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Clouds, aerosols, and precipitation in the marine boundary layer: an ARM Mobile Facility Deployment

机译:海洋边界层中的云,气溶胶和降水:ARM移动设施部署

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摘要

The Clouds, Aerosol, and Precipitation in the Marine Boundary Layer (CAP-MBL) deployment at Graciosa Island in the Azores generated a 21-month (April 2009–December 2010) comprehensive dataset documenting clouds, aerosols, and precipitation using the Atmospheric Radiation Measurement Program (ARM) Mobile Facility (AMF). The scientific aim of the deployment is to gain improved understanding of the interactions of clouds, aerosols, and precipitation in the marine boundary layer.ududGraciosa Island straddles the boundary between the subtropics and midlatitudes in the northeast Atlantic Ocean and consequently experiences a great diversity of meteorological and cloudiness conditions. Low clouds are the dominant cloud type, with stratocumulus and cumulus occurring regularly. Approximately half of all clouds contained precipitation detectable as radar echoes below the cloud base. Radar and satellite observations show that clouds with tops from 1 to 11 km contribute more or less equally to surface-measured precipitation at Graciosa. A wide range of aerosol conditions was sampled during the deployment consistent with the diversity of sources as indicated by back-trajectory analysis. Preliminary findings suggest important two-way interactions between aerosols and clouds at Graciosa, with aerosols affecting light precipitation and cloud radiative properties while being controlled in part by precipitation scavenging.ududThe data from Graciosa are being compared with short-range forecasts made with a variety of models. A pilot analysis with two climate and two weather forecast models shows that they reproduce the observed time-varying vertical structure of lower-tropospheric cloud fairly well but the cloud-nucleating aerosol concentrations less well. The Graciosa site has been chosen to be a permanent fixed ARM site that became operational in October 2013.
机译:在亚速尔群岛的Graciosa岛部署的海洋边界层中的云,气溶胶和降水(CAP-MBL)生成了一个21个月(2009年4月至2010年12月)的综合数据集,使用大气辐射测量记录了云,气溶胶和降水程序(ARM)移动设施(AMF)。部署的科学目的是要加深对海洋边界层中云,气溶胶和降水相互作用的了解。 ud udGraciosa岛横跨东北大西洋的亚热带和中纬度之间的边界,因此经历了一次气象条件和阴天条件的多样性。低云是主要的云类型,平积云和积云定期发生。所有云层中约有一半包含降水量,这些降水可作为雷达回波在云层底下检测到。雷达和卫星观测结果表明,从1至11 km的高空云对Graciosa的地面测量降水的贡献大致相同。部署期间对广泛的气溶胶条件进行了采样,这与反向轨迹分析表明的来源的多样性相一致。初步发现表明,Graciosa气溶胶与云之间存在重要的双向相互作用,气溶胶会影响光降水和云辐射特性,同时部分受到降水清除的控制。 ud udGraciosa的数据正在与通过多种型号。对两个气候和两个天气预报模型进行的先导分析表明,它们很好地再现了对流层低层云的观察到的时变垂直结构,但成云的气溶胶浓度却不太好。 Graciosa站点已被选为永久性ARM固定站点,于2013年10月投入运营。

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