Comparison of Brewer UV irradiance measurements with TOMS satellite retrievals

Comparison of measured UV irradiance with estimates from satellite observation is potentially effective for the validation of the data from the two sources. Data from 10 Canadian Brewer sites were compared in this study with noon UV irradiance estimated from TOMS measurements. In general, TOMS estimates can successfully reproduce long-term and major short-term UV variations, although there are some systematic differences between the measurements at the ground and satellite-retrieved UV irradiance. Up to 9% of the Brewer-TOMS difference can be attributed to the Brewer cosine response error. This error depends on the solar zenith angle and cloud conditions and is different from instrument to instrument. When the cosine response of the Brewer instrument is considered and applied, the Brewer data are still lower than TOMS-estimated UV irradiance at most of the sites by 10% on average. The bias for clear-sky condition is smaller, about 4%, than for overcast conditions (about 20% on average) with some wavelength dependence. The bias was close to 0 at one station (Saturna Island), possibly due to its much cleaner air.

[1]  G. Seckmeyer,et al.  Surface UV from ERS‐2/GOME and NOAA/AVHRR data: A case study , 1997 .

[2]  Dan Lubin,et al.  Global surface ultraviolet radiation climatology from TOMS and ERBE data , 1998 .

[3]  James B. Kerr,et al.  Derivation of UV-A irradiance from pyranometer measurements , 1999 .

[4]  A. J. Miller,et al.  Ultraviolet Index Forecasts Issued by the National Weather Service , 1996 .

[5]  B. Mayer,et al.  Estimation of surface actinic flux from satellite (TOMS) ozone and cloud reflectivity measurements , 1998 .

[6]  M Blumthaler,et al.  Correcting global solar ultraviolet spectra recorded by a brewer spectroradiometer for its angular response error. , 1998, Applied optics.

[7]  Jean Verdebout,et al.  A method to generate surface UV radiation maps over Europe using GOME, Meteosat, and ancillary geophysical data , 2000 .

[8]  H. Slaper,et al.  Reduction of solar UV by clouds: A comparison between satellite‐derived cloud effects and ground‐based radiation measurements , 2000 .

[9]  James B. Kerr,et al.  Long‐term variations of UV‐B irradiance over Canada estimated from Brewer observations and derived from ozone and pyranometer measurements , 2001 .

[10]  P. Bhartia,et al.  UV‐B increases (1979–1992) from decreases in total ozone , 1996 .

[11]  James B. Kerr,et al.  Satellite retrievals of erythemal UV dose compared with ground-based measurements at northern and southern , 2001 .

[12]  James B. Kerr,et al.  Satellite estimation of spectral surface UV irradiance in the presence of tropospheric aerosols , 1998 .

[13]  Ziauddin Ahmad,et al.  Satellite estimation of spectral surface UV irradiance: 2. Effects of homogeneous clouds and snow , 2001 .

[14]  Jay R. Herman,et al.  Earth surface reflectivity climatology at 340–380 nm from TOMS data , 1997 .

[15]  Jay R. Herman,et al.  Distribution of UV radiation at the Earth's surface from TOMS-measured UV-backscattered radiances , 1999 .

[16]  James B. Kerr,et al.  Satellite estimation of spectral UVB irradiance using TOMS derived total ozone and UV reflectivity , 1995 .