@article{mikolaskovaContinentalOceanicPrecipitation2009,
  title = {Continental and Oceanic Precipitation Régime in {{Europe}}},
  author = {Mikolaskova, Katerina},
  date = {2009-06},
  journaltitle = {Open Geosciences},
  volume = {1},
  pages = {176+},
  issn = {2391-5447},
  doi = {10.2478/v10085-009-0013-8},
  url = {https://doi.org/10.2478/v10085-009-0013-8},
  abstract = {This work considers continentality from the point of view of an annual course of precipitation. It assesses continentality according to percentage of precipitation in summer and winter half year, ratio of precipitation in summer to winter half year and the period of half year precipitation in the area of WMO Region VI (Europe). Region VI can be divided into five main regions according to their annual course of precipitation. These regions are: Northwestern Europe with precipitation in all seasons, a predominance of winter precipitation and maximum precipitation in December and January; Central Europe with precipitation in all seasons, a predominance of summer precipitation and maximum precipitation in July; Eastern Europe with less precipitation over the year than in Northwestern Europe, a predominance of summer precipitation and maximum precipitation in July; the Mediterranean region with a predominance of winter precipitation, a dry season in summer and maximum precipitation in November and December; and Western Asia with a variable climate, a predominance of winter precipitation and maximum precipitation in December and January. Continentality from the point of view of precipitation rises towards the east. In comparison with thermal continentality, according to Gorczynski, it unexpectedly reaches its maximum in the centre of Europe (especially in northeast of the Czech Republic and south of Poland).},
  keywords = {*imported-from-citeulike-INRMM,~INRMM-MiD:c-14689593,bioclimatic-predictors,ecological-zones,europe,maritime-climate,mediterranean-region,precipitation,winter-vs-summer},
  number = {2}
}

{"_id":"R3FT3SuRBDuek4Evf","bibbaseid":"mikolaskova-continentalandoceanicprecipitationrgimeineurope","authorIDs":[],"author_short":["Mikolaskova, K."],"bibdata":{"bibtype":"article","type":"article","title":"Continental and Oceanic Precipitation Régime in Europe","author":[{"propositions":[],"lastnames":["Mikolaskova"],"firstnames":["Katerina"],"suffixes":[]}],"date":"2009-06","journaltitle":"Open Geosciences","volume":"1","pages":"176+","issn":"2391-5447","doi":"10.2478/v10085-009-0013-8","url":"https://doi.org/10.2478/v10085-009-0013-8","abstract":"This work considers continentality from the point of view of an annual course of precipitation. It assesses continentality according to percentage of precipitation in summer and winter half year, ratio of precipitation in summer to winter half year and the period of half year precipitation in the area of WMO Region VI (Europe). Region VI can be divided into five main regions according to their annual course of precipitation. These regions are: Northwestern Europe with precipitation in all seasons, a predominance of winter precipitation and maximum precipitation in December and January; Central Europe with precipitation in all seasons, a predominance of summer precipitation and maximum precipitation in July; Eastern Europe with less precipitation over the year than in Northwestern Europe, a predominance of summer precipitation and maximum precipitation in July; the Mediterranean region with a predominance of winter precipitation, a dry season in summer and maximum precipitation in November and December; and Western Asia with a variable climate, a predominance of winter precipitation and maximum precipitation in December and January. Continentality from the point of view of precipitation rises towards the east. In comparison with thermal continentality, according to Gorczynski, it unexpectedly reaches its maximum in the centre of Europe (especially in northeast of the Czech Republic and south of Poland).","keywords":"*imported-from-citeulike-INRMM,~INRMM-MiD:c-14689593,bioclimatic-predictors,ecological-zones,europe,maritime-climate,mediterranean-region,precipitation,winter-vs-summer","number":"2","bibtex":"@article{mikolaskovaContinentalOceanicPrecipitation2009,\n title = {Continental and Oceanic Precipitation Régime in {{Europe}}},\n author = {Mikolaskova, Katerina},\n date = {2009-06},\n journaltitle = {Open Geosciences},\n volume = {1},\n pages = {176+},\n issn = {2391-5447},\n doi = {10.2478/v10085-009-0013-8},\n url = {https://doi.org/10.2478/v10085-009-0013-8},\n abstract = {This work considers continentality from the point of view of an annual course of precipitation. It assesses continentality according to percentage of precipitation in summer and winter half year, ratio of precipitation in summer to winter half year and the period of half year precipitation in the area of WMO Region VI (Europe). Region VI can be divided into five main regions according to their annual course of precipitation. These regions are: Northwestern Europe with precipitation in all seasons, a predominance of winter precipitation and maximum precipitation in December and January; Central Europe with precipitation in all seasons, a predominance of summer precipitation and maximum precipitation in July; Eastern Europe with less precipitation over the year than in Northwestern Europe, a predominance of summer precipitation and maximum precipitation in July; the Mediterranean region with a predominance of winter precipitation, a dry season in summer and maximum precipitation in November and December; and Western Asia with a variable climate, a predominance of winter precipitation and maximum precipitation in December and January. Continentality from the point of view of precipitation rises towards the east. In comparison with thermal continentality, according to Gorczynski, it unexpectedly reaches its maximum in the centre of Europe (especially in northeast of the Czech Republic and south of Poland).},\n keywords = {*imported-from-citeulike-INRMM,~INRMM-MiD:c-14689593,bioclimatic-predictors,ecological-zones,europe,maritime-climate,mediterranean-region,precipitation,winter-vs-summer},\n number = {2}\n}\n\n","author_short":["Mikolaskova, K."],"key":"mikolaskovaContinentalOceanicPrecipitation2009","id":"mikolaskovaContinentalOceanicPrecipitation2009","bibbaseid":"mikolaskova-continentalandoceanicprecipitationrgimeineurope","role":"author","urls":{"Paper":"https://doi.org/10.2478/v10085-009-0013-8"},"keyword":["*imported-from-citeulike-INRMM","~INRMM-MiD:c-14689593","bioclimatic-predictors","ecological-zones","europe","maritime-climate","mediterranean-region","precipitation","winter-vs-summer"],"downloads":0},"bibtype":"article","biburl":"https://tmpfiles.org/dl/58794/INRMM.bib","creationDate":"2020-07-02T22:41:15.245Z","downloads":0,"keywords":["*imported-from-citeulike-inrmm","~inrmm-mid:c-14689593","bioclimatic-predictors","ecological-zones","europe","maritime-climate","mediterranean-region","precipitation","winter-vs-summer"],"search_terms":["continental","oceanic","precipitation","gime","europe","mikolaskova"],"title":"Continental and Oceanic Precipitation Régime in Europe","year":null,"dataSources":["DXuKbcZTirdigFKPF"]}