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The impact of land cover generated by a dynamic vegetation model on climate over east Asia in present and possible future climate

机译:动态植被模型产生的土地覆盖对当前和未来气候中东亚气候的影响

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This study investigates the impacts of land cover change, as simulated by adynamic vegetation model, on the summertime climatology over Asia. Theclimate model used in this study has systematic biases of underestimatedrainfall around Korea and overestimation over the South China Sea. Whencoupled to a dynamic vegetation model, the resulting change in land cover isaccompanied by an additional direct radiative effect over dust-producingregions. Both the change in land surface conditions directly and the effectof increased bare-soil fraction on dust loading affect the climate in theregion and are examined separately in this study. The direct radiativeeffect of the additional dust contributes to increasing the rainfall biases,while the land surface physical processes are related to local temperaturebiases such as warm biases over North China. In time slice runs for futureclimate, as the dust loading changes, anomalous anticyclonic flows aresimulated over South China Sea, resulting in reduced rainfall over the SouthChina Sea and more rainfall near Korea and south China. In contrast with therainfall changes, the influence of land cover change and the associated dustradiative effects are very small for a future projection of temperature, whichis dominated by atmospheric CO2 increase. The results in this studysuggest that the land cover simulated by a dynamic vegetation model canaffect, and be affected by, model systematic biases on regional scales overdust emission source regions such as Asia. In particular, the analysis of theradiative effects of dust changes associated with land cover change isimportant in order to understand future changes in regional precipitation inglobal warming.
机译:这项研究调查了动态植被模型模拟的土地覆盖变化对亚洲夏季气候的影响。本研究中使用的气候模型对韩国周围的降雨被低估以及南中国海的高估具有系统性的偏见。当耦合到动态植被模型时,土地覆盖的最终变化将伴随着产尘区的额外直接辐射效应。土地表面条件的直接变化和裸土含量增加对粉尘负荷的影响都影响该地区的气候,本研究对此进行了单独研究。额外粉尘的直接辐射效应导致降雨偏倚增加,而地表物理过程与局部温度偏倚有关,例如华北地区的温暖偏倚。在未来气候变化的时间片中,随着尘埃含量的变化,在南中国海模拟了反气旋异常流动,导致南中国海的降水减少,而韩国和华南附近的降水增加。与降雨变化相反,对于未来的温度预测,土地覆盖变化和相关的尘埃辐射效应的影响很小,这主要是由大气中CO 2 的增加决定的。本研究的结果表明,动态植被模型模拟的土地覆盖可以影响区域尺度上的系统性偏差,并受到其影响,例如亚洲。尤其是,分析与土地覆盖变化相关的尘埃变化的辐射效应非常重要,以便了解全球变暖对区域降水的未来变化。

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