Nalazite se na CroRIS probnoj okolini. Ovdje evidentirani podaci neće biti pohranjeni u Informacijskom sustavu znanosti RH. Ako je ovo greška, CroRIS produkcijskoj okolini moguće je pristupi putem poveznice www.croris.hr
izvor podataka: crosbi

20th-century changes of temperature in the mountain regions of Central Europe (CROSBI ID 81379)

Prilog u časopisu | izvorni znanstveni rad | međunarodna recenzija

Weber, O.W. ; Talkner, P. ; Auer, I. ; Bohm, R. ; Gajić-Čapka, Marjana ; Zaninović, Ksenija ; Brazdil, R. ; Faško, P. 20th-century changes of temperature in the mountain regions of Central Europe // Climatic change, 36 (1997), 327-344-x

Podaci o odgovornosti

Weber, O.W. ; Talkner, P. ; Auer, I. ; Bohm, R. ; Gajić-Čapka, Marjana ; Zaninović, Ksenija ; Brazdil, R. ; Faško, P.

engleski

20th-century changes of temperature in the mountain regions of Central Europe

Daily maximum and minimum temperatures from 29 low-lying and mountain stations of 7 countries in Central Europe were analysed. The analysis of the annual vaiation of diurnal temperature range helps to distinguish unique climatic characteristics of high and low altitude stations. A comparison of the tame series of extreme daily temperatures as well as mean temperature shows a good agreement between the low-lying stations and the mountain stations. Many of the pronounced warm and cold periods are present in all time series and are therefore representative for the whole region. A linear trend analysis of the station data fro the period 1901-1990 (19 statios) and 1951-1990 (all 29 stations) shows spatial patterns of similar changes in maximum and minimum daily temperatures and diurnal temperature range. Mountain stations show only small changes of the diurnal temperature range over the 1901-1990 period, whereas the low-lying stations in the western part of the Alps show a significant decrease of diurnal temperature range, caused by strong increase of yhe minimum temperature range decreases at the western low-lying stations, mainly in spring, whereas it remains roughly constant at the mountain stations. The decrease of diurnal temperature range is stronger in the western part than in the eastern part of the Alps.

temperature; changes; Central Europe

nije evidentirano

nije evidentirano

nije evidentirano

nije evidentirano

nije evidentirano

nije evidentirano

Podaci o izdanju

36

1997.

327-344-x

objavljeno

0165-0009

1573-1480

Povezanost rada

Geologija