Travel Aid for Symposium on the Tropospheric Chemistry of Southern High Latitudes

南半球高纬对流层（南纬60 °以南）， 与北极对流层不同，它位于一个高冰之上， 覆盖的大陆，完全被广泛的 和生物活跃的南部海洋。 它连接着 全球大气和海洋与南极冰盖 和平流层是全球剧烈变化的焦点 今天的研究 南极洲协调研究相对较少 对流层化学及其控制因素， 尽管对流层的巨大潜力， 影响气候的过程，例如通过气候变化 云核的产生，以及云的形而上学 这些特性可能最终并显著影响 高纬度海洋区域的辐射平衡。 这次研讨会将重点讨论的主题是： 1. 对流层中的气溶胶和气体：源、汇、 和发生。 2. 空气-地面交换。 3. 对流层-平流层交换。 4. 与对流层成分有关的冰雪化学 和气候。 5. 云的化学和物理。 6. 气象过程的作用

The southern high latitude troposphere (south of 60o S), in contrast to the Arctic troposphere, lies over an elevated ice- covered continent and is completely surrounded by the extensive and biologically active southern oceans. It links the rest of the global atmosphere and the oceans with the Antarctic ice sheet and stratosphere that are the focus of intense global change research today. Relatively few coordinated studies of Antarctic tropospheric chemistry and its controlling factors have been undertaken, despite the immense potential of tropospheric processes to affect climate, for example through changes in the production of cloud nuclei, and hence cloud metaphysics properties, that may ultimately and significantly affect the radiation balance over the high latitude oceanic regions. The topics to be highlighted in this symposium are: 1. Aerosols and gases in the troposphere: sources, sinks, and occurrence. 2. Air-surface exchange. 3. Troposphere-stratosphere exchange. 4. Ice-snow chemistry related to tropospheric composition and climate. 5. Chemistry and physics of clouds. 6. Role of meteorological processes.