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What drives daily precipitation over the central Amazon? Differences observed between wet and dry seasons

机译:什么推动了亚马逊中央沉淀的日子? 潮湿和干燥季节之间观察到的差异

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This study offers an alternative presentation regarding how diurnal precipitation is modulated by convective events that developed over the central Amazon during the preceding nighttime period. We use data collected during the Observations and Modelling of the Green Ocean Amazon (GoAmazon?2014/2015) field campaign that took place from 1?January?2014 to 30?November?2015 in the central Amazon. Local surface-based observations of cloud occurrence, soil temperature, surface fluxes, and planetary boundary layer characteristics are coupled with satellite data to identify the physical mechanisms that control the diurnal rainfall in central Amazon during the wet and dry seasons. This is accomplished through evaluation of the atmospheric properties during the nocturnal periods preceding raining and non-raining events. Comparisons between these non-raining and raining transitions are presented for the wet (January to April) and dry (June to September) seasons. The results suggest that wet-season diurnal precipitation is modulated by nighttime cloud coverage and local influences such as heating induced turbulence, whereas the dry-season rain events are controlled by large-scale circulations.
机译:本研究提供了有关在前面的夜间期间在中央亚马逊中开发的对流事件调节日差的调制程度的替代介绍。我们使用在绿色海洋亚马逊的观察和建模期间收集的数据(Goamazon?2014/2015)现场活动,从1?1月份到2014年至30岁?11月?2015年在亚马逊中部。基于局部的云发生观察,土壤温度,表面磁通和行星边界层特性与卫星数据相结合,以识别在潮湿和干燥季节期间控制亚马逊中央降雨量的物理机制。这是通过评估下雨和非下雨事件前的夜间时期的大气性质来实现的。这些非雨和下雨过渡之间的比较呈现为潮湿(1月至4月),干燥(6月至9月)季节。结果表明,湿季昼夜降水由夜间云覆盖和局部影响,例如加热造成湍流,而干季雨季事件由大规模循环控制。

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