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首页> 外文期刊>Revista Brasileira de Meteorologia >AS INCERTEZAS ASSOCIADAS àS CONDI??ES CLIMáTICAS OBTIDAS PELO MODELO ETA CPTEC/HADCM3: AVALIA??O COMPARATIVA ENTRE OS DADOS SIMULADOS E OBSERVADOS DE PRECIPITA??O, EVAPOTRANSPIRA??O E VAZ?O NA BACIA HIDROGRáFICA DO RIO IJUí, BRASIL.
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AS INCERTEZAS ASSOCIADAS àS CONDI??ES CLIMáTICAS OBTIDAS PELO MODELO ETA CPTEC/HADCM3: AVALIA??O COMPARATIVA ENTRE OS DADOS SIMULADOS E OBSERVADOS DE PRECIPITA??O, EVAPOTRANSPIRA??O E VAZ?O NA BACIA HIDROGRáFICA DO RIO IJUí, BRASIL.

机译:ETA CPTEC / HADCM3模型所具有的与气候条件有关的不确定性:巴西水道盆地中模拟和观测到的降水数据,蒸发蒸腾和空度之间的比较评估。

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This study aims to evaluate the climate scenarios simulated by the Eta CPTEC/HadCM3 model, conducted by four members of the HadCM3 global climate model (CNTRL, LOW, MID and HIGH), at the Ijuí River Basin, Brazil. The used control period was from 1961 to 1975, looking for the assessment of climate scenarios and river flow during the 1976 and 1990 period. The task was divided into five stages: spatial interpolation of climate data, correction of simulated climatic variables series (bias correction), calculation of reference evapotranspiration, hydrological simulation of monthly river flow, comparison between simulated and observed conditions of precipitation, evapotranspiration and river flow. Although the correction methods used to eliminate the simulated climate series biases have originated very different scenarios, neither methods presented a better performance in all examined criteria. Sometimes, the differences between the simulated values based on the Eta Model and the observed values were higher than 20%, both in both rainfall and river flow resulting from the hydrologic modeling processes. Therefore, one must consider that these uncertainties will propagate to future scenarios, when analyzing the effects of climate change on water availability.
机译:这项研究旨在评估由Eta CPTEC / HadCM3模型模拟的气候情景,该模型由HadCM3全球气候模型的四个成员(CNTRL,LOW,MID和HIGH)在巴西伊尤伊河流域进行。所用的控制时期是1961年至1975年,用于评估1976年和1990年期间的气候情景和河流流量。该任务分为五个阶段:气候数据的空间插值,模拟气候变量系列的校正(偏差校正),参考蒸散量的计算,每月河流流量的水文模拟,降水的模拟条件与观测条件,蒸散量和河流流量之间的比较。尽管用于消除模拟的气候序列偏差的校正方法源自非常不同的场景,但是两种方法在所有检查的标准中均未显示出更好的性能。有时,基于Eta模型的模拟值与观测值之间的差异在水文模拟过程产生的降雨和河流流量中都超过20%。因此,在分析气候变化对水供应的影响时,必须考虑到这些不确定性会传播到未来的情况。

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