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Trends of Precipitation and Air Temperature in Northern California under SRES Scenarios

机译:SRES情景下北加州北加州降水和空气温度趋势

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In this study, recent precipitation trends based on CCSM3-based MM5 simulations were investigated against PRISM-based precipitation for 11 years from water year 2000 to water year 2010 for 8 watersheds in Northern California. Six precipitation projections (A1B1, A2, B1, A1FI, Ensemble 1 and Ensemble2) were used for this study. In general, the case of Ensemble2 shows the most realistic trends against PRISM precipitation, especially for last 5 years, and is similar to PRISM in total volume of precipitation for 11 years. However, the case of A1FI also shows the realistic trends in mountainous watersheds (UFRW, ARW and YBW). It means that the precipitation under A1FI scenario is also important for future climate change impact study. Less precipitation was found under A1B and A1FI scenarios and more precipitation was found under A2 scenario. Although precipitation under Bl scenario is realistic compared to other scenarios (A1B, A2 and A1FI), the most realistic scenario is Ensemble2 (ensemble average of 4 scenarios). However, it was found that the precipitation difference against PRISM precipitation is locally different for all scenarios. Through the analyses for the extreme precipitation between the control run for 20th century and the projections for 21st century under CCSM3 gas emission scenarios, the extreme precipitation not only under A1B, A2 and B1 but also under A1FI scenario was much frequently found than historical period. It means that the A1FI scenario is also important to assess the future climate change impacts not only for water resources but also extreme floods.
机译:在这项研究中,研究了基于CCSM3的MM5模拟的最新降水趋势,从2000年到2010年到2010年到2010年的北加州8分水岭的棱镜沉淀到2010年的普遍沉淀。用于本研究使用六种沉淀突起(A1B1,A2,B1,A1FI,集合1和Ensemble2)。一般来说,Ensemble2的情况表明,棱镜降水的最逼真趋势,特别是在过去5年中,与棱镜相似,沉淀总量11年。然而,A1FI的情况也显示了山区流域(UFRW,ARW和YBW)的现实趋势。这意味着A1FI场景下的降水对未来的气候变化影响研究也很重要。在A1B下发现少沉淀,并在A2场景下发现了A1FI场景和更多的降水。尽管与其他场景(A1B,A2和A1FI)相比,BL情景下的降水是现实的,但最具现实的情景是Ensemble2(4场景的集合平均值)。然而,发现对所有场景的棱镜降水的降水差异是局部不同。通过分析到20世纪的控制运行之间的极端降水量和21世纪下的投影在CCSM3气体发射场景下,不仅在A1B,A2和B1下的极端降水,而且在A1FI情景下比历史时期很多。这意味着A1FI情景也很重要,评估未来的气候变化不仅对水资源影响而且极端的洪水。

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