hrcak mascot   Srce   HID

Izvorni znanstveni članak
https://doi.org/10.15291/geoadria.142

Precipitation variability in Croatian areas with maritime pluviometric regime

Mladen Maradin ; Department of Geography, Faculty of Science, Zagreb

Puni tekst: engleski, pdf (3 MB) str. 3-27 preuzimanja: 553* citiraj
APA 6th Edition
Maradin, M. (2013). Precipitation variability in Croatian areas with maritime pluviometric regime. Geoadria, 18 (1), 3-27. https://doi.org/10.15291/geoadria.142
MLA 8th Edition
Maradin, Mladen. "Precipitation variability in Croatian areas with maritime pluviometric regime." Geoadria, vol. 18, br. 1, 2013, str. 3-27. https://doi.org/10.15291/geoadria.142. Citirano 12.04.2021.
Chicago 17th Edition
Maradin, Mladen. "Precipitation variability in Croatian areas with maritime pluviometric regime." Geoadria 18, br. 1 (2013): 3-27. https://doi.org/10.15291/geoadria.142
Harvard
Maradin, M. (2013). 'Precipitation variability in Croatian areas with maritime pluviometric regime', Geoadria, 18(1), str. 3-27. https://doi.org/10.15291/geoadria.142
Vancouver
Maradin M. Precipitation variability in Croatian areas with maritime pluviometric regime. Geoadria [Internet]. 2013 [pristupljeno 12.04.2021.];18(1):3-27. https://doi.org/10.15291/geoadria.142
IEEE
M. Maradin, "Precipitation variability in Croatian areas with maritime pluviometric regime", Geoadria, vol.18, br. 1, str. 3-27, 2013. [Online]. https://doi.org/10.15291/geoadria.142
Puni tekst: hrvatski, pdf (3 MB) str. 3-27 preuzimanja: 437* citiraj
APA 6th Edition
Maradin, M. (2013). Varijabilnost padalina na području Hrvatske s maritimnim pluviometrijskim režimom. Geoadria, 18 (1), 3-27. https://doi.org/10.15291/geoadria.142
MLA 8th Edition
Maradin, Mladen. "Varijabilnost padalina na području Hrvatske s maritimnim pluviometrijskim režimom." Geoadria, vol. 18, br. 1, 2013, str. 3-27. https://doi.org/10.15291/geoadria.142. Citirano 12.04.2021.
Chicago 17th Edition
Maradin, Mladen. "Varijabilnost padalina na području Hrvatske s maritimnim pluviometrijskim režimom." Geoadria 18, br. 1 (2013): 3-27. https://doi.org/10.15291/geoadria.142
Harvard
Maradin, M. (2013). 'Varijabilnost padalina na području Hrvatske s maritimnim pluviometrijskim režimom', Geoadria, 18(1), str. 3-27. https://doi.org/10.15291/geoadria.142
Vancouver
Maradin M. Varijabilnost padalina na području Hrvatske s maritimnim pluviometrijskim režimom. Geoadria [Internet]. 2013 [pristupljeno 12.04.2021.];18(1):3-27. https://doi.org/10.15291/geoadria.142
IEEE
M. Maradin, "Varijabilnost padalina na području Hrvatske s maritimnim pluviometrijskim režimom", Geoadria, vol.18, br. 1, str. 3-27, 2013. [Online]. https://doi.org/10.15291/geoadria.142

Sažetak
The paper deals with the precipitation variability areas of Croatia with pluviometric regime. Precipitation variability was analyzed using yearly and monthly values of the mean relative variability for 18 stations in the period 1950-2007. The research results showed that there is relatively large range of precipitation variability in the researched area. The highest precipitation variability was recorded in Lastovo and the lowest in Parg station. The primary maximum of precipitation variability in the northern Adriatic area is in October, while in the southern part of the Adriatic maximum variability occurs during the summer months - July or August. The minimum variability in most of the stations with maritime pluviometric regime occurs in April, except in the central part of the Adriatic, where it occurs in November. The lowest precipitation variability is in the mountain region of Croatia. The highest values of precipitation variability occur during summer months in the southern part of Adriatic. The values of precipitation variability in the Kvarner region are relatively higher than the variability of the surrounding stations in almost all months.

Ključne riječi
precipitation; precipitation variability; maritime pluviometric regime; Coastal region of Croatia; Mountain region of Croatia

Hrčak ID: 105822

URI
https://hrcak.srce.hr/105822

[hrvatski]

Posjeta: 1.426 *