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Asian Monsoon and Elevated Heat Pump Mechanism in the CMCC coupled aerosol-climate model simulations

机译:CMCC中的亚洲季风和高热泵机理耦合的气溶胶-气候模型模拟

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摘要

A coupled aerosol-atmosphere-ocean-seaice model is used to analyse the relationship between aerosol and the Asian summer monsoon. In this analysis the elevated heat pump hypothesis and the solar dimming effect associ- ated with aerosol loading are verified and are found to be consistent with our simulations. When increased aerosol loading is found on the Himalayas slopes in the pre-monsoon period (April-May), an intensification in early mon- soon rainfall over India is obtained. An increase in rainfall and cloudiness during the early monsoon has a cooling effect on the land surface. Here it is verified that this cooling is produced also through the solar dimming effect by the presence of more dust from the deserts brought by an increased westerly flow in early monsoon season. A subsequent reduction in monsoon rainfall over India is found, with a beginning of this decrease in northern India. As these results, obtained with a fully coupled model, reproduce a reasonably realistic pattern, it is possible to consider absorbing aerosols as a possible source of seasonal predictability of the Asian summer monsoon over the Indian subcontinent.
机译:利用气溶胶-大气-海洋-海面耦合模型分析了气溶胶与亚洲夏季风之间的关系。在此分析中,验证了升高的热泵假说以及与气溶胶负荷相关的太阳减光效果,发现与我们的模拟结果一致。如果在季风前期(4月至5月)的喜马拉雅山斜坡上发现气溶胶负荷增加,印度早期雨季降雨就会加剧。季风初,降雨和阴天的增加对陆地表面有冷却作用。在这里可以证明,由于季风初季的西风流量增加,沙漠中出现了更多的尘埃,这种降温也是通过太阳能调光效应产生的。随后发现印度各地的季风降雨量减少,而印度北部的降雨量开始减少。由于使用完全耦合模型获得的这些结果重现了合理的实际模式,因此可以考虑将吸收的气溶胶作为印度次大陆上亚洲夏季风的季节可预测性的可能来源。

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