COMPARISON BETWEEN ATMOSPHERIC TURBIDITY COEFFICIENTS OF DESERT AND TEMPERATE CLIMATES

被引：33

作者：

ABDELRAHMAN, MA ^{[1
]}

SAID, SAM ^{[1
]}

SHUAIB, AN ^{[1
]}

机构：

[1] KING FAHD UNIV PETR & MINERALS,DEPT MECH ENGN,DHAHRAN 31261,SAUDI ARABIA

来源：

SOLAR ENERGY | 1988年 / 40卷 / 03期

关键词：

SOLAR RADIATION - Measurements;

D O I：

10.1016/0038-092X(88)90044-8

中图分类号：

TE [石油、天然气工业]; TK [能源与动力工程];

学科分类号：

0807 ; 0820 ;

摘要：

A summary of factors affecting the atmospheric turbidity is given. Data on aerosol optical depth and atmospheric turbidity coefficients (i. e. , the Linke factor, T, and Angstrom coefficient, beta ) calculated from measurements of broad band filters at Dhahran (Saudi Arabia), desert climate, are reported. A linear regression model fitted to beta versus T for Dhahran is similar to the models reported for Avignon (France) and Potsdam (Germany), temperate climate. The coefficients of Dharham model are different from the approximately equal coefficients of Avignon and Potsdam models. The variation in the monthly average values of beta and T at Dhahran is of similar trend to that of Avignon and Potsdam. However, Dhahran has shown higher values of atmospheric turbidity coefficients than Avignon and Potsdam due to the effect of the former's desert climate.

引用

页码：219 / 225

页数：7

共 18 条

[1]

ABDELRAHMAN MA, 1981, P ISES C BRIGHTON

[2]

ABDELRAHMAN MA, 1984, ATMOSPHERIC ENV, V18

[3] TECHNIQUES OF DETERMINIG THE TURBIDITY OF THE ATMOSPHERE [J].

ANGSTROM, A .

TELLUS, 1961, 13 (02) :214-223

[4]

ANGSTROM A, 1961, ARK GEOFYSIK, V3

[5]

BOWER LW, 1977, SOLAR ENERGY, V19

[6]

FLOWERS EC, 1969, J APPL METEOROL, V8

[7]

GATES DM, 1966, SCIENCE, V152

[8]

HOYT DV, 1977, THEORETICAL CALCULAT

[9]

HOYT DV, 1978, SOLAR ENERGY, V22

[10]

KATZ M, 1982, SOLAR ENERGY, V28

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