Results from the first ARM diffuse horizontal shortwave irradiance comparison

被引:25
作者
Michalsky, JJ [1 ]
Dolce, R
Dutton, EG
Haeffelin, M
Major, G
Schlemmer, JA
Slater, DW
Hickey, JR
Jeffries, WQ
Los, A
Mathias, D
McArthur, LJB
Philipona, R
Reda, I
Stoffel, T
机构
[1] SUNY Albany, Atmospher Sci Res Ctr, Albany, NY 12222 USA
[2] Kipp & Zonen Inc, Bohemia, NY 11716 USA
[3] NOAA, Climate Monitoring & Diagnost Lab, Boulder, CO 80305 USA
[4] Virginia Polytech Inst & State Univ, Blacksburg, VA 24061 USA
[5] Budapest Univ Econ Sci & Publ Adm, Budapest, Hungary
[6] Pacific NW Natl Lab, Richland, WA USA
[7] Eppley Lab Inc, Newport, RI 02840 USA
[8] Yankee Environm Syst Inc, Turners Falls, MA 01376 USA
[9] Carter Scott Design, Brunswick, Vic, Australia
[10] Meteorol Serv Canada, Downsview, ON, Canada
[11] Phys Meteorol Observ, Davos, Switzerland
[12] World Radiat Ctr, Davos, Switzerland
[13] Natl Renewable Energy Lab, Golden, CO USA
关键词
pyranometer; diffuse horizontal irradiance; zero irradiance offset; penumbral corrections; reproducibility; intensive observation period;
D O I
10.1029/2002JD002825
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
[1] The first intensive observation period (IOP) dedicated exclusively to the measurement of diffuse horizontal shortwave irradiance was held in the Fall 2001 at the central facility of the Atmospheric Radiation Measurement (ARM) Southern Great Plains (SGP) site with the cooperation of the Baseline Surface Radiation Network (BSRN) community. The purpose of the study was to compare diffuse irradiance measurements among most commercial pyranometers and a few prototypes calibrated independently using current practices. The hope was to achieve a consensus for this measurement with the goal of improving the uncertainty of shortwave diffuse irradiance measurements. All diffuse broadband measurements were made using the same type of two-axis tracker with the direct beam blocked by shading balls. Tracking was excellent during the IOP with no lost data associated with tracker problems. Fourteen simultaneous measurements were obtained over a two-week period under mostly clear skies with low to moderate aerosol loading. Totally overcast data were obtained during the morning of one day. Five of the measurements are reproducible to about 2 W/m(2) at the 95% confidence level. Three more agree with the mean of these five to about 4 W/m(2) at the 95% confidence level after correction for thermal offsets.
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