Temperature Variability and Trends in Nzoia River Basin, Kenya

Ernest Othieno Odwori
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引用次数: 1

Abstract

Nzoia River Basin is one of the regions that is highly vulnerable to climate change in Kenya. Many attempts have been made to identify and quantify the impact of climate change on socio-economic sectors and ecosystems using global studies resulting into recommendations on policy changes aimed at generating sustainable mitigation and adaptation strategies. This top-down approach by using global studies lacks the required local and regional climate change specificities to address the regional and local climate change challenges. Temperature is one of the most important components of the climatic parameters widely measured as a starting point towards the apprehension of climate change courses. This study aims at filling the top-down approach knowledge gaps in Nzoia River Basin by assessing temperature variability and trends at three stations for the period 1979 to 2014, using Linear regression analysis and Mann-Kendall statistical test. Monthly maximum and minimum temperature data for Kitale, Kakamega and Eldoret stations was obtained from Kenya Meteorological Department, Nairobi, Kenya. The main findings reveal that Kakamega has highest temperatures, followed by Kitale and the lowest temperatures are found at Eldoret. This trend seems to go with altitude as the lowest temperatures are found at highest altitudes and highest temperatures at lowest altitudes. There are significant increases in annual temperatures for Kitale and Kakamega stations, with Kitale showing annual maximum temprature rising at 0.0006260 C/year; annual minimum temperature rising at 0.0011630 C/year and the annual mean temprature rising at 0.0008940 C/year. Kakamega shows annual maximum temperature rising at 0.0007710 C/year; annual minimum temperatures rising at 0.0004710 C/year and the annual mean temperatures rising at 0.0006230 C/year. Eldoret shows falling maximum temperature at - 0.002020 C/year; rising minimum temperature at 0.0008130 C/year and falling mean temperatures at - 0.001420 C/year. The results for Kitale and Eldoret stations show statistically significant trends whereas those for Kakamega station were statistically insignificant. Eldoret annual minimum temperatures are rising faster than the maximum whereas in Kakamega it’s the annual maximum temperatures that are rising faster than the minimum. Kitale and Kakamega show annual mean temperatures rising at about 0.10C per century which compares well with IPCC Third Assessment Report estimated global warming rate of 0.6 0C during the twentieth century and other studies from the African continent and East African region.
肯尼亚Nzoia河流域的温度变化和趋势
Nzoia河流域是肯尼亚最容易受到气候变化影响的地区之一。为了确定和量化气候变化对社会经济部门和生态系统的影响,已经进行了许多尝试,利用全球研究得出了旨在制定可持续缓解和适应战略的政策变化建议。这种利用全球研究的自上而下的方法缺乏应对区域和地方气候变化挑战所需的地方和区域气候变化特异性。温度是广泛测量的气候参数中最重要的组成部分之一,是理解气候变化过程的起点。本研究利用线性回归分析和Mann-Kendall统计检验,对Nzoia河流域1979 - 2014年3个站点的温度变化趋势进行了评估,旨在填补自上而下方法的知识空白。Kitale、Kakamega和Eldoret站的月最高和最低气温资料来自肯尼亚内罗毕的肯尼亚气象部门。主要发现显示卡卡梅加的温度最高,其次是基塔莱,而埃尔多雷特的温度最低。这种趋势似乎与海拔高度有关,因为海拔最高的地方温度最低,海拔最低的地方温度最高。基塔莱站和卡卡梅加站年最高气温显著上升,基塔莱站年最高气温上升0.0006260℃/年;年最低气温上升幅度为0.0011630℃/年,年平均气温上升幅度为0.0008940℃/年。Kakamega的年最高温升为0.0007710℃/年;年最低气温上升0.0004710℃/年,年平均气温上升0.0006230℃/年。埃尔多雷特的最高温度为- 0.002020℃/年;最低气温上升0.0008130℃/年,平均气温下降- 0.001420℃/年。基塔莱和埃尔多雷特站的结果在统计上有显著的趋势,而卡卡梅加站的结果在统计上不显著。埃尔多雷特的年最低气温比最高气温上升得快,而卡卡梅加的年最高气温比最低气温上升得快。Kitale和Kakamega显示,年平均气温每世纪上升约0.10℃,这与IPCC第三次评估报告估计的20世纪全球变暖率0.6℃以及非洲大陆和东非地区的其他研究结果相当。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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