尼日利亚热带、山地和炎热半干旱气候的行星层递减率比较

D. Edokpa, P. Ede
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摘要

本研究评估了尼日利亚主要气候带的行星层递减率模式。从Era-Interim再分析数据中心获得了6年(2010-2015年)大气压力水平在1000毫巴到850毫巴之间的气温数据。数据在6小时天气时(0000H、0600H、1200H和1800H)以0.125格点分辨率检索。结果表明,各气候带对流层低层均存在正递减率。年平均递减率条件为:热带湿区(哈科特港)-5.6 oC/km;双模式热带大陆带(埃努古)5.8℃/km;山地带(Jos) -6.5℃/km;单模式热带大陆带(卡诺)-6.6℃/km;热半干旱区(迈杜古里)-6.6℃/km。这一平均值表明,渐变速率接近饱和绝热渐变速率(SALR)。各气候带的日平均观测结果表明,下午和过渡时期的日较差率高于其他时段,并从沿海地区向北增加。白天气温下降率最高的季节为12月至5月(即5.8-9.5℃/公里),6月至11月略有下降。整个地区在黎明期间观测到的正递减率范围为-1.8 - -5.9 oC/km,这表明红外辐射仍在释放,并受到尼日利亚表层特征的能量较低的机械湍流的影响。这也表明全球变暖是真实的,而且影响很大。研究结果表明,整个区域普遍存在条件不稳定性,因此,行星层环境将具有缓慢到中等的分散潜力,并且需要引入强有力的机制来提升排放。建议工业烟囱高度在50米以上,以增强高空排放的扩散。
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Planetary Layer Lapse Rate Comparison of Tropical,Montane and hot Semi-Arid Climates of Nigeria
This study assessed the pattern of planetary layer lapse rate across the major climate belts of Nigeria. Six years’ data (2010-2015) for air temperature values between 1000 mbar and 850 mbar atmospheric pressure levels were acquired from Era-Interim Re-analysis data centre. The data was retrieved at 6-hourly synoptic hours: 0000H, 0600H, 1200H and 1800H at 0.125o grid resolution. Results showed that the lower tropospheric layers throughout the various climate belts has a positive lapse rate. Findings also revealed that the average annual lapse rate condition were: Tropical wet zone (Port Harcourt) -5.6 oC/km; Bi-modal Tropical continental zone (Enugu) 5.8 oC/km; Montane zone (Jos) -6.5 oC/km; Mono-modal Tropical continental zone (Kano) -6.6 oC/km; and Hot semi-arid zone (Maiduguri) -6.6 oC/km. This average values presents the lapse rates to be close to the Saturated Adiabatic Lapse Rate (SALR). Average diurnal results for the climate belts showed that lapse rate is higher during the afternoon and transition periods than the rest periods and increases from the coastal areas northward. The seasonal periods of highest lapse rates during the day time are from December – May (i.e. 5.8-9.5 oC/km) with slight decrease from June – November. The positive lapse rate of range -1.8 –    -5.9 oC/km observed during the period of dawn across the entire region showed that infrared radiation was still being released and modified by less energetic mechanical turbulence that characterizes the surface layer across Nigeria. This also indicates that global warming is real and in substantial effect. The study findings imply that conditional instability prevailed over the entire region, therefore, the planetary layer environment will be of slow to moderate dispersive potential and will require forceful mechanism to lift emissions are introduced into it. It is recommended that industrial stacks are above 50 m to enhance the dispersion of emissions aloft.
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