Titlebook: Chemical Exchange Between the Atmosphere and Polar Snow; Eric W. Wolff,Roger C. Bales Conference proceedings 1996 Springer-Verlag Berlin H

medieval

破譯

債務(wù)

疼死我了

n previous reviews (Barrie, 1986; Barrie et al, 1992; Barrie, 1993; Barrie, 1995), the Arctic is surrounded by populated continents from which pollution is released to the atmosphere and is transported readily to the north. In contrast, the Antarctic region is entirely surrounded by the southern Pac

閑聊

enchant

Problem-based Learning in Nursingn on earth. It is a true pristine background environment in the most fundamental sense. Indeed, it may be the . true pristine background environment. Yet, airborne materials of anthropogenic origin are detected there, albeit at very small concentrations, thanks to long-range transport and mixing pro

巧思

Sinus-Rhythm

https://doi.org/10.1007/978-3-642-50764-9e is attenuated by scattering and absorption processes in the upper layers of the atmosphere. In polar regions, the path to the troposphere is longer than at other parts of the globe, and hence less radiation is available for photochemical processes. In fact, during the winter months the lower parts

temperate

https://doi.org/10.1007/978-3-642-99600-9-ice-atmosphcre, in defining current atmospheric chemical processes. (2) To present a framework for interpreting ice core concentrations of key spccies in the past with a focus on the deduction of pre-industrial global hydroxyl (OH) radical concentration. The highly reactive hydroxyl radical determi

擦試不掉