Reconstructing of erythemal ultraviolet radiation levels in Europe for the past 4 decades

被引:65
作者
den Outer, P. N. [1 ]
Slaper, H. [1 ]
Kaurola, J. [6 ]
Lindfors, A. [6 ,8 ]
Kazantzidis, A. [7 ,9 ]
Bais, A. F. [9 ]
Feister, U. [2 ]
Junk, J. [2 ,5 ]
Janouch, M. [3 ]
Josefsson, W. [4 ]
机构
[1] Natl Inst Publ Hlth & Environm, Radiat Res Lab, NL-3720 BA Bilthoven, Netherlands
[2] Deutsch Wetterdienst, Richard Assmann Observatorium Lindenberg, D-15848 Lindenberg, Germany
[3] Czech Hydrometeorol Inst, Solar & Ozone Observ, Hradec Kralove 50008 8, Czech Republic
[4] Swedish Meteorol & Hydrol Inst, S-60176 Norrkoping, Sweden
[5] Ctr Rech Publ Gabriel Lippmann, L-4422 Belvaux, Luxembourg
[6] Finnish Meteorol Inst, FI-00101 Helsinki, Finland
[7] Univ Patras, Dept Phys, Lab Atmospher Phys, G-26504 Patras, Greece
[8] Univ Edinburgh, Sch Geosci, Edinburgh EH8 9XP, Midlothian, Scotland
[9] Aristotle Univ Thessaloniki, Lab Atmospher Phys, GR-54124 Thessaloniki, Greece
关键词
TOTAL OZONE; SOLAR UV; VITAMIN-D; IRRADIANCE; TRENDS; MODEL; THESSALONIKI; VARIABILITY; ALGORITHM; REVISION;
D O I
10.1029/2009JD012827
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
This paper is based on a comparative study on ultraviolet radiation (UV) measurements and UV reconstruction models for eight sites in Europe. Reconstruction models include neural network techniques and radiative transfer modeling combined with empirical relationships. The models have been validated against quality-controlled ground-based measurements, 8 to 20 years, on time scales ranging from daily to yearly UV sums. The standard deviations in the ratios of modeled to measured daily sums vary between 10 and 15%. The yearly sums agree within a 5% range. Depending on the availability of ancillary measurements, reconstructions have been carried out to the early 1960s. A method has been set up to educe one best estimate of the historical UV levels that takes into account the long-term stability and underlying agreement of the models, and the agreement with actual UV measurements. Using this best estimate, the yearly sums of erythemally weighted UV irradiance showed a range of 300 kJ/m(2) at 67 degrees N to 750 kJ/m(2) at 40 degrees N. The year-to-year variability was lowest at 40 degrees N with a relative variation of 4.3%; for central and northern European latitudes this year-to-year variation was 5.2 to 6.5%. With regard to the period 1980 to 2006, first-order trend lines range from 0.3 +/- 0.1 to 0.6 +/- 0.2% per year, approximately two thirds of which can be attributed to the diminishing of cloudiness and one third to ozone decline.
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页数:17
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