THE BLIZZARD PHENOMENON IN SOUTHWESTERN ROMANIA

The most common situation when blizzard occurs in this region is when the East-European anticyclon’s ridge and a mediterranean low pressure field are coupled. Very rarrely the blizzard occures due to the atmospheric coupling between Azores anticyclone with a low pressure field. In this paper these p...
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Gespeichert in:

Autor*in:	BRÂNCUŞ MIHAELA [verfasserIn] BURADA CRISTINA [verfasserIn] MĂNESCU CARMEN [verfasserIn] BĂCESCU M. [verfasserIn]

Format:	E-Artikel
Sprache:	Englisch

Erschienen:	2014

Schlagwörter:	blizzard snowfall wind gust anticyclone cyclone

Übergeordnetes Werk:	In: Aerul şi Apa: Componente ale Mediului - Cluj University Press, 2010, (2014), Seite 338-345
Übergeordnetes Werk:	year:2014 ; pages:338-345

Links:	Link aufrufen Link aufrufen Journal toc Journal toc

Katalog-ID:	DOAJ05238599X

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520			\|a The most common situation when blizzard occurs in this region is when the East-European anticyclon’s ridge and a mediterranean low pressure field are coupled. Very rarrely the blizzard occures due to the atmospheric coupling between Azores anticyclone with a low pressure field. In this paper these posibillities of blizzard’s occurrence are studied. Their specific elements were compared in order to help operational activity of weather forecasters. For establishing the synoptic and mesoscale contexts that had generated the severe weather events listed below, global numerical model output -ECMWF (European Centre for Mediumum-Range Weather Forecast) and short-range numerical model output - ALADIN, EUMETSAT satellite imagies, maps using data from ESTOFEX site and observational data from meteorological stations, validated and administrated by National Meteorological Administration were used.
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allfields	(DE-627)DOAJ05238599X (DE-599)DOAJefe75c86bd9a493fb795d7397e5309ca DE-627 ger DE-627 rakwb eng QC851-999 BRÂNCUŞ MIHAELA verfasserin aut THE BLIZZARD PHENOMENON IN SOUTHWESTERN ROMANIA 2014 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier The most common situation when blizzard occurs in this region is when the East-European anticyclon’s ridge and a mediterranean low pressure field are coupled. Very rarrely the blizzard occures due to the atmospheric coupling between Azores anticyclone with a low pressure field. In this paper these posibillities of blizzard’s occurrence are studied. Their specific elements were compared in order to help operational activity of weather forecasters. For establishing the synoptic and mesoscale contexts that had generated the severe weather events listed below, global numerical model output -ECMWF (European Centre for Mediumum-Range Weather Forecast) and short-range numerical model output - ALADIN, EUMETSAT satellite imagies, maps using data from ESTOFEX site and observational data from meteorological stations, validated and administrated by National Meteorological Administration were used. blizzard snowfall wind gust anticyclone cyclone Meteorology. Climatology BURADA CRISTINA verfasserin aut MĂNESCU CARMEN verfasserin aut BĂCESCU M. verfasserin aut In Aerul şi Apa: Componente ale Mediului Cluj University Press, 2010 (2014), Seite 338-345 (DE-627)662163877 (DE-600)2612709-X 2067743X nnns year:2014 pages:338-345 https://doaj.org/article/efe75c86bd9a493fb795d7397e5309ca kostenfrei http://aerapa.conference.ubbcluj.ro/2014/PDF/45-Brancus.pdf kostenfrei https://doaj.org/toc/2067-743X Journal toc kostenfrei https://doaj.org/toc/2067-743X Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2014 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4367 GBV_ILN_4700 AR 2014 338-345
spelling	(DE-627)DOAJ05238599X (DE-599)DOAJefe75c86bd9a493fb795d7397e5309ca DE-627 ger DE-627 rakwb eng QC851-999 BRÂNCUŞ MIHAELA verfasserin aut THE BLIZZARD PHENOMENON IN SOUTHWESTERN ROMANIA 2014 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier The most common situation when blizzard occurs in this region is when the East-European anticyclon’s ridge and a mediterranean low pressure field are coupled. Very rarrely the blizzard occures due to the atmospheric coupling between Azores anticyclone with a low pressure field. In this paper these posibillities of blizzard’s occurrence are studied. Their specific elements were compared in order to help operational activity of weather forecasters. For establishing the synoptic and mesoscale contexts that had generated the severe weather events listed below, global numerical model output -ECMWF (European Centre for Mediumum-Range Weather Forecast) and short-range numerical model output - ALADIN, EUMETSAT satellite imagies, maps using data from ESTOFEX site and observational data from meteorological stations, validated and administrated by National Meteorological Administration were used. blizzard snowfall wind gust anticyclone cyclone Meteorology. Climatology BURADA CRISTINA verfasserin aut MĂNESCU CARMEN verfasserin aut BĂCESCU M. verfasserin aut In Aerul şi Apa: Componente ale Mediului Cluj University Press, 2010 (2014), Seite 338-345 (DE-627)662163877 (DE-600)2612709-X 2067743X nnns year:2014 pages:338-345 https://doaj.org/article/efe75c86bd9a493fb795d7397e5309ca kostenfrei http://aerapa.conference.ubbcluj.ro/2014/PDF/45-Brancus.pdf kostenfrei https://doaj.org/toc/2067-743X Journal toc kostenfrei https://doaj.org/toc/2067-743X Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2014 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4367 GBV_ILN_4700 AR 2014 338-345
allfields_unstemmed	(DE-627)DOAJ05238599X (DE-599)DOAJefe75c86bd9a493fb795d7397e5309ca DE-627 ger DE-627 rakwb eng QC851-999 BRÂNCUŞ MIHAELA verfasserin aut THE BLIZZARD PHENOMENON IN SOUTHWESTERN ROMANIA 2014 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier The most common situation when blizzard occurs in this region is when the East-European anticyclon’s ridge and a mediterranean low pressure field are coupled. Very rarrely the blizzard occures due to the atmospheric coupling between Azores anticyclone with a low pressure field. In this paper these posibillities of blizzard’s occurrence are studied. Their specific elements were compared in order to help operational activity of weather forecasters. For establishing the synoptic and mesoscale contexts that had generated the severe weather events listed below, global numerical model output -ECMWF (European Centre for Mediumum-Range Weather Forecast) and short-range numerical model output - ALADIN, EUMETSAT satellite imagies, maps using data from ESTOFEX site and observational data from meteorological stations, validated and administrated by National Meteorological Administration were used. blizzard snowfall wind gust anticyclone cyclone Meteorology. Climatology BURADA CRISTINA verfasserin aut MĂNESCU CARMEN verfasserin aut BĂCESCU M. verfasserin aut In Aerul şi Apa: Componente ale Mediului Cluj University Press, 2010 (2014), Seite 338-345 (DE-627)662163877 (DE-600)2612709-X 2067743X nnns year:2014 pages:338-345 https://doaj.org/article/efe75c86bd9a493fb795d7397e5309ca kostenfrei http://aerapa.conference.ubbcluj.ro/2014/PDF/45-Brancus.pdf kostenfrei https://doaj.org/toc/2067-743X Journal toc kostenfrei https://doaj.org/toc/2067-743X Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2014 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4367 GBV_ILN_4700 AR 2014 338-345
allfieldsGer	(DE-627)DOAJ05238599X (DE-599)DOAJefe75c86bd9a493fb795d7397e5309ca DE-627 ger DE-627 rakwb eng QC851-999 BRÂNCUŞ MIHAELA verfasserin aut THE BLIZZARD PHENOMENON IN SOUTHWESTERN ROMANIA 2014 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier The most common situation when blizzard occurs in this region is when the East-European anticyclon’s ridge and a mediterranean low pressure field are coupled. Very rarrely the blizzard occures due to the atmospheric coupling between Azores anticyclone with a low pressure field. In this paper these posibillities of blizzard’s occurrence are studied. Their specific elements were compared in order to help operational activity of weather forecasters. For establishing the synoptic and mesoscale contexts that had generated the severe weather events listed below, global numerical model output -ECMWF (European Centre for Mediumum-Range Weather Forecast) and short-range numerical model output - ALADIN, EUMETSAT satellite imagies, maps using data from ESTOFEX site and observational data from meteorological stations, validated and administrated by National Meteorological Administration were used. blizzard snowfall wind gust anticyclone cyclone Meteorology. Climatology BURADA CRISTINA verfasserin aut MĂNESCU CARMEN verfasserin aut BĂCESCU M. verfasserin aut In Aerul şi Apa: Componente ale Mediului Cluj University Press, 2010 (2014), Seite 338-345 (DE-627)662163877 (DE-600)2612709-X 2067743X nnns year:2014 pages:338-345 https://doaj.org/article/efe75c86bd9a493fb795d7397e5309ca kostenfrei http://aerapa.conference.ubbcluj.ro/2014/PDF/45-Brancus.pdf kostenfrei https://doaj.org/toc/2067-743X Journal toc kostenfrei https://doaj.org/toc/2067-743X Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2014 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4367 GBV_ILN_4700 AR 2014 338-345
allfieldsSound	(DE-627)DOAJ05238599X (DE-599)DOAJefe75c86bd9a493fb795d7397e5309ca DE-627 ger DE-627 rakwb eng QC851-999 BRÂNCUŞ MIHAELA verfasserin aut THE BLIZZARD PHENOMENON IN SOUTHWESTERN ROMANIA 2014 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier The most common situation when blizzard occurs in this region is when the East-European anticyclon’s ridge and a mediterranean low pressure field are coupled. Very rarrely the blizzard occures due to the atmospheric coupling between Azores anticyclone with a low pressure field. In this paper these posibillities of blizzard’s occurrence are studied. Their specific elements were compared in order to help operational activity of weather forecasters. For establishing the synoptic and mesoscale contexts that had generated the severe weather events listed below, global numerical model output -ECMWF (European Centre for Mediumum-Range Weather Forecast) and short-range numerical model output - ALADIN, EUMETSAT satellite imagies, maps using data from ESTOFEX site and observational data from meteorological stations, validated and administrated by National Meteorological Administration were used. blizzard snowfall wind gust anticyclone cyclone Meteorology. Climatology BURADA CRISTINA verfasserin aut MĂNESCU CARMEN verfasserin aut BĂCESCU M. verfasserin aut In Aerul şi Apa: Componente ale Mediului Cluj University Press, 2010 (2014), Seite 338-345 (DE-627)662163877 (DE-600)2612709-X 2067743X nnns year:2014 pages:338-345 https://doaj.org/article/efe75c86bd9a493fb795d7397e5309ca kostenfrei http://aerapa.conference.ubbcluj.ro/2014/PDF/45-Brancus.pdf kostenfrei https://doaj.org/toc/2067-743X Journal toc kostenfrei https://doaj.org/toc/2067-743X Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2014 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4367 GBV_ILN_4700 AR 2014 338-345
language	English
source	In Aerul şi Apa: Componente ale Mediului (2014), Seite 338-345 year:2014 pages:338-345
sourceStr	In Aerul şi Apa: Componente ale Mediului (2014), Seite 338-345 year:2014 pages:338-345
format_phy_str_mv	Article
institution	findex.gbv.de
topic_facet	blizzard snowfall wind gust anticyclone cyclone Meteorology. Climatology
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container_title	Aerul şi Apa: Componente ale Mediului
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callnumber-first	Q - Science
author	BRÂNCUŞ MIHAELA
spellingShingle	BRÂNCUŞ MIHAELA misc QC851-999 misc blizzard misc snowfall misc wind gust misc anticyclone misc cyclone misc Meteorology. Climatology THE BLIZZARD PHENOMENON IN SOUTHWESTERN ROMANIA
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topic_title	QC851-999 THE BLIZZARD PHENOMENON IN SOUTHWESTERN ROMANIA blizzard snowfall wind gust anticyclone cyclone
topic	misc QC851-999 misc blizzard misc snowfall misc wind gust misc anticyclone misc cyclone misc Meteorology. Climatology
topic_unstemmed	misc QC851-999 misc blizzard misc snowfall misc wind gust misc anticyclone misc cyclone misc Meteorology. Climatology
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title	THE BLIZZARD PHENOMENON IN SOUTHWESTERN ROMANIA
ctrlnum	(DE-627)DOAJ05238599X (DE-599)DOAJefe75c86bd9a493fb795d7397e5309ca
title_full	THE BLIZZARD PHENOMENON IN SOUTHWESTERN ROMANIA
author_sort	BRÂNCUŞ MIHAELA
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author-letter	BRÂNCUŞ MIHAELA
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title_sort	blizzard phenomenon in southwestern romania
callnumber	QC851-999
title_auth	THE BLIZZARD PHENOMENON IN SOUTHWESTERN ROMANIA
abstract	The most common situation when blizzard occurs in this region is when the East-European anticyclon’s ridge and a mediterranean low pressure field are coupled. Very rarrely the blizzard occures due to the atmospheric coupling between Azores anticyclone with a low pressure field. In this paper these posibillities of blizzard’s occurrence are studied. Their specific elements were compared in order to help operational activity of weather forecasters. For establishing the synoptic and mesoscale contexts that had generated the severe weather events listed below, global numerical model output -ECMWF (European Centre for Mediumum-Range Weather Forecast) and short-range numerical model output - ALADIN, EUMETSAT satellite imagies, maps using data from ESTOFEX site and observational data from meteorological stations, validated and administrated by National Meteorological Administration were used.
abstractGer	The most common situation when blizzard occurs in this region is when the East-European anticyclon’s ridge and a mediterranean low pressure field are coupled. Very rarrely the blizzard occures due to the atmospheric coupling between Azores anticyclone with a low pressure field. In this paper these posibillities of blizzard’s occurrence are studied. Their specific elements were compared in order to help operational activity of weather forecasters. For establishing the synoptic and mesoscale contexts that had generated the severe weather events listed below, global numerical model output -ECMWF (European Centre for Mediumum-Range Weather Forecast) and short-range numerical model output - ALADIN, EUMETSAT satellite imagies, maps using data from ESTOFEX site and observational data from meteorological stations, validated and administrated by National Meteorological Administration were used.
abstract_unstemmed	The most common situation when blizzard occurs in this region is when the East-European anticyclon’s ridge and a mediterranean low pressure field are coupled. Very rarrely the blizzard occures due to the atmospheric coupling between Azores anticyclone with a low pressure field. In this paper these posibillities of blizzard’s occurrence are studied. Their specific elements were compared in order to help operational activity of weather forecasters. For establishing the synoptic and mesoscale contexts that had generated the severe weather events listed below, global numerical model output -ECMWF (European Centre for Mediumum-Range Weather Forecast) and short-range numerical model output - ALADIN, EUMETSAT satellite imagies, maps using data from ESTOFEX site and observational data from meteorological stations, validated and administrated by National Meteorological Administration were used.
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title_short	THE BLIZZARD PHENOMENON IN SOUTHWESTERN ROMANIA
url	https://doaj.org/article/efe75c86bd9a493fb795d7397e5309ca http://aerapa.conference.ubbcluj.ro/2014/PDF/45-Brancus.pdf https://doaj.org/toc/2067-743X
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up_date	2024-07-04T00:51:55.198Z
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THE BLIZZARD PHENOMENON IN SOUTHWESTERN ROMANIA

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Zugang & Verfügbarkeit

Vorhandene Bände

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