COMPARISON BETWEEN THE RESULTS OF A MONTE-CARLO ATMOSPHERIC DIFFUSION-MODEL AND TRACER EXPERIMENTS

被引：35

作者：

BRUSASCA, G ^{[1
]}

TINARELLI, G ^{[1
]}

ANFOSSI, D ^{[1
]}

机构：

[1] CNR,IST COSMOGEOFIS,TURIN,ITALY

来源：

ATMOSPHERIC ENVIRONMENT | 1989年 / 23卷 / 06期

关键词：

D O I：

10.1016/0004-6981(89)90151-0

中图分类号：

X [环境科学、安全科学];

学科分类号：

08 ; 0830 ;

摘要：

引用

页码：1263 / 1280

页数：18

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[3]

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[4]

Brusasca G., 1987, Environmental Software, V2, P151, DOI 10.1016/0266-9838(87)90017-7

[5]

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[6] TURBULENCE STRUCTURE IN CONVECTIVE BOUNDARY-LAYERS AND IMPLICATIONS FOR DIFFUSION [J].

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KITCHEN, M ;

LEIGHTON, JR .

BOUNDARY-LAYER METEOROLOGY, 1983, 25 (04) :345-352

[7] MARKOV-CHAIN SIMULATIONS OF VERTICAL DISPERSION FROM ELEVATED SOURCES INTO THE NEUTRAL PLANETARY BOUNDARY-LAYER [J].

DAVIS, PA .

BOUNDARY-LAYER METEOROLOGY, 1983, 26 (04) :355-376

[8] AN APPLICATION OF THE LANGEVIN EQUATION FOR INHOMOGENEOUS CONDITIONS TO DISPERSION IN A CONVECTIVE BOUNDARY-LAYER [J].

DEBAAS, AF ;

VANDOP, H ;

NIEUWSTADT, FTM .

QUARTERLY JOURNAL OF THE ROYAL METEOROLOGICAL SOCIETY, 1986, 112 (471) :165-180

[9]

DEBAAS AF, 1988, M2627 RIS NAT LAB

[10]

DICKERSON MH, 1986, UCRL95497 L LIV NAT

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