Measurements of spectral solar UV irradiance in tropical Australia

被引:76
作者
Bernhard, G [1 ]
Mayer, B [1 ]
Seckmeyer, G [1 ]
Moise, A [1 ]
机构
[1] JAMES COOK UNIV N QUEENSLAND, DEPT PHYS, TOWNSVILLE, QLD 4811, AUSTRALIA
关键词
D O I
10.1029/97JD00072
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
Measurements of global spectral irradiance in the UV and visible range were carried out during December 1995 and January 1996 in Townsville, Australia (19.33 degrees S, 146.76 degrees E, 30 m above sea level (asl)) using the mobile spectroradiometer of the Fraunhofer Institute for Atmospheric Environmental Research, Germany. These are, to our knowledge, the first reported spectral UV measurements in the tropics of Australia. For cloudless days, the spectral measurements are consistent with results of a radiative transfer model. In the UVA, measurement and model agree within +/-10% for solar elevations above 10 degrees. In the UVB, the differences are larger (approximate to 15% at 300 nm), which can be explained by uncertainties in the model input parameters of total ozone column and ozone absorption cross section. The variation of the daily erythemal irradiation was found to be +/-24% (+/- 1 sigma) for the period of the campaign. The variation of the total ozone column contributes less than +/-3% to this variability; the main part is introduced by clouds. These attenuate UV irradiation less than total irradiation (300 nm - 3000 nm); the daily total irradiation averaged over the period of the campaign was reduced by a factor of 0.71 owing to cloudiness compared to the clear-sky case while the erythemal irradiation was only diminished by a factor of 0.78. Using long-term records of total irradiation and ozone column, the parameters influencing UV radiation on Earth were found to be typical for the period and site of the campaign. The maximum erythemally weighted irradiance measured during the campaign was 429 mW/m(2), and the average daily erythemal irradiation for this period was 6.06 kJ/m(2). These high radiation levels were found to exceed the corresponding values for Garmisch-Partenkirchen (47.5 degrees N, 11.0 degrees E, 730 m asl). Germany, by between 55 and 70%. This pronounced difference in the radiation environment between Australia and Germany is explained by the higher solar elevation and the lower ozone column in the tropics.
引用
收藏
页码:8719 / 8730
页数:12
相关论文
共 36 条
  • [1] Anderson G, 1986, AFGLTR860110
  • [2] BARTON IJ, 1983, 46 CSIRO AUSTR DIV A, P1
  • [3] SOLAR UVB-ALBEDO OF VARIOUS SURFACES
    BLUMTHALER, M
    AMBACH, W
    [J]. PHOTOCHEMISTRY AND PHOTOBIOLOGY, 1988, 48 (01) : 85 - 88
  • [4] Bodeker GE, 1996, J APPL METEOROL, V35, P1860, DOI 10.1175/1520-0450(1996)035<1860:AAFISU>2.0.CO
  • [5] 2
  • [6] New ultraviolet spectroradiometer measurements at Mauna Loa observatory
    Bodhaine, BA
    McKenzie, RL
    Johnston, PV
    Hofmann, DJ
    Dutton, EG
    Schnell, RC
    Barnes, JE
    Ryan, SC
    Kotkamp, M
    [J]. GEOPHYSICAL RESEARCH LETTERS, 1996, 23 (16) : 2121 - 2124
  • [7] BOJKOV RD, 1995, PUBL WORLD METEOROL
  • [8] TOTAL SOLAR-RADIATION AND THE INFLUENCE OF CLOUDS AND AEROSOLS ON THE BIOLOGICALLY EFFECTIVE UV
    BORDEWIJK, JA
    SLAPER, H
    REINEN, HAJM
    SCHLAMANN, E
    [J]. GEOPHYSICAL RESEARCH LETTERS, 1995, 22 (16) : 2151 - 2154
  • [9] STRATOSPHERIC OZONE REDUCTION, SOLAR UV-B RADIATION AND TERRESTRIAL ECOSYSTEMS
    CALDWELL, MM
    FLINT, SD
    [J]. CLIMATIC CHANGE, 1994, 28 (04) : 375 - 394
  • [10] *GERM I STAND, 1982, 5031 DIN GERM I ST 3