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A5-UNIBO EXPERIMENT ONBOARD BEXUS 18: A RESEARCH ON AEROSOLS AND CLOUD FORMATION

机译:A5-UNIBO实验机载BEXUS 18:气溶胶和云团形成的研究

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Aerosols are solid or liquid particles suspended in the atmosphere. Aerosols acting as cloud condensation nuclei are required for cloud formation in the atmosphere. Aerosols and clouds still contribute the largest uncertainties to the Earth's changing energy budget. Ion-induced nucleation has been proposed as a possible mechanism for new particle formation in addition to homogeneous nucleation in the presence of sulphuric acid. Since atmospheric ion concentrations are largely determined by the intensity of galactic cosmic rays, this mechanism could explain the observed cosmic ray-climate correlation. A5-Unibo experiment, flown onboard BEXUS 18 stratospheric balloon within the REXUS/BEXUS programme, was proposed to gain a better understanding of these processes. The experiment acquired different measurements from specific instruments and sensors integrated in the system to create vertical profiles of different atmospheric parameters. The preliminary results have identified a possible role of positive ions for nucleation in the lower troposphere, and of negative ions in the upper troposphere/lower stratosphere.
机译:气溶胶是悬浮在大气中的固体或液体颗粒。在大气中形成云需要用作云凝结核的气溶胶。气溶胶和云仍然是地球不断变化的能源预算中最大的不确定因素。除了在硫酸存在下的均匀成核作用外,还提出了离子诱导成核作用作为新颗粒形成的可能机理。由于大气中的离子浓度很大程度上取决于银河系宇宙射线的强度,因此这种机制可以解释观测到的宇宙线与气候的相关性。建议在REXUS / BEXUS计划中的BEXUS 18平流层气球上飞行A5-Unibo实验,以更好地了解这些过程。实验从集成在系统中的特定仪器和传感器获得了不同的测量值,以创建不同大气参数的垂直剖面。初步结果已经确定,正离子在对流层下部对成核作用和负离子在对流层上部/平流层下部具有可能的作用。

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