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ROLE OF THE LAND PLUME IN THE TRANSPORT OF OZONE OVER THE OCEAN DURING INDOEX (1999)

机译:在印度支那期间,陆羽在臭氧在海洋上的运输中的作用(1999年)

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摘要

Observations from aircraft, an island station, and two research vessels are used to investigate the development of an elevated mixed layer or land plume over the Arabian sea during the Indian Ocean Experiment Intensive Field Phase 1999 (INDOEX) through air mass modification. Much of the transport of aerosols and gases occurs in this plume located above a well-mixed convective marine boundary layer with a depth of 800-1000 m. The depth of the land plume is approximately 2000 m with the peak ozone concentrations occurring near the centre of this land plume. Significant latitudinal variations in the concentration of ozone occur in the marine boundary layer and in the plume. Mean ozone concentrations in the land plume decreased with distance from the Indian coastline.
机译:在飞机,岛站和两艘研究船上的观测数据被用来研究印度洋在1999年印度洋实验密集场阶段(INDOEX)期间通过气团改良而形成的高架混合层或陆地羽流的形成。气溶胶和气体的大部分运输发生在位于高度混合的对流海洋边界层上方的羽流中,深度为800-1000 m。陆地羽流的深度约为2000 m,臭氧浓度峰值出现在该陆地羽流的中心附近。在海洋边界层和羽流中,臭氧浓度出现了明显的纬度变化。陆地羽流中的平均臭氧浓度随距印度海岸线的距离而降低。

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