CHARACTERISTICS OF HOURLY GLOBAL IRRADIANCE MODELED FROM CLOUD DATA

被引：13

作者：

OLSETH, JA

SKARTVEIT, A

机构：

[1] Geophysical Institute, Division of Meteorology, University of Bergen, N-5007 Bergen

来源：

SOLAR ENERGY | 1993年 / 51卷 / 03期

关键词：

D O I：

10.1016/0038-092X(93)90097-8

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 model yielding hourly global irradiance from cloud observations is presented. Tested against independent observations of hourly irradiance, the model yields a correlation coefficient 0.92. The corresponding correlation coefficients for daily and monthly values are 0.975 and 0.998, respectively. The mean bias and root-mean-square errors for hourly data are less than, respectively, 3% and 30% of the average. Moreover, the frequency distributions and the lag one autocorrelations of modelled hourly averages are close to those of the observed data.

引用

页码：197 / 204

页数：8

共 10 条

[1] PERTURBATION OF THE NORTHERN-HEMISPHERE RADIATIVE BALANCE BY BACKSCATTERING FROM ANTHROPOGENIC SULFATE AEROSOLS
CHARLSON, RJ
LANGNER, J
RODHE, H
LEOVY, CB
WARREN, SG
[J]. TELLUS SERIES A-DYNAMIC METEOROLOGY AND OCEANOGRAPHY, 1991, 43 (04) : 152 - 163
[2] ESTIMATING SOLAR IRRADIANCE AND COMPONENTS
DAVIES, JA
MCKAY, DC
[J]. SOLAR ENERGY, 1982, 29 (01) : 55 - 64
[3] EVALUATION OF SELECTED MODELS FOR ESTIMATING SOLAR-RADIATION ON HORIZONTAL SURFACES
DAVIES, JA
MCKAY, DC
[J]. SOLAR ENERGY, 1989, 43 (03) : 153 - 168
[4] Davies JA, 1988, VALIDATION MODELS ES
[5] SOLAR AND TERRESTRIAL-RADIATION DEPENDENT ON THE AMOUNT AND TYPE OF CLOUD
KASTEN, F
CZEPLAK, G
[J]. SOLAR ENERGY, 1980, 24 (02) : 177 - 189
[6] LUND H, 1985, EUR10208 EN TU DENM
[7] OBSERVED AND MODELED HOURLY LUMINOUS EFFICACIES UNDER ARBITRARY CLOUDINESS
OLSETH, JA
SKARTVEIT, A
[J]. SOLAR ENERGY, 1989, 42 (03) : 221 - 233
[8] OLSETH JA, 1992, 1992 P NORTH SUN 92, P439
[9] THE PROBABILITY DENSITY AND AUTOCORRELATION OF SHORT-TERM GLOBAL AND BEAM IRRADIANCE
SKARTVEIT, A
OLSETH, JA
[J]. SOLAR ENERGY, 1992, 49 (06) : 477 - 487
[10] 1965, RAD OBSERVATIONS BER

← 1 →