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HAZES AND FOGS OVER POLAR SEAS

机译:极地的霾和雾

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摘要

Field studies conducted in the expanse of the Laptev, White, and Pechora seas show that the probability of occurrence of surface maritime fogs is fairly high in transition seasons. For example, in the period from 20 July to 10 September 1995 dense fogs or dense hazes occurred in about 60% of all observations in the Laptev Sea. The concentration of aerosol particles with a diameter in excess of D = 3 μm was 10-1000 times greater than the baseline. Satellite observations in that period showed no significant decrease in visibility. Dependence of the concentration and dispersity of particles with diameter 0.01-3.0 μm on air temperature and wind speed is analyzed. The measurement results provide new data on the physics of polar surface fogs and hazes.
机译:在拉普捷夫,怀特和佩霍拉海域的广阔地区进行的实地研究表明,在过渡季节出现表面海雾的可能性相当高。例如,在1995年7月20日至9月10日期间,拉普捷夫海的所有观测中约有60%发生浓雾或浓雾。直径超过D = 3μm的气溶胶颗粒浓度比基线高10-1000倍。在那个时期的卫星观测结果表明能见度没有明显下降。分析了直径为0.01-3.0μm的颗粒的浓度和分散度与空气温度和风速的关系。测量结果为极性雾和雾的物理性质提供了新的数据。

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