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- W2080497364 abstract "The structure of the planetary boundary layer above a valley of the Swiss Plateau is investigated. The very high night-time loss rates of O3 observed are mainly attributable to dry deposition at the surface. Although it can be inferred that smog-chemistry plays an important role, homogeneous chemistry accounts on average for only about 20% of the observed O3 destruction rates. It is concluded that the dry deposition of O3 at night is much more effective in the hilly terrain around the field site than over horizontally homogeneous terrain. This increase in efficiency is linked with a local wind system. The O3 destruction due to dry deposition occurs mainly in layers of nocturnal downslope wind where O3-rich air is brought to the ground during the whole night. Hence the air reaching the bottom of the valley has a very low O3 content and the upward airflow associated with this local wind system leads to continuous O3 depletion within the lower part of the boundary layer. It follows that the increased effectiveness of the dry deposition in hilly terrain results in a self-cleaning mechanism of the atmosphere which is not necessarily restricted to O3." @default.
- W2080497364 created "2016-06-24" @default.
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- W2080497364 date "1985-01-01" @default.
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- W2080497364 title "The influence of locally induced wind systems on the effectiveness of nocturnal dry deposition of ozone" @default.
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- W2080497364 doi "https://doi.org/10.1016/0004-6981(85)90215-x" @default.
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