Aircraft observations of the solar ultraviolet irradiance throughout the troposphere

Observations of the biological effective solar ultraviolet irradiance, made by instrumentation flown on a Falcon aircraft over the entire Greek area, from the sea up to the tropopause level, obtained in the frame of the Radiation Field in the Troposphere-Scientific Training and Access to Aircraft for Atmospheric Research Throughout Europe project, are presented to discuss among others its altitude dependence. The experimental data of the biological effective solar UV irradiance as a function of height, throughout the troposphere, showed an average increase of about 7.2±1.2% km−1, which is in close agreement with the theoretically derived one, by using an appropriate algorithm, providing the biological effective solar UV irradiance at various altitudes from the Earth's surface. This increase rate has also been compared with the burden ozone content at each height level as it was derived from ozone concentration measurements obtained by both balloon ascents and the aircraft's instrumentation. This comparison showed a strong anticorrelation (correlation coefficient r = −0.98) between the biological effective solar UV irradiance and the integrated ozone content above each height level corresponding to 0.25% increase in UV per 1 Dobson Unit (1DU = 0.001 atm cm) decrease in total ozone column, approximately.

[1]  R. Bird,et al.  Simple Solar Spectral Model for Direct and Diffuse Irradiance on Horizontal and Tilted Planes at the Earth's Surface for Cloudless Atmospheres , 1986 .

[2]  R. McKenzie,et al.  New Ultraviolet Spectroradiometer measurements at Mauna Loa Observatory , 1996 .

[3]  S. Bozzo,et al.  Variations in UV radiation in Chile. , 1995, Journal of photochemistry and photobiology. B, Biology.

[4]  On radiant energy in high-temperature research , 1961 .

[5]  Costas A. Varotsos,et al.  The role of clouds on the solar ultraviolet radiation , 1995 .

[6]  Ellsworth G. Dutton,et al.  UV measurements at Mauna Loa: July 1995 to July 1996 , 1997 .

[7]  S. Madronich,et al.  Changes in ultraviolet-radiation reaching the earths surface , 1994 .

[8]  Bernhard Mayer,et al.  New maximum UV irradiance levels observed in Central Europe , 1997 .

[9]  C. Varotsos Solar ultraviolet radiation and total ozone, as derived from satellite and ground-based instrumentation , 1994 .

[10]  H. Neckel,et al.  Improved data of solar spectral irradiance from 0.33 to 1.25 microns , 1981 .

[11]  K. Kondratyev,et al.  On the relationship between total ozone and solar ultraviolet radiation at St. Petersburg, Russia , 1995 .

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

[13]  H. Piazena,et al.  The effect of altitude upon the solar UV-B and UV-A irradiance in the tropical Chilean Andes , 1996 .

[14]  Bo G Leckner,et al.  The spectral distribution of solar radiation at the earth's surface—elements of a model , 1978 .

[15]  Costas A. Varotsos,et al.  Erythemally weighted UV trends over northern latitudes derived from Nimbus 7 TOMS measurements , 2000 .

[16]  M. Blumthaler,et al.  Increase in solar UV radiation with altitude , 1997 .

[17]  Costas A. Varotsos,et al.  On the altitude dependence of solar effective UV , 1999 .