2006-2100年埃塞俄比亚韦布河流域年降水和气温变化趋势

A. B. Serur
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摘要

基于GFDL-ESM2M、CanESM2和GFDL-ESM2G地球系统模型的预测,研究了2006-2100年韦布河流域代表性浓度路径(RCP) 2.6/4.5/8.5情景下的年降水量、最高气温和最低气温的变化特征。结果表明,与基线情景(1981-2005年)相比,近期(2011-2040年)、中期(2041-2070年)和长期(2071-2100年)降水、最高气温和最低气温均将上升。在所有三个时间段内,GFDL-ESM2M预测的增量都比GFDL-ESM2G和CanESM2预测的增量大。RCP8.5情景下的降水、最高温度和最低温度的变率均高于RCP4.5和RCP2.6情景。渭河流域降水、最高气温和最低气温的时空变化特征表明,21世纪渭河流域干旱或洪涝灾害的发生频率可能会增加。
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TRENDS AND VARIABILITIES IN ANNUAL PRECIPITATION AND TEMPERATURE DURING 2006–2100 IN THE WEYB RIVER BASIN, ETHIOPIA
This study investigates on variabilities in annual precipitation, maximum temperature, and minimum temperature within the Weyb River basin during 2006–2100 under representative concentration pathway (RCP) 2.6/4.5/8.5 scenarios based on predictions of three Earth System Models (GFDL-ESM2M, CanESM2, and GFDL-ESM2G). Our results showed that precipitation, maximum temperature, and minimum temperature would rise in the near term (2011–2040), the medium term (2041–2070), and the long term (2071–2100) as compared to the baseline scenario (1981–2005). The larger increments are predicted by GFDL-ESM2M than those by GFDL-ESM2G and CanESM2 in all three time periods. The variabilities of precipitation, maximum temperature, and minimum temperature are predicted to be higher under RCP8.5 scenario than those under RCP4.5 or RCP2.6 scenario in simulations of all three ESMs. Results also revealed that there would be significant spatiotemporal variations in precipitation, maximum temperature, and minimum temperature within the Weyb River basin, which implies that the basin would possibly experience droughts or floods more frequently during the 21st century.
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