首页> 外文期刊>International Journal of Climatology: A Journal of the Royal Meteorological Society >Possible impact of climate change on future extreme precipitation of the Oldman, Bow and Red Deer River Basins of Alberta
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Possible impact of climate change on future extreme precipitation of the Oldman, Bow and Red Deer River Basins of Alberta

机译:气候变化可能对艾伯塔省奥尔德曼河,鲍德河和红鹿河流域未来极端降水的影响

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The impact of climate change on extreme precipitation events in the Oldman (ORB), Bow, (BRB) and Red Deer (RRB) River Basins of southern Alberta, Canada, was assessed using six extreme climate indices for the rainy period of May-August (MJJA), and 9-km resolution Special Report on Emission Scenarios (SRES) A2 and A1B climate scenarios of four Coupled Model Intercomparison Project Phase 3 (CMIP3) Global Climate Models (GCMs) dynamically downscaled by a regional climate model, MM5. R95p of the three study sites showed an increase of 4% for the 2050s (2041-2070) and 10% for the 2080s (2071-2100) period, whereas R99p increased by 39% (2050s) and 42% (2080s) which suggest a projected increase in the volume of precipitation expected in future very wet and particularly extremely wet days. Similarly, R20mm, P30yr, RX1day and RX5day are also projected to increase by about 15% by the mid-and late 21st century in the three study sites. However, compared to BRB and RRB, ORB located in the southernmost part of the study site is projected to undergo a relatively higher increase in both temperature and precipitation intensity, which is assessed in terms of indices such as P30yr, RX1day and RX5day. On the other hand, RRB and BRB are projected to experience higher increase in R20mm, which suggest a relatively higher increase in the number of very heavy precipitation days projected for these two basins. Overall, these results suggest that in the 2050s and 2080s, southern Alberta will be expected to experience more frequent and severe intensive storm events in the MJJA season that could potentially increase the risk of future flooding in this region.
机译:使用五月至八月雨季的六个极端气候指数评估了气候变化对加拿大艾伯塔省南部的奥尔德曼(ORB),鲍尔(BRB)和红鹿(RRB)流域的极端降水事件的影响。 (MJJA),以及9公里分辨率的“排放情景​​(SRES)A2和A1B气候情景特别报告”,其中四项耦合模型比对项目第三阶段(CMIP3)全球气候模型(GCM)由区域气候模型MM5动态缩小。三个研究地点的R95p在2050年代(2041-2070)增长了4%,在2080s(2071-2100)时期增长了10%,而R99p增长了39%(2050s)和42%(2080s),这表明预计未来非常潮湿,尤其是非常潮湿的日子,降水量将增加。同样,在三个研究地点,到20世纪中叶后期,R20mm,P30yr,RX1day和RX5day也预计将增加约15%。但是,与BRB和RRB相比,位于研究地点最南端的ORB预计温度和降水强度都会相对较高地增加,这可以通过P30yr,RX1day和RX5day等指标来评估。另一方面,RRB和BRB的R20mm预计会出现更高的增加,这表明这两个盆地的非常重的降水天数预计会相对增加。总体而言,这些结果表明,在2050年代和2080年代,预计艾伯塔省南部在MJJA季节将经历更频繁,更严重的强风暴事件,这有可能增加该地区未来洪水的风险。

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