Suvremene promjene klime i smanjenje protoka Save u Zagrebu
| Autor: | Tomislav Šegota, Anita Filipčić |
|---|---|
| Jazyk: | angličtina |
| Rok vydání: | 2007 |
| Předmět: |
Hydrology
Atmospheric Science Humid continental climate promjene klime Sava protoka padaline Geography Planning and Development lcsh:G1-922 Geography promjena klime godišnje padaline u Ljubljani i Zagrebu srednji godišnji protok Save u Zagrebu atmosferski tlak u Zagrebu Streamflow Evapotranspiration Precipitation climate change annual precipitation in Ljubljana and Zagreb mean annual Sava flow through Zagreb atmospheric pressure in Zagreb lcsh:Geography (General) Earth-Surface Processes Demography |
| Zdroj: | Geoadria, Vol 12, Iss 1, Pp 47-58 (2007) Geoadria Volume 12 Issue 1 |
| ISSN: | 1848-9710 1331-2294 |
| Popis: | Koeficijent korelacije 0,81 između protoka Save u Zagrebu i padalina u Ljubljani ukazuje na dominantno značenje padalina. U najtoplijim mjesecima protok Save mnogo ovisi o evapotranspiraciji. Protok Save ima silazni trend, a oštro se luče dva razdoblja: 1926.-1959. i 1960.-1995. To je posljedica isto takvog hoda padalina u gornjem toku Save. U cijelom promatranom razdoblju postoji trend porasta atmosferskog tlaka. Za "padalinsku kontinentalnost" značajna je promjena trenda. Od 1960. god. opada udio "ljetnih" padalina. Correlation coefficient of 0.81 between Sava River flow through Zagreb and precipitation in Ljubljana points at dominant significance of precipitation. In the warmest months Sava flow is very much dependent on evapotranspiration. Sava River flow has downward trend, and two intervals can be sharply distinguished: 1926-1959 and 1960-1995. That is the result of the identical precipitation trend at the Upper Sava. There is the trend of atmospheric pressure rise in the entire observed period. "Precipitation continentality" is characterized by change of trend. Share of "summer" precipitation has been declining since 1960. |
| Databáze: | OpenAIRE |
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