areas indicate strong latitudinal positions with drier and hotter weather pattern northwards. Average air temperature across diurnal hours were 23.2-26oC, 23-29oC, 26-32oC, 26-34oC and 26.6-34 oC for Port Harcourt, Enugu, Jos, Kano and Maiduguri. Average solar radiation peaked at 1200 noon with values 508 W/m2, 639 W/m2, 830 W/m2, 905 W/m2, 832 W/m2 for the areas. Average wind speed increases northwards, i.e. 0.9-1.3m/s, 2.0-2.5m/s, 2.1-2.5m/s, 2.4-3.0m/s and 2.9-3.5m/s respectively. The wind variation is due to the surface characteristics across the areas. Southwesterly winds dominated coastal zone while southeasterly/northeasterly winds dominated the arid zone except during periods of peak rainy season. Average cloud cover for the coastal and northern domains in oktas was: 6-7 and 2-4. Relative humidity shows that prevailing atmospheric conditions at any given time are stronger at the areas close to the sources of influence and the position of Intertropical discontinuity (ITD). Humidity values were: 67-93% and 31-71% for coastal and northern domains. Rainfall amount reduces northwards i.e. 200-46 mm. Rainfall pattern is significantly influenced by the air masses source regions. These regions include closeness to massive water bodies, proximity to Sahara Desert and effects of mountainous barriers.
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