Some results of turbidity networks
Some results of turbidity networks
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浊度网络的一些结果
DOI：
10.3402/tellusa.v21i5.10111
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发表时间：
1969
期刊：
影响因子：
--
通讯作者：
F. Volz
中科院分区：
文献类型：
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作者：
F. Volz
作者于1961年在美国俄亥俄州辛辛那提的国家空气污染控制中心和1963年至1967年在西欧建立了浊度网络，用于通过测量太阳辐射(主要是通过太阳光度计)获得雾霾日衰减值。给出了这两个网络在感兴趣的时期的浑浊过程。当提到气团快速变化的时期时，讨论浑浊的天气变化是相当困难的，但在宁静、晴朗的天气期间，经常可以观察到网络大部分地区的一致性。其他数据显示，中欧地区的工业活动导致垂直光学厚度每天增加T D？0.02，而平均T D=0.23。因此，经常观测到的高浑浊度(T D？1.1)通常一定有其他原因，在北美和欧洲的气候中，可能主要与云物理有关。DOI：10.1111/j.2153-3490.1969.tb00468.x
Turbidity networks to obtain daily values of haze attenuation from measurements of solar radiation, mostly by means of sun photometers, were established in 1961 in the USA by the National Center for Air Pollution Control, Cincinnati, Ohio, and in Western Europe from 1963 to 1967 by the author. The course of turbidity in the two networks during interesting periods is presented. Discussion of synoptic variations of turbidity is rather difficult, when referring to periods of rapid change of air masses, but consistency over large parts of the network is often observed during periods of quiet, sunny weather. Other data show that industrial activity over Central Europe is resulting in a daily increase of vertical optical thickness T D ? 0.02, while T D = 0.23 in the average. Thus, the often observed high values of turbidity (T D ? 1.1) must normally have other causes and may, in the climate of North America and Europe, be related mostly to cloud physics. DOI: 10.1111/j.2153-3490.1969.tb00468.x