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Cold air intrusions over southeastern South America - GFDL model behavior regarding climate simulations in the 20th century and future projections

机译:南美东南部的冷空气入侵-与20世纪气候模拟有关的GFDL模型行为及未来预测

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Cold air intrusions in three areas frequently affected by frosts of southeastern South America are analyzed based on GFDL-CM2.0 Coupled Atmospheric and Oceanic Global Circulation Model. The general objective is to investigate the model ability to simulate the frequency of intrusions in the present climate as well as the changes in the frequency of occurrence and atmospheric characteristics in a future climate scenario. The cold period (May to September) is analyzed for the control period 1961 to 1990 and for the period 2081 to 2100 from the CMIP3 A2 scenario, which reflects the extreme global warming. The coupled GFDL-CM2.0 overestimated the number of cold air intrusions for the present climate (control). This systematic error should be considered in the analyses of future climate results. Future projections indicated a reduction of these cases in GFDL results. As this model overestimated the number of cases, the reduction could be even greater. Composites of extreme cases for the present and future climate in the three areas indicated intensification of the temperature gradient which suggests more vigorous frontal systems, intensification of post-frontal highs and cold air extending to lower latitudes as compared to the present climate. Anomaly intensification was related to the climatological mean temperature, which is higher in the future than in the present. Therefore, even with less cold air intrusion over southeastern South America and a lower number of frost cases in the three areas, the occurrence of more intense systems would have an impact on the agriculture of these areas and such impact would extend to lower latitudes.
机译:基于GFDL-CM2.0大气和海洋全球环流耦合模型,分析了南美洲东南部经常受霜冻影响的三个地区的冷空气入侵。总的目的是研究模拟模型的能力,以模拟当前气候下的入侵频率以及未来气候情景下的发生频率和大气特征的变化。从CMIP3 A2情景分析了1961年至1990年的冷期(5月至9月)和2081年至2100年的冷期,这反映了全球极端变暖。耦合的GFDL-CM2.0高估了当前气候(控制)的冷空气入侵次数。在分析未来气候结果时应考虑这一系统性误差。未来的预测表明GFDL结果中这些案例的减少。由于该模型高估了案件数量,因此减少的幅度可能更大。与当前气候相比,这三个地区当前和未来气候的极端情况综合表明温度梯度的升高,这表明额叶系统更加活跃,额叶后高点的增强以及冷空气延伸到较低的纬度。异常加剧与气候平均温度有关,未来的平均温度比现在更高。因此,即使南美南部东南部的冷空气入侵较少,而这三个地区的霜冻案例数量减少,更密集的系统的发生也会对这些地区的农业产生影响,并且这种影响将扩展到低纬度地区。

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