UV exposure, which is the main source for a sufficient level of Vitamin D in the human body, is found to be up to a factor of 7 lower in Northern Germany (52° N) in the winter months compared to UV levels in the central region of New Zealand's South Island (45° S). When corrected for the influence of solar zenith angle, the Vitamin D-weighted exposure is still a factor of 2 higher in the southern hemisphere at the corresponding latitude. The major part of the difference can be attributed to differences in cloudiness, and a minor part to total ozone and aerosols. Data from several stations in Europe show a high variability due to cloudiness differences between the stations and between different years, but they also show that the differences are not restricted to individual sites and may characterize a northern versus southern hemisphere contrast.Wintertime erythemally-weighted irradiance is also found to be much higher in New Zealand than in Europe. Whereas on a monthly average clouds weaken the UV irradiation by up to 25% for most locations in New Zealand, the reduction is usually up to 50% in central Europe in winter.
Why is it so hard to gain enough Vitamin D by solar exposure in the European winter? / Seckmeyer, Gunther; Mustert, Christopher; Schrempf, Michael; Mckenzie, Richard; Liley, Ben; Kotkamp, Michael; Bais, Alkiviadis; Gillotay, Didier; Slaper, Harry; Siani, Anna-Maria; Smedley, Andrew; Webb, Ann. - In: METEOROLOGISCHE ZEITSCHRIFT. - ISSN 0941-2948. - 27:3(2018), pp. 223-233. [10.1127/metz/2018/0855]
Why is it so hard to gain enough Vitamin D by solar exposure in the European winter?
Siani, Anna-Maria;
2018
Abstract
UV exposure, which is the main source for a sufficient level of Vitamin D in the human body, is found to be up to a factor of 7 lower in Northern Germany (52° N) in the winter months compared to UV levels in the central region of New Zealand's South Island (45° S). When corrected for the influence of solar zenith angle, the Vitamin D-weighted exposure is still a factor of 2 higher in the southern hemisphere at the corresponding latitude. The major part of the difference can be attributed to differences in cloudiness, and a minor part to total ozone and aerosols. Data from several stations in Europe show a high variability due to cloudiness differences between the stations and between different years, but they also show that the differences are not restricted to individual sites and may characterize a northern versus southern hemisphere contrast.Wintertime erythemally-weighted irradiance is also found to be much higher in New Zealand than in Europe. Whereas on a monthly average clouds weaken the UV irradiation by up to 25% for most locations in New Zealand, the reduction is usually up to 50% in central Europe in winter.File | Dimensione | Formato | |
---|---|---|---|
Seckmeyer_Why_2018.pdf
accesso aperto
Tipologia:
Documento in Post-print (versione successiva alla peer review e accettata per la pubblicazione)
Licenza:
Creative commons
Dimensione
863.74 kB
Formato
Adobe PDF
|
863.74 kB | Adobe PDF |
I documenti in IRIS sono protetti da copyright e tutti i diritti sono riservati, salvo diversa indicazione.