Pregled bibliografske jedinice broj: 5589
Is the observed air temperature increase in Europe during our century anthropogenic?
Is the observed air temperature increase in Europe during our century anthropogenic? // Annales Geophysicae, Supplement II to Volume 15 / Richter, A.K. (ur.).
Katlenburg-Lindau: European Geosciences Union (EGU), 1997. (poster, međunarodna recenzija, sažetak, znanstveni)
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Naslov
Is the observed air temperature increase in Europe during our century anthropogenic?
(Is the observed air temperature increase in europe during our century anthropogenetic?)
Autori
Šinik, Nadežda ; Marki, Antun ; Poje, Dražen
Vrsta, podvrsta i kategorija rada
Sažeci sa skupova, sažetak, znanstveni
Izvornik
Annales Geophysicae, Supplement II to Volume 15
/ Richter, A.K. - Katlenburg-Lindau : European Geosciences Union (EGU), 1997
Skup
XXII General Assembly of the European Geophysical Society
Mjesto i datum
Beč, Austrija, 21.04.1997. - 25.04.1997
Vrsta sudjelovanja
Poster
Vrsta recenzije
Međunarodna recenzija
Ključne riječi
climatic fluctuations; "green-house" effect; anthropogenic CO_2 increase; long series of temperature and cloudiness
(climatic fluctuations; "green-house" effect; anthropogenic CO_2 increase; long series of temperature and cloudiness.)
Sažetak
Usual today"s scenarios of climatic fluctuations modelling explain the observed temperature increase in Europe by the "green house" effect due to a continuous anthropogenic CO_2 increase in the atmosphere. A testing of this assumption by means of filtered long series of temperature, not alone - but in a comparison to simultaneous series of cloudiness at several locations in Europe, revealed a significant and high positive correlation between those two meteorological elements. Such results suggest that - beside anthropogenic influences - natural climatic variations, related to the general circulation of the atmosphere, are still predominant. The paper gives some possible explanations which take into account the cloudiness interference into a very sensitive balance between the received solar and the lost terrestrial radiations which governs all processes in our planetary atmosphere
Izvorni jezik
Engleski
Znanstvena područja
Geologija