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Validation of the effects of temperature simulated by multi-model ensemble and prediction of mean temperature changes for the next three decades in China
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作者 Ke Liu Jie Pan +1 位作者 ShengCai Tao YinLong Xu 《Research in Cold and Arid Regions》 2012年第1期56-64,共9页
Using series of daily average temperature observations over the period of 1961-1999 of 701 meteorological stations in China, and simulated results of 20 global climate models (such as BCCR_BCM2.0, CGCM3T47) during t... Using series of daily average temperature observations over the period of 1961-1999 of 701 meteorological stations in China, and simulated results of 20 global climate models (such as BCCR_BCM2.0, CGCM3T47) during the same period as the observation, we validate and analyze the simulated results of the models by using three factor statistical method, achieve the results of mul- ti-model ensemble, test and verify the results of multi-model ensemble by using the observation data during the period of 1991-1999. Finally, we analyze changes of the annual mean temperature result of multi-mode ensemble prediction for the period of 2011-2040 under the emission scenarios A2, A1B and B 1. Analyzed results show that: (1) Global climate models can repro- duce Chinese regional spatial distribution of annual mean temperature, especially in low latitudes and eastern China. (2) With the factor of the trend of annual mean temperature changes in reference period, there is an obvious bias between the model and the observation. (3) Testing the result of multi-model ensemble during the period of 1991-1999, we can simulate the trend of temper- ature increase. Compared to observation, the result of different weighing multi-model ensemble prediction is better than the same weighing ensemble. (4) For the period of 20ll-2040, the growth of the annual mean temperature in China, which results from multi-mode ensemble prediction, is above 1℃. In the spatial distribution of annual mean temperature, under the emission scenarios of A2, A1B and B 1, the trend of growth in South China region is the smallest, the increment is less than or equals to 0.8℃; the trends in the northwestern region and south of the Qinghai-Tibet Plateau are the largest, the increment is more than 1℃. 展开更多
关键词 global climate model different weighing multi-model ensemble same weighing multi-model ensemble wanning
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多模式集合对中国气温的模拟效果及未来30年中国气温变化预估 被引量:16
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作者 刘珂 许吟隆 +2 位作者 陶生才 潘婕 杨红龙 《高原气象》 CSCD 北大核心 2011年第2期363-370,共8页
利用1961-1999年中国区域701个气象站气温观测资料,分析了20个全球气候模式(IPCCAR4)在中国区域地面气温的模拟能力;利用三因素统计方法,先确定各模式气温模拟的权重因子,最后对多模式做不等权重和等权重的集合模拟。在此基础上分析了A2... 利用1961-1999年中国区域701个气象站气温观测资料,分析了20个全球气候模式(IPCCAR4)在中国区域地面气温的模拟能力;利用三因素统计方法,先确定各模式气温模拟的权重因子,最后对多模式做不等权重和等权重的集合模拟。在此基础上分析了A2,A1B,B1排放情景下未来时段(2011-2040年)中国区域的气温变化。结果表明:(1)全球模式对中国区域年平均气温的空间分布模拟较好,特别是在低纬地区及东部地区;但年平均气温演变趋势的模拟值较观测值偏差较大;(2)两种不同集合方法都可以模拟出中国区域的升温趋势,但不等权重集合效果略好于等权重集合;(3)2011-2040年,相对于1961-1990时段,多模式集合预估结果表明,3种温室气体排放情景下中国区域年平均气温的增幅均在1℃以上,其中华南地区的增幅最小,增幅<0.8℃,而西北和青藏高原南部地区增幅均在1℃以上。 展开更多
关键词 全球气候模式 模式不等权重集合 模式等权重集合 增温
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