Zobrazeno 1 - 10
of 40
pro vyhledávání: '"Danijel Orešić"'
Autor:
Ivan Čanjevac, Danijel Orešić
Publikováno v:
Acta Geographica Slovenica, Vol 58, Iss 2, Pp 7–18-7–18 (2018)
This paper presents the results of the first comprehensive national analysis of changes in discharge regimes of rivers in Croatia. Seven types of discharge regimes have been defined for rivers in Croatia. We analyzed the changes in discharge regimes
Externí odkaz:
https://doaj.org/article/c85bcbc7d07349e4994e74b0d908e736
Publikováno v:
Geoadria, Vol 18, Iss 1, Pp 29-39 (2013)
This paper investigates the changes in precipitation levels in Croatia that can be observed since the mid 20th century. Based on the data from 22 weather stations, linear trends show very little oscillation for the period 1950–2010. In eastern Croa
Externí odkaz:
https://doaj.org/article/736acb468407444e879eb4ad541fabdd
Publikováno v:
Geoadria, Vol 18, Iss 1, Pp 29-39 (2013)
padaline; Hrvatska; dugogodišnji trend
Externí odkaz:
https://doaj.org/article/a7499920936a4fb1a38b8f040faafd60
Publikováno v:
Geoadria, Vol 14, Iss 2, Pp 201-220 (2009)
Područje riječkoga vodoopskrbnog sustava pripada kršu za koji je značajno podzemno cirkuliranje vode, ali i velika osjetljivost na vanjske utjecaje, odnosno mogućnosti onečišćenja vode. Izdašni izvori temelj su vodoopskrbe. Minimalna izdašn
Externí odkaz:
https://doaj.org/article/17f65e051ab44359986621acf83a9c6d
Publikováno v:
Geoadria, Vol 14, Iss 2, Pp 201-220 (2009)
The area of Rijeka's water supply system belongs to karst which is featured with a significant underground water circulation, as well as with a high sensitivity to external influences such as water pollution. Abundant springs are the basis of water s
Externí odkaz:
https://doaj.org/article/5d5337e5a64640829f77b6589b2ee747
Autor:
Danijel Orešić, Emir Temimović
Publikováno v:
Geoadria, Vol 13, Iss 1, Pp 3-17 (2008)
U članku se razmatra godišnji hod, intenzitet i vjerojatnost padalina u poriječju Sane (u sjeverozapadnom dijelu Bosne i Hercegovine). Poriječje Sane je općenito humidno područje, a u godišnjem hodu padalina na većini postaja jasno se javljaj
Externí odkaz:
https://doaj.org/article/86feee8a90e24d43bfa76aaff4405e20
Autor:
Danijel Orešić, Emir Temimović
Publikováno v:
Geoadria, Vol 13, Iss 1, Pp 3-17 (2008)
The paper deals with the annual mean amounts, the intensity and the probability of precipitation in the drainage area of the river Sana (in the northwestern part of Bosnia and Herzegovina). Generally, the Sana drainage area is a humid region. Thus, t
Externí odkaz:
https://doaj.org/article/24e4741f55184f9e838fc64d2550a7dd
Publikováno v:
Geoadria
Volume 14
Issue 2
Geoadria, Vol 14, Iss 2, Pp 201-220 (2009)
Volume 14
Issue 2
Geoadria, Vol 14, Iss 2, Pp 201-220 (2009)
Područje riječkoga vodoopskrbnog sustava pripada kršu za koji je značajno podzemno cirkuliranje vode, ali i velika osjetljivost na vanjske utjecaje, odnosno mogućnosti onečišćenja vode. Izdašni izvori temelj su vodoopskrbe. Minimalna izdašn
Autor:
Danijel Orešić, Ivan Čanjevac
Publikováno v:
Springer Water ISBN: 9783030224677
Croatia is a middle-sized country at the south of Central Europe, a member state of the European Union (since 2013), with a land area of 56,594 km2 and total population of around 4.2 million. Despite the size, it has very heterogeneous physical-geogr
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c93167b95035d0c40ca47d281f162b4c
https://doi.org/10.1007/978-3-030-22468-4_7
https://doi.org/10.1007/978-3-030-22468-4_7
Autor:
Ivan Čanjevac, Danijel Orešić
Publikováno v:
Springer Water ISBN: 9783030224677
The quantity and distribution of groundwater resources in Croatia are determined primarily by hydrogeology and climate. The most important aquifers in inland Pannonia region are formed as alluvial deposits of intergranular porosity and of high hydrau
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d1b8e23329cab42738c9f1658a3a43c5
https://doi.org/10.1007/978-3-030-22468-4_5
https://doi.org/10.1007/978-3-030-22468-4_5