C. Mares1, I. Mares1, A. Stanciu1, M. Mihailescu2, 1 National Institute of Hydrology and Water Management Sos. Bucuresti – Ploiesti, 97, Bucharest, Romania 2 Agricultural University, Bucharest, Romania constantin.mares@hidro.ro    Abstract The North Atlantic Oscillation (NAO) is represented through a circulation index which emphasizes the difference between the characteristics of the atmospheric circulation at high […]

Mihai Doroftei*, Marian Mierla Danube Delta National Institute for Research and Development, Tulcea, Romania doroftei@indd.tim.ro   Abstract Research has been conducted in the entire area covered by the Danube Delta Biosphere Reserve (Romania). Within this protected site, the Black Sea coastline as well as the area between Chilia and Sf. Gheorghe branches has been studied […]

Maria Albu Dinu1, Lidia Sălăjan2, Adrian Apostol3 1 University of Bucharest – Romanian 2National Institute of Hydrology and Water Management, University of Bucharest – Romanian 3National Institute of Hydrology and Water Management of Bucharest – Romanian, lidia.salajan@yahoo.com   Abstract The Călmăţui basin is an autochthonous river, tributary to the Danube River, situated in the Boian Plain. […]

Ion Marinica1; Andreea-Floriana Marinică2, 1 Regional Meteorological Centre Oltenia, Ph.D. Senior Researcher III, Senior Forecaster Meteorologist First Degree, National Meteorological Administration, Oltenia Regional Meteorological Centre, Craiova, Romania 2 Jacobs University Bremen, Department of Earth and Space Sciences, Bremen, Germany seryblack@yahoo.com ionmarinica@yahoo.com   Abstract We have analysed the climatic conditions in Oltenia in 2010. This paper […]

Ion Marinica1, Vaduva Iulica2 1 PhD. CS III, MMP1, Regional Meteorological Center, Craiova, Romania, ionmarinica@yahoo.com 2 Lecturer PhD., Faculty of Geography, Spiru Haret University, Bucharest, Romania iulicavaduva@yahoo.com   Abstract The cold wave from the period 23-26th of January 2010 was extremely intense. Among the effects of this climatic risk phenomenon it is worth mentioning: 22 […]

Lidia Sălăjan, Alexandrina Frâncu, Smaranda Druţă National Institute of Hydrology and Water Management-Romanian, Romania lidia.salajan@yahoo.com   Abstract In this paper, the causes of floods produced over the period January-May 2010 are identified. These ones were due to the high discharges recorded at the end of the year 2009, the precipitation amounts and the snow melting. […]

Liliana Zaharia1, Gabriel Minea1 , Gabriela Ioana-Toroimac1, Ruth Barbu2 , Ioan Sârbu1 1University of Bucharest – Faculty of Geography, Department of Meteorology and Hydrology, Bucharest, Romania 2University of Bucharest, Faculty of Geography, “Simion Mehedinţi – Nature and Sustainable Development” Doctoral School, Bucharest, Romania zaharialil@yahoo.com, gabriel.minea@gmail.com, gabriela_toroimac@yahoo.com   Abstract This paper aims to identify the areas […]

Ion Marinica1; Andreea-Floriana Marinică2, 1 Regional Meteorological Centre Oltenia, Ph.D. Senior Researcher III, Senior Forecaster Meteorologist First Degree, National Meteorological Administration, Oltenia Regional Meteorological Centre, Craiova, Romania, ionmarinica@yahoo.com 2 Jacobs University Bremen, Department of Earth and Space Sciences, Bremen, Germany seryblack@yahoo.com ionmarinica@yahoo.com   Abstract We have analysed the climatic conditions in Oltenia in 2010. This […]

Ph.D. Eng. Ec. Dan Dascaliţa “Vasile Alecsandri” University of Bacau, Romania Siret River Water Basin Administration Bacau City dan_dsclt@yahoo.com   Abstract Hydro-climatic processes and phenomena present daily, monthly, yearly and multiannual variations, situated in the general conditions of regional climate, but with multiple local variations. The rise of medium air temperature on a global level […]

Lidia Sălajan, Tudorache Nicolae, Oprea Rodflorina National Institute of Hydrology and Water Management, Romania lidia.salajan@yahoo.com   Abstract This paper highlights the main non-climatic components (relief, hydrography, geology, soil science, and vegetation) and climatic (temperature, precipitation) that influence the flow in this basin. These components have a decisive role in the formation of the river network; […]