SMOKE AS A QUANTITATIVE ATMOSPHERIC DIFFUSION TRACER

被引：23

作者：

GIFFORD, FA

机构：

[1] Air Resources Atmospheric Turbulence Diffusion Lab., Nat. Oceanic Atmospheric Adm., Oak Ridge, Tenn. 37830, United States

来源：

ATMOSPHERIC ENVIRONMENT | 1980年 / 14卷 / 10期

关键词：

D O I：

10.1016/0004-6981(80)90175-4

中图分类号：

X [环境科学、安全科学];

学科分类号：

08 ; 0830 ;

摘要：

Generalizations of the ″opacity method″ of analyzing visible smoke-plume diffusion are presented. The horizontal disperson length is derived from the outline of a plume having an arbitrary vertical concentration distribution. The vertical dispersion length is derived for a plume with concentration varying as arbitrary powers in the exponential terms.

引用

页码：1119 / 1121

页数：3

共 9 条

[1]

GIFFORD F, 1957, J METEOROL, V14, P410, DOI 10.1175/1520-0469(1957)014<0410:RADOSP>2.0.CO

[2]

[3]

GIFFORD F, 1959, INT J AIR WATER POLL, V2, P42

[4]

GIFFORD FA, 1968, METEOROLOGY ATOMIC E, pCH3

[5]

MONIN AS, 1971, STATISTICAL FLUID ME, V12

[6]

NAPPO CJ, 1979, 4TH AMS S TURB DIFF, P46

[7]

PASQUILL F, 1974, ATMOSPHERIC TURBULEN

[8]

RANDERSON D, 1977, SP380 NASA, pCH14

[9] The theoretical scattering of smoke in a turbulent atmosphere. [J].

Roberts, OFT .

PROCEEDINGS OF THE ROYAL SOCIETY OF LONDON SERIES A-CONTAINING PAPERS OF A MATHEMATICAL AND PHYSICAL CHARACTER, 1923, 104 (728) :640-654

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