Typhon marinus
Typhon marinussivehuracanumesttempestasmarinacuiusventicircumagentesmagnaspluviascohibentes 33 m/s (118 km/h) excedunt.Antiquitatehominesverbocataegis(-idis) utebantur ad tempestates potentes inMari Mediterraneoappellandas, sed tempestates quas typhones hodie appellamus ibi numquam fiebant.PersaeetArabespostmodo nomineTyphonis,deiGraeci,utebantur ad typhones marinosSinus Indipotentes appellandos.[1]DeindenautaemediaevalesinEuropaeodem nomine usi solebant.[2]Typhonfuit deusGraecusmonstrumque,qui, secundumHesiodum,procellasemissit elacunaTartaro.Hodie,Americimalunt typhones quoque appellarefuracana.Verbumfuracanum(etiamhuracanetfuracan) provenit e nomine dei venti destructionisqueindorum AmericanorumTainietMaiae,quisextodecimo saeculoinMari Caribaeovivebant,[3]ubi multos typhones marinos quotannis pati solebant.
Incipiunt fere omnes tempestates marinae inregionibuspressionisaerisdemissae, quaeventosviolentos etinundationesper se circumagentes efficiunt. Eae tempestatesnaturaliterannumerantur secundum sui venticeleritatem.Depressiones tropicaeventos habent minores quam 17 m/s (62 km/h), tempestates tropicae (sive procellae[2]) ventos inter 17 m/s et 33 m/s (62 et 118 km/h), et typhones marini ventos qui 33 m/s (118 km/h) excedunt.[4]De typhonum marinorummagnitudinedeindesystema Saffir-SimpsonNOAA quinque gradus additionales distinguit:[5]gradum primum ventibus inter 33 m/s et 41 m/s (118 et 153 km/h), secundum ventibus inter 41 m/s et 49 m/s (154 et 177 km/h), tertium ventibus inter 49 m/s et 58 m/s (178 et 209 km/h), quartum ventibus inter 58 m/s et 69 m/s (210 et 249 km/h), quintum ventibus qui excedunt 69 m/s (249 km/h). Typhones gradus quinti ventos tam rapidos habent ut magnas alluviones 6 m supermaris aequoret magnum exitium tectisaedificationibusqueefficiant.
Nomina typhonum marinorum anno 2006 in Mari Atlantico Septentrionali
[recensere|fontem recensere]Meteorologisolent dare nomina propria tempestatibus quando status "tempestatum tropicarum" attingunt. Exempli gratia anno2006nomina typhonum marinorum fuerunt:
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Typhpnes nonnulli famosi
[recensere|fontem recensere]Nexus interni
[recensere|fontem recensere]Notae
[recensere|fontem recensere]- ↑Videpaginam Typhon apud Vicipaediam Anglicam:"Typhon is also the father of hot dangerous storm winds which issue forth from the stormy pit of Tartarus, according to Hesiod. His name is apparently derived from the Greek" typhein ", to smoke, hence it is considered to be a possible etymology for the word typhoon, supposedly borrowed by the Persians (as طوفان Tufân) and Arabs to describe the cyclonic storms of the Indian Ocean. The Greeks also frequently represented him as a storm-daemon, especially in the version where he stole Zeus's thunderbolts and wrecked the earth with storms (cf. Hesiod, Theogony; Nonnus, Dionysiaca)."
- ↑2.02.1Vide opusHistoria ventorumFrancisco Bacono auctore apud Google Books.
- ↑Videfontes, quod procellam ingentem marinam nominehuracanvelfuracanvelfuracanumdescribunt.;vide etiam paginamHuracan apud Vicipaediam Hispanicam.
- ↑De definitionibus, lege apudsitum interretialem NOAA (Anglice).
- ↑Videde systemate Saffir-Simpson NOAA (Anglice);et de vocabulograduslege apuddiarium interretialemEphemeris(Augusti 2007):"Nam quintum gradum roboris attigisse putatur typhon Dean.".
Bibliographia
[recensere|fontem recensere]- Battan, Louis Joseph.1961.The Nature of Violent Storms.Garden City Novi Eboraci: Anchor Books Doubleday & Co..
- Christopherson, R.1992.Geosystems: An Introduction to Physical Geography.Novi Eboraci: Macmillan Publishing.ISBN 0-02-322443-6.
- Elsner, James B., et Thomas H. Jagger, eds.2009.Hurricanes and climate change.Proceedings of the Summit on Hurricanes and Climate Change (Cretae,2007). Novi Eboraci: Springer.ISBN 9780387094090,ISBN 0387094091.
- Sanchez-Gonzalez, D.2011.Peligrosidad y exposición a los ciclones tropicales en ciudades del Golfo de México: El caso de Tampico.Revista de Geografía Norte Grande50:151–170. ISSN 0718-3402.
- Whipple, A. (1982),1984.Storm.Time Life Books.ISBN 0-8094-4312-0.
Nexus externi
[recensere|fontem recensere]VideTyphon marinusinVictionario. |
Vicimedia Communiaplura habent quae adtyphones marinos tropicosspectant. |
- Propria media meteorologica regionalia
- Central Pacific Hurricane Center,www.prh.noaa.gov (Pacificus Medius)
- Fiji Meteorological Service,www.met.gov.fj (PacificusAustralis ad occidentem 160°E, septentriones 25° S)
- U.S. National Hurricane Center,www.nhc.noaa.gov (AtlanticusSeptentrionalis,PacificusOrientalis)
- India Meteorological Department,www.imd.gov.in (Sinus BengaliaeetMare Arabicum)
- Japan Meteorological Agency,www.jma.go.jp (Pacificus Boreoccidentalis)
- Météo-France: La Reunion,www.meteo.fe (Oceanus Indicusa 30°E ad 90°E)
- Tropica admonitionum typhonum media
- Australian Bureau of Meteorology,www.bom.gov.au (TCWC's Perth, Darwin & Brisbane) (Oceanus Indicus et Oceanus Pacificus Australis a 90°E ad 160°E, ad australem 10°S
- Indonesian Meteorological Department,maritim.bmg.go.id (Oceanus Indicusa 90°E ad 125°E, in septentrionibus 10°S
- Meteorological Service of New Zealand Limited,metservice.com (Pacificus Australis ad occidentem 160°E, ad australem 25°S
- Quod attinet ad rationem
- Glossarium verborum de typhonibus,www.a-z-dictionaries.com
- Varia
- Atlantic Oceanographic and Meteorological Laboratory, Hurricane Research Division.Frequently Asked Questions: What are the average, most, and least tropical cyclones occurring in each basin?NOAA.
- National Hurricane Center.Tropical Prediction Center.
- Tropical Cyclones - CIMSS - UW-Madison.NASA / NOAA.
- Tropical Products - SSD.NOAA.
- Tropical Storm Risk.University College London.
- What is the difference between a hurricane, a cyclone, and a typhoon?Ocean Facts, National Ocean Service, NOAA.