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Effect of anthropogenic aerosol emissions on precipitation in warm conveyor belts in the western North Pacific in winter – a model study with ECHAM6-HAM

机译:人为气溶胶排放对冬季北太平洋西部暖流输送带降水的影响– ECHAM6-HAM模型研究

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摘要

While there is a clear impact of aerosol particles on the radiationbalance, whether and how aerosol particles influence precipitation iscontroversial. Here we use the ECHAM6-HAM global climate model coupled to anaerosol module to analyse whetheran impact of anthropogenic aerosol particles on the timing and amount ofprecipitation can be detected in North Pacific warm conveyor belts. Warmconveyor belts are the strongest precipitation-producing airstreams inextratropical cyclones and are identified here with a Lagrangian technique,i.e. by objectively identifying the most strongly ascending trajectories inNorth Pacific cyclones. These conveyor belts have been identified separatelyin 10-year ECHAM6-HAM simulations with present-day and pre-industrial aerosolconditions. Then, the evolution of aerosols and cloud properties has beenanalysed in detail along the identified warm conveyor belt trajectories. Theresults show that, under present-day conditions, some warm conveyor belttrajectories are strongly polluted (i.e. high concentrations of black carbonand sulfur dioxide) due to horizontal transport from eastern Asia to theoceanic region where warm conveyor belts start their ascent. In thesepolluted trajectories a weak delay and reduction of precipitation formationoccurs compared to clean warm conveyor belt trajectories. However, all warmconveyor belts consist of both polluted and clean trajectories at the timethey start their ascent, and the typically more abundant clean trajectoriesstrongly reduce the aerosol impact from the polluted trajectories. The mainconclusion then is that the overall amount of precipitation is comparable inpre-industrial conditions, when all warm conveyor belt trajectories areclean, and in present-day conditions, when warm conveyor belts consist of amixture of clean and polluted trajectories.
机译:虽然气溶胶颗粒对辐射平衡有明显的影响,但是否以及如何影响降水是有争议的。在这里,我们将ECHAM6-HAM全球气候模型与厌氧剂模块耦合使用,以分析在北太平洋暖流输送带中是否可以检测到人为气溶胶颗粒对时间和降水量的影响。温带是在热带气旋中最强的产生降水的气流,在这里用拉格朗日技术确定。通过客观地确定北太平洋气旋中最强烈的上升轨迹。这些传送带已在10年ECHAM6-HAM模拟中分别与当前和工业化前的气溶胶条件一起确定。然后,沿着确定的温暖的输送带轨迹详细分析了气溶胶和云特性的演变。结果表明,在当今条件下,由于从东亚向海底地区的水平运输,温暖的输送带开始上升,一些温暖的输送带轨迹被严重污染(即高浓度的黑碳和二氧化硫)。与干净的温暖的输送带轨迹相比,在这些污染的轨迹中,出现了微弱的延迟并减少了降水的形成。但是,所有温暖的输送带在开始上升时都由污染轨迹和清洁轨迹组成,通常更丰富的清洁轨迹会大大减少污染轨迹对气溶胶的影响。因此,主要结论是,在工业前条件下,当所有温暖的输送带轨迹都清洁时,以及在当今条件下,当温暖的输送带由干净和污染轨迹的混合物组成时,总的降水量是可比的。

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