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THE RADIATE AND LIGHT CHARACTERISTICS OF THE CLIMATE CHANGE DURING THE SECOND HALF OF 20th CENTURY IN MOSCOW

机译:20世纪下半叶在莫斯科的下半年气候变化的辐射和光明特征

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In the second half of the 20th Century in the Meteorological Observatory of Moscow State University the analysis of long-term actinometric measurements was done. This analysis included the examination of multiannual variability of the aerosol optical thickness at (lambda)(velence)550 nm (AOT), total (N_(T)) and low (N_(L)) cloud amount, sunshine duration, net radiation and its components, surface albedo, natural illuminance (E), ultraviolet (UV, lambda<=380 nm) and photosynthetically active (PAR, 380-710 nm) solar radiation. Besides, there the presence of "clear" period in Moscow was revealed, characterized by low values of AOT at 1994-2001. Compared with the norm the increase of integral (300-5000 nm) and UV radiation was estimated in clear sky condition during this period. On the example of one month (March) the strong connection between monthly means of surface albedo and air temperature was showed.
机译:在20世纪下半叶在莫斯科国有大学的气象观测所做的长期传感测量分析。该分析包括在(λ)(柔岩)550nm(AOT),总(n_(t))和低(n_(l))云量,阳光持续时间,净辐射和净辐射和其成分,表面反照,天然照度(E),紫外(UV,λ<= 380nm)和光合作用(PAR,380-710nm)的太阳辐射。此外,揭示了莫斯科在莫斯科的“明确”时期的存在,其特征在于1994 - 2001年的AOT值低。与常规相比,在此期间,在清晰的天空状态下估计整体(300-5000nm)和紫外线辐射的增加。在一个月(3月)的例子上,表明了表面玻璃体和空气温度的月度平均手段之间的强烈连接。

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