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Statements

Subject Item: dbr:Cagayan_de_Oro
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Subject Item: dbr:Typhoon_Meranti_(2004)
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Subject Item: dbr:Mesocyclone
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Subject Item: dbr:Meteorological_history_of_Hurricane_Gordon
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Subject Item: dbr:Meteorological_history_of_Hurricane_Luis
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Subject Item: dbr:Tropical_Depression_Twelve-E_(2011)
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Subject Item: dbr:Tropical_Storm_Becky_(1970)
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Subject Item: dbr:Winter_flooding_of_2013–14_on_the_Somerset_Levels
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Subject Item: dbr:Tropical_Storm_Odile_(2008)
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Subject Item: dbr:December_2015_North_American_storm_complex
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Subject Item: dbr:Anticyclone
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Subject Item: dbr:Anticyclonic_rotation
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Subject Item: dbr:Holt-Bragg_Bridge
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Subject Item: dbr:Hurricane_Adrian_(2005)
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Subject Item: dbr:Hurricane_Alma_(1966)
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Subject Item: dbr:Hurricane_Bertha_(2014)
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Subject Item: dbr:Hurricane_Bob_(1979)
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Subject Item: dbr:Hurricane_Bret
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Subject Item: dbr:Hurricane_Danny_(1985)
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Subject Item: dbr:Hurricane_Dean
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Subject Item: dbr:Hurricane_Dorian
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Subject Item: dbr:Hurricane_Earl_(2016)
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Subject Item: dbr:Hurricane_Emilia_(1994)
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Subject Item: dbr:Hurricane_Fifi–Orlene
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Subject Item: dbr:Hurricane_Florence
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Subject Item: dbr:Hurricane_Greta_(1956)
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Subject Item: dbr:Hurricane_Hugo
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Subject Item: dbr:Hurricane_Ike
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Subject Item: dbr:Hurricane_Irma
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Subject Item: dbr:Hurricane_Isabel
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Subject Item: dbr:Hurricane_Jerry_(1989)
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Subject Item: dbr:Hurricane_Karl
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Subject Item: dbr:Hurricane_Kyle_(2002)
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Subject Item: dbr:Hurricane_Laura
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Subject Item: dbr:Hurricane_Leslie_(2018)
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Subject Item: dbr:Hurricane_Opal
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Subject Item: dbr:Hurricane_Ophelia_(2005)
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Subject Item: dbr:Hurricane_Pali
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Subject Item: dbr:Hurricane_Patricia
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Subject Item: dbr:Hurricane_Raymond_(2013)
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Subject Item: dbr:Hurricane_Rick_(2009)
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Subject Item: dbr:Hurricane_Sandra_(2015)
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Subject Item: dbr:Hurricane_Sergio_(2018)
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Subject Item: dbr:List_of_Category_1_Pacific_hurricanes
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Subject Item: dbr:List_of_Category_2_Pacific_hurricanes
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Subject Item: dbr:List_of_Category_3_Pacific_hurricanes
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Subject Item: dbr:List_of_Eastern_Pacific_tropical_storms
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Subject Item: dbr:List_of_retired_Australian_region_cyclone_names
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Subject Item: dbr:Peasedown_St_John
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Subject Item: dbr:Cyclogenesis
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Subject Item: dbr:2006_Pacific_typhoon_season
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Subject Item: dbr:2006–07_Australian_region_cyclone_season
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Subject Item: dbr:2006–07_South-West_Indian_Ocean_cyclone_season
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Subject Item: dbr:2007_Atlantic_hurricane_season
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Subject Item: dbr:1953_Pacific_hurricane_season
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Subject Item: dbr:1954_Pacific_hurricane_season
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Subject Item: dbr:1956_Atlantic_hurricane_season
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Subject Item: dbr:1959_Atlantic_hurricane_season
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Subject Item: dbr:1960_Atlantic_hurricane_season
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Subject Item: dbr:1961_Atlantic_hurricane_season
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Subject Item: dbr:1963_Pacific_typhoon_season
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Subject Item: dbr:1964_Atlantic_hurricane_season
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Subject Item: dbr:1964_Rameswaram_cyclone
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Subject Item: dbr:1965_Atlantic_hurricane_season
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Subject Item: dbr:1967_Atlantic_hurricane_season
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Subject Item: dbr:1967_Oak_Lawn_tornado_outbreak
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Subject Item: dbr:1968_Burma_cyclone
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Subject Item: dbr:1968_Pacific_hurricane_season
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Subject Item: dbr:Backwell
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Subject Item: dbr:Banwell
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Subject Item: dbr:British_Isles
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Subject Item: dbr:Burnett,_Somerset
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Subject Item: dbr:Burnham-on-Sea
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Subject Item: dbr:Timeline_of_the_2008_Atlantic_hurricane_season
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Subject Item: dbr:Timeline_of_the_2019_Atlantic_hurricane_season
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Subject Item: dbr:Tornado
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Subject Item: dbr:Tornado_outbreak_of_April_22–23,_2020
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Subject Item: dbr:Tornado_outbreak_of_April_27–29,_1912
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Subject Item: dbr:Tornado_outbreak_of_April_27–30,_2014
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Subject Item: dbr:Tornado_outbreak_of_April_2–3,_1956
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Subject Item: dbr:Tornado_outbreak_of_April_3,_2012
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Subject Item: dbr:Tornado_outbreak_of_April_30_–_May_2,_1967
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Subject Item: dbr:Tornado_outbreak_of_April_4–5,_1966
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Subject Item: dbr:Tornado_outbreak_of_February_28_–_March_1,_2017
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Subject Item: dbr:Tornado_outbreak_of_February_28_–_March_2,_2007
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Subject Item: dbr:Tornado_outbreak_of_February_5–7,_2020
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Subject Item: dbr:Tornado_outbreak_of_January_21–23,_1999
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Subject Item: dbr:Tornado_outbreak_of_June_16–18,_2014
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Subject Item: dbr:Tornado_outbreak_of_June_19,_1951
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Subject Item: dbr:Tornado_outbreak_of_Leap_Day_1952
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Subject Item: dbr:Tornado_outbreak_of_March_27,_1890
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Subject Item: dbr:Tornado_outbreak_of_March_28–31,_2007
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Subject Item: dbr:Tornado_outbreak_of_March_29–31,_2022
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Subject Item: dbr:Tornado_outbreak_of_March_2–3,_2012
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Subject Item: dbr:Tornado_outbreak_of_March_2–3,_2020
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Subject Item: dbr:Tornado_outbreak_of_March_3,_2019
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Subject Item: dbr:Tornado_outbreak_of_March_6–7,_2017
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Subject Item: dbr:Tornado_outbreak_of_May_15–17,_2013
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Subject Item: dbr:Tornado_outbreak_of_May_18–21,_2013
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Subject Item: dbr:Tornado_outbreak_of_May_24–25,_1957
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Subject Item: dbr:Tornado_outbreak_of_October_20–22,_2019
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Subject Item: dbr:Tornado_outbreak_of_September_24,_2001
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Subject Item: dbr:Tornado_outbreak_sequence_of_April_19–24,_2011
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Subject Item: dbr:Tornado_outbreak_sequence_of_April_2–5,_1957
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Subject Item: dbr:Tornado_outbreak_sequence_of_December_18–20,_1957
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Subject Item: dbr:Tornado_outbreak_sequence_of_June_20–23,_1957
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Subject Item: dbr:Tornado_outbreak_sequence_of_May_21–26,_2011
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Subject Item: dbr:Tornado_outbreak_sequence_of_May_25–June_1,_1917
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Subject Item: dbr:Tornadoes_of_1999
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Subject Item: dbr:Tornadoes_of_2012
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Subject Item: dbr:Tri-State_tornado_outbreak
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Subject Item: dbr:Tropical_Storm_Andrea_(2013)
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Subject Item: dbr:Tropical_Storm_Arlene_(1993)
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Subject Item: dbr:Tropical_Storm_Bret_(1981)
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Subject Item: dbr:Tropical_Storm_Chanthu_(2004)
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Subject Item: dbr:Tropical_Storm_Debbie_(1965)
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Subject Item: dbr:Tropical_Storm_Etau_(2009)
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Subject Item: dbr:Tropical_Storm_Flossie_(2013)
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Subject Item: dbr:Tropical_Storm_Gil_(2007)
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Subject Item: dbr:Tropical_Storm_Gladys_(1991)
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Subject Item: dbr:Tropical_Storm_Hermine_(2010)
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Subject Item: dbr:Tropical_Storm_Irving_(1992)
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Subject Item: dbr:Tropical_Storm_Lidia_(2017)
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Subject Item: dbr:Tropical_Storm_Marco_(2008)
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Subject Item: dbr:Tropical_Storm_Olga_(2019)
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Subject Item: dbr:Tropical_Storm_Toraji_(2007)
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Subject Item: dbr:Tropical_Storm_Winona_(1990)
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Subject Item: dbr:Tropical_Storm_Zelda_(1991)
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Subject Item: dbr:Tropical_cyclones_in_2002
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Subject Item: dbr:Tropical_cyclones_in_2009
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Subject Item: dbr:Tropical_cyclones_in_2020
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Subject Item: dbr:Typhoon_Agnes_(1981)
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Subject Item: dbr:Typhoon_Bilis_(2000)
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Subject Item: dbr:Typhoon_Choi-wan_(2009)
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Subject Item: dbr:Typhoon_Dujuan_(2015)
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Subject Item: dbr:Typhoon_Gay_(1989)
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Subject Item: dbr:Typhoon_Haiyan
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Subject Item: dbr:Typhoon_Halong_(2014)
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Subject Item: dbr:Typhoon_Megi_(2016)
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Subject Item: dbr:Typhoon_Nanmadol_(2004)
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Subject Item: dbr:Typhoon_Nuri_(2014)
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Subject Item: dbr:Typhoon_Ophelia
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Subject Item: dbr:Typhoon_Sally_(1996)
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Subject Item: dbr:Typhoon_Saomai_(2000)
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Subject Item: dbr:Typhoon_Vera
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Subject Item: dbr:Typhoon_Zola
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Subject Item: dbr:Wake_low
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Subject Item: dbr:Washington_(state)
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Subject Item: dbr:Weather_of_2020
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Subject Item: dbr:Wedmore
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Subject Item: dbr:Weston-super-Mare
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Subject Item: dbr:Westonzoyland
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Subject Item: dbr:Windsor_Locks,_Connecticut,_tornado
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Subject Item: dbr:Winter_of_1946–47_in_the_United_Kingdom
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Subject Item: dbr:Winter_of_2009–10_in_Europe
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Subject Item: dbr:Gale_warning
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Subject Item: dbr:Cyclonic_vortex
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Subject Item: dbr:Heat_wave
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Subject Item: dbr:Johnstown_Flood
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Subject Item: dbr:June_1990_Lower_Ohio_Valley_tornado_outbreak
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Subject Item: dbr:June_2010_Northern_Plains_tornado_outbreak
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Subject Item: dbr:June_2019_Southern_and_Southeastern_U.S._flooding
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Subject Item: dbr:Late-May_2010_tornado_outbreak
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Subject Item: dbr:Line_echo_wave_pattern
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Subject Item: dbr:Tropical_Storm_Arthur_(2008)
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Subject Item: dbr:Tropical_Storm_Dolly_(2014)
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Subject Item: dbr:Tropical_Storm_Gabrielle_(2007)
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Subject Item: dbr:Tropical_Storm_Rumbia_(2000)
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Subject Item: dbr:Tropical_Storm_Talas_(2011)
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Subject Item: dbr:Pressure_system
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Subject Item: dbr:Tropical_Storm_Alberto_(1994)
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Subject Item: dbr:Tropical_Storm_Colin_(2010)
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Subject Item: dbr:Tropical_Storm_Bret_(2011)
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Subject Item: dbr:2013–14_Australian_region_cyclone_season
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Subject Item: dbr:Atmospheric_circulation
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Subject Item: dbr:Atmospheric_model
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Subject Item: dbr:Isle_Abbots
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Subject Item: dbr:January_2015_North_American_blizzard
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Subject Item: dbr:January_2016_United_States_blizzard
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Subject Item: dbr:January_2018_North_American_blizzard
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Subject Item: dbr:January_2022_North_American_blizzard
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Subject Item: dbr:Taunton
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Subject Item: dbr:Teignmouth
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Subject Item: dbr:Hurricane_Adrian_(1999)
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Subject Item: dbr:Hurricane_Adrian_(2011)
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Subject Item: dbr:Hurricane_Alex_(2010)
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Subject Item: dbr:Hurricane_Ana
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Subject Item: dbr:Hurricane_Arthur
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Subject Item: dbr:Hurricane_Barbara_(2013)
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Subject Item: dbr:Hurricane_Beatriz_(2011)
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Subject Item: dbr:Hurricane_Belle
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Subject Item: dbr:Hurricane_Bertha_(2008)
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Subject Item: dbr:Hurricane_Beta
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Subject Item: dbr:Hurricane_Beulah
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Subject Item: dbr:Hurricane_Blanca_(2015)
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Subject Item: dbr:Hurricane_Bud_(2012)
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Subject Item: dbr:Hurricane_Bud_(2018)
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Subject Item: dbr:Hurricane_Celia_(2010)
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Subject Item: dbr:Hurricane_Charley_(1986)
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Subject Item: dbr:Hurricane_Cindy_(1959)
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Subject Item: dbr:Hurricane_Dalilia
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Subject Item: dbr:Hurricane_Daniel_(2006)
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Subject Item: dbr:Hurricane_Danny_(2015)
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Subject Item: dbr:Hurricane_Debbie_(1961)
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Subject Item: dbr:Hurricane_Debby_(2000)
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Subject Item: dbr:Hurricane_Delta
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Subject Item: dbr:Hurricane_Dennis_(1999)
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Subject Item: dbr:Hurricane_Dora
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Subject Item: dbr:Hurricane_Dora_(2011)
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Subject Item: dbr:Hurricane_Earl_(1998)
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Subject Item: dbr:Hurricane_Earl_(2010)
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Subject Item: dbr:Hurricane_Enrique_(2021)
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Subject Item: dbr:Hurricane_Epsilon_(2020)
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Subject Item: dbr:Hurricane_Erick_(2013)
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Subject Item: dbr:Hurricane_Erin_(1995)
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Subject Item: dbr:Hurricane_Erin_(2001)
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Subject Item: dbr:Hurricane_Ernesto_(2006)
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Subject Item: dbr:Hurricane_Florence_(2000)
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Subject Item: dbr:Hurricane_Fox_(1952)
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Subject Item: dbr:Hurricane_Fran
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Subject Item: dbr:Hurricane_Fran_(1973)
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Subject Item: dbr:Hurricane_Fred_(2009)
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Subject Item: dbr:Hurricane_Fred_(2015)
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Subject Item: dbr:Hurricane_Genevieve_(2014)
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Subject Item: dbr:Hurricane_Genevieve_(2020)
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Subject Item: dbr:Hurricane_Gert
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Subject Item: dbr:Hurricane_Gert_(2017)
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Subject Item: dbr:Hurricane_Gladys_(1968)
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Subject Item: dbr:Hurricane_Gonzalo
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Subject Item: dbr:Hurricane_Greg_(1999)
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Subject Item: dbr:Hurricane_Guillermo_(1997)
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Subject Item: dbr:Hurricane_Hattie
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Subject Item: dbr:Hurricane_Hector_(2018)
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Subject Item: dbr:Hurricane_Hernan_(2002)
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Subject Item: dbr:Hurricane_Hilary_(2011)
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Subject Item: dbr:Hurricane_Howard_(2004)
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Subject Item: dbr:Hurricane_Humberto_(2001)
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Subject Item: dbr:Hurricane_Humberto_(2019)
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Subject Item: dbr:Hurricane_Ian
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Subject Item: dbr:Hurricane_Ida_(2009)
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Subject Item: dbr:Hurricane_Igor
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Subject Item: dbr:Hurricane_Iota
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Subject Item: dbr:Hurricane_Irene
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Subject Item: dbr:Hurricane_Isaac_(2012)
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Subject Item: dbr:Hurricane_Isbell
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Subject Item: dbr:Hurricane_Iselle
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Subject Item: dbr:Hurricane_Jimena_(2009)
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Subject Item: dbr:Hurricane_Joaquin
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Subject Item: dbr:Hurricane_Jova_(2011)
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Subject Item: dbr:Hurricane_Julia_(2010)
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Subject Item: dbr:Hurricane_Kathleen
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Subject Item: dbr:Hurricane_Katia_(2017)
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Subject Item: dbr:Hurricane_Kiko_(1989)
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Subject Item: dbr:Hurricane_Lane_(2018)
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Subject Item: dbr:Hurricane_Lenny
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Subject Item: dbr:Hurricane_Linda_(2015)
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Subject Item: dbr:Hurricane_Madeline_(1976)
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Subject Item: dbr:Hurricane_Manuel
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Subject Item: dbr:Hurricane_Maria_(2011)
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Subject Item: dbr:Hurricane_Marie_(2014)
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Subject Item: dbr:Hurricane_Michael
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Subject Item: dbr:Hurricane_Nana_(2020)
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Subject Item: dbr:Hurricane_Nate
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Subject Item: dbr:Hurricane_Nate_(2011)
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Subject Item: dbr:Hurricane_Nicole_(2016)
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Subject Item: dbr:Hurricane_Nora_(2021)
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Subject Item: dbr:Hurricane_Norbert_(2014)
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Subject Item: dbr:Hurricane_Odile
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Subject Item: dbr:Hurricane_Olivia_(2018)
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Subject Item: dbr:Hurricane_Ophelia_(2011)
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Subject Item: dbr:Hurricane_Ophelia_(2017)
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Subject Item: dbr:Hurricane_Otto_(2010)
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Subject Item: dbr:Hurricane_Pablo
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Subject Item: dbr:Hurricane_Paul_(1982)
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Subject Item: dbr:Hurricane_Paula
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Subject Item: dbr:Hurricane_Pauline_(1968)
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Subject Item: dbr:Hurricane_Rafael
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Subject Item: dbr:Hurricane_Raymond_(1989)
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Subject Item: dbr:Hurricane_Richard
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Subject Item: dbr:Hurricane_Rita
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Subject Item: dbr:Hurricane_Rosa_(2018)
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Subject Item: dbr:Hurricane_Roslyn_(1986)
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Subject Item: dbr:Hurricane_Shary
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Subject Item: dbr:Hurricane_Uleki
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Subject Item: dbr:Hurricane_Walaka
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Subject Item: dbr:Hurricane_Willa
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Subject Item: dbr:Hurricane_Zeta
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Subject Item: dbr:2017_Visayas_and_Mindanao_floods
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Subject Item: dbr:2019_South_Sulawesi_floods
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Subject Item: dbr:Ash_Wednesday_Storm_of_1962
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Subject Item: dbr:Atmosphere_of_Earth
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Subject Item: dbr:Chard,_Somerset
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Subject Item: dbr:Cheddar,_Somerset
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Subject Item: dbr:Chew_Valley
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Subject Item: dbr:Chewton_Mendip
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Subject Item: dbr:Chicago
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Subject Item: dbr:Kelvin
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Subject Item: dbr:La_Baie
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Subject Item: dbr:Lake-effect_snow
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Subject Item: dbr:Langport
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Subject Item: dbr:Blizzard
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Subject Item: dbr:Suwałki
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Subject Item: dbr:Sydney
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Subject Item: dbr:Effects_of_Hurricane_Isaac_in_Florida
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Subject Item: dbr:Effects_of_Hurricane_Isaac_in_Louisiana
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Subject Item: dbr:High-pressure_area
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Subject Item: dbr:Trough_(meteorology)
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Subject Item: dbr:Typhoon_Tingting
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Subject Item: dbr:Winter_storm
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Subject Item: dbr:Regional_Specialized_Meteorological_Centre
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Subject Item: dbr:September_1921_San_Antonio_floods
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Subject Item: dbr:Trade_winds
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Subject Item: dbr:Buys_Ballot's_law
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Subject Item: dbr:Port_Mansfield_Channel
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Subject Item: dbr:Somerset
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Subject Item: dbr:Somerset_Levels
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Subject Item: dbr:Soria
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Subject Item: dbr:South_Florida_tornadoes_of_March_17,_1983
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Subject Item: dbr:South_Pacific_tropical_cyclone
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Subject Item: dbr:South_Petherton
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Subject Item: dbr:Gregale
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Subject Item: dbr:Typhoon_Dinah_(1987)
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Subject Item: dbr:Typhoon_Kelly
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Subject Item: dbr:Typhoon_Koppu
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Subject Item: dbr:Typhoon_Ma-on_(2004)
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Subject Item: dbr:Typhoon_Nepartak
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Subject Item: dbr:Typhoon_Nesat_(2017)
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Subject Item: dbr:Typhoon_Rai
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Subject Item: dbr:Typhoon_Soudelor
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Subject Item: dbr:Typhoon_Surigae
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Subject Item: dbr:Typhoon_Trami
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Subject Item: dbr:Typhoon_Winnie
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Subject Item: dbr:Typhoon_Wutip_(2019)
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Subject Item: dbr:Ilminster
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Subject Item: dbr:Meteorological_history_of_Hurricane_Dennis
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Subject Item: dbr:October_2021_nor'easter
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Subject Item: dbr:Radiation_effects_from_the_Fukushima_Daiichi_nuclear_disaster
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Subject Item: dbr:September_1948_Florida_hurricane
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Subject Item: dbr:Christmas_1994_nor'easter
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Subject Item: dbr:List_of_Category_4_Pacific_hurricanes
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Subject Item: dbr:Mesoscale_convective_system
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Subject Item: dbr:Mesovortex
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Subject Item: dbr:Santa_Ana_winds
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Subject Item: dbr:South_Atlantic_tropical_cyclone
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Subject Item: dbr:Sawad
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Subject Item: dbr:Tropical_Storm_Beryl_(2012)
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Subject Item: dbr:Tornado_outbreak_of_April_27–28,_2002
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Subject Item: dbr:Tornado_outbreak_of_January_2008
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Subject Item: dbr:Extratropical_cyclone
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Subject Item: dbr:List_of_tornadoes_in_the_1999_Oklahoma_tornado_outbreak
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Subject Item: dbr:Little_Ice_Age_volcanism
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Subject Item: dbr:Low
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Subject Item: dbr:Low-pressure_area
rdf:type: yago:WikicatBasicMeteorologicalConceptsAndPhenomena yago:Content105809192 yago:Idea105833840 dbo:Settlement owl:Thing yago:Abstraction100002137 yago:Concept105835747 yago:RoundShape113865483 yago:Cognition100023271 yago:Attribute100024264 yago:Shape100027807 yago:PsychologicalFeature100023100 yago:Whirl113878112 yago:WikicatVortices
rdfs:label: Депресія (фізика) Депрессия (метеорология) 低気圧 Dépression (météorologie) Depressió atmosfèrica Low-pressure area Área de baixa pressão Malalta aeropremo Lagedrukgebied Borrasca 低气压 Wilayah bertekanan rendah Lågtryck Niż baryczny 저기압 Tiefdruckgebiet Lagrach منخفض جوي Depresio (meteorologia)
rdfs:comment: Una depressió atmosfèrica és una zona amb la pressió atmosfèrica més baixa que les zones del voltant. A l'hemisferi nord les depressions giren en sentit contrari al de les agulles d'un rellotge, en canvi a l'hemisferi sud giren en sentit contrari en ambdós casos això ho motiva l'efecte de Coriolis. Les depressions s'originen a la Zona de convergència intertropical formant part de la circulació de la cèl·lula de Hadley. Een lagedrukgebied, depressie of minimum is een gebied waarin de luchtdruk op zeeniveau laag is ten opzichte van de omgeving. Dit in tegenstelling tot een hogedrukgebied, waarin juist relatief hoge barometerstanden worden gemeten. Het symbool voor een lagedrukgebied is de letter L. Hiermee wordt op weerkaarten aangegeven waar een lagedrukgebied zich bevindt. Het geeft altijd de kern van een lagedrukgebied aan, waar de luchtdruk het laagst is. Ook de fronten van een lagedrukgebied worden op de weerkaart getoond, omdat dit slecht weer met zich meebrengt. Ein Tiefdruckgebiet (kurz das Tief, auch die Störung) ist ein Teil der Erdatmosphäre mit niedrigerem Luftdruck gegenüber dessen großräumiger Umgebung. Ihm steht begrifflich und räumlich das Hochdruckgebiet gegenüber. Von einem Tiefdruckgebiet spricht man nur dann, wenn ein Zentrum ausgemacht werden kann, von dem aus gesehen der Druck horizontal in jede Richtung zunimmt. In anderen Fällen handelt es sich um einen Trog. Man unterscheidet thermische Tiefdruckgebiete und dynamische Tiefdruckgebiete (Zyklone). Niż baryczny, cyklon – układ baryczny, w którym występują zazwyczaj układy frontalne. Nacisk jest tutaj położony na to, że niż baryczny jest zjawiskiem pogodowym, a nie obszarem niskiego ciśnienia. Wraz z przyjściem centrum niżu obserwuje się spadek ciśnienia i zazwyczaj zmianę innych parametrów, takich jak temperatura czy zachmurzenie. Wbrew potocznym oczekiwaniom wiatr, w rozwiniętym (czasowo) niżu barycznym, nie wieje od obszaru ciśnienia wysokiego do niskiego, lecz prawie równolegle do linii stałego ciśnienia. W niżu wiatry wieją cyklonalnie, czyli na półkuli północnej przeciwnie do wskazówek zegara. المنخفض الجوي هو منطقة مغلقة بخطوط ضغط متساوية حيث تكون أقل قيمة للضغط الجوي في المركز وتزداد كلما ابتعدنا عن المركز، اتجاه الرياح حول المنخفض الجوي عكس عقارب الساعة في نصف الكرة الشمالي والعكس في نصف الكرة الجنوبي. عادة يكون الطقس المصاحب للمنخفض الجوي ظهور الغيوم وحدوث الهطول بأشكاله المختلفة (يعتمد على الفترة الزمنية وعلى مصدر الكتلة الهوائية المصاحبة له ومسارها), اتجاه الرياح حول المنخفض الجوي في نصف الكرة الشمالي عكس عقارب الساعة والحرارة تعتمد على الكتلة الهوائية المصاحبة له فالرياح الجنوبية والجنوبية الغربية تؤدي إلى ارتفاع على درجات الحرارة. الرياح الغربية والشمالية الغربية وكذلك الشمالية تؤدي إلى حدوث انخفاض على درجات الحرارة. In meteorology, a low-pressure area, low area or low is a region where the atmospheric pressure is lower than that of surrounding locations. Low-pressure areas are commonly associated with inclement weather (such as cloudy, windy, with possible rain or storms), while high-pressure areas are associated with lighter winds and clear skies. Winds circle anti-clockwise around lows in the northern hemisphere, and clockwise in the southern hemisphere, due to opposing Coriolis forces. Low-pressure systems form under areas of wind divergence that occur in the upper levels of the atmosphere (aloft). The formation process of a low-pressure area is known as cyclogenesis. In meteorology, atmospheric divergence aloft occurs in two kinds of places: Sa mheitéareolaíocht, córas brú ísil ag domhanleithid arda is mheánacha. Tugtar cioclón air ag domhanleithid ísle. De ghnáth, téann an córas trí staideanna réasúnta dea-shainithe lena bpatrúin aimsire féin. Tosaíonn lagrach nuair a fhásann tonn ar fhronta idir mais aeir fhuair is mais aeir the. Titeann an brú ag círín na toinne. Bíonn fronta te i dtosach an lagraigh, agus ina dhiaidh sin an fronta fuar, le teascán te eatarthu. Ach taistealaíonn an fronta fuar ar luas níos mó ná luas an fhronta the, agus mar sin tagann suas leis an bhfronta te chun fronta oclúidithe a chruthú. Nuair a tharlaíonn sé seo, méadaíonn an brú agus cailleann an lagrach luas. Gluaiseann gaotha dromchlacha ar tuathal timpeall an lagraigh sa leathsféar thuaidh (ar deiseal sa leathsféar theas). Bíonn lagraigh 1,000-2, 低壓區（英語：Low Pressure Area，符號為L）是大氣中氣壓較鄰近地區為低的地帶。一般都是成螺旋狀，是為氣旋。在北半球低氣壓區域內的空氣作逆時針方向旋轉，在南半球則順時針方向。偶爾也有一連串低壓區連在一起，稱為「低壓槽」，因該區的大氣壓力比其兩旁為低，所以稱為槽，是為槽線取其陷下的意思。低壓區一般都伴着雲，或會有風、雨（通常雨勢較大並夾雜着狂風雷暴） Lågtryck, motsatsen till högtryck (anticyklon), är ett område där lufttrycket är lägre än omgivningen. På mellanbredderna och högre latituder blåser vinden i en virvel (cyklon) kring och in mot lågtryckets centrum. Corioliseffekten gör att vindarna blåser moturs på det norra halvklotet och medurs på det södra. Ju högre lufttrycksgradienten är, desto kraftigare blir vindarna. Det finns flera olika sorters lågtryck. På sommaren bildas värmelågtryck över kontinenter. Dessa ger ofta stora nederbördsmängder i form av regn- och åskskurar. Dessa är så kallade halvstationära lågtryck. Депре́сія — метеорологічна область порівняно слабкого атмосферного тиску або низького стояння барометра . Депресії бувають періодичні — Азійська (центр над Афганістаном), Австралійська річна депресія — Австралія, Нова Гвінея, Індонезія, Алеутська — Алеутські острови, постійні — екваторіальні, субполярні. Циклон також являє собою метеорологічну депресію, тільки рухливу. Em meteorologia, uma área de baixa pressão, área baixa ou baixa é uma região onde a pressão atmosférica é menor do que a das localidades vizinhas. Os sistemas de baixa pressão se formam sob áreas de divergência do vento que ocorrem nos níveis superiores da atmosfera. O processo de formação de uma área de baixa pressão é conhecido como ciclogênese. No campo da meteorologia, a divergência atmosférica no alto ocorre em duas áreas. A primeira área está no lado leste dos vales superiores, que formam a metade de uma onda de Rossby dentro dos ventos do oeste (uma crista com grande comprimento de onda que se estende pela troposfera). Uma segunda área de divergência do vento no alto ocorre à frente dos cristas de ondas curtas embutidas, que são de comprimento de onda menor. Ventos divergentes no al Депре́ссия в метеорологии — область сравнительно низкого атмосферного давления (низкого стояния барометра). Депрессии бывают периодически возникающие — Азиатская (центр над Афганистаном), Австралийская летняя депрессия — Австралия, Новая Гвинея, Индонезия, Алеутская — Алеутские острова; постоянные — экваториальные, субполярные.Циклон также представляет собой метеорологическую депрессию, только подвижную. Una borrasca o zona de baja presión es una masa de aire donde la presión atmosférica es más baja que la del aire circundante. Las tormentas tropicales, ciclones extratropicales, y los ciclones polares y árticos, reciben el nombre de células de baja presión, especialmente en comunidades angloparlantes. Los sistemas de baja presión en superficie tenderán a ser pequeños en área y tener vientos en superficie más fuertes que un sistema anticiclónico, debido a la fricción en superficie, al gradiente barométrico, fuerza centrífuga y efecto Coriolis que controlan la circulación. 저기압(低氣壓)은 주위에 비해 기압이 낮은 곳을 말하며, 일기도에서 보면 중심의 주위에 막힌 등압선이 그려져 있다. 기호는 'L'이다. Meteorologian, depresioa, beheragunea edo behe presioko gunea, ingurunearen aldean, presio atmosferiko apala duen eremua da. Behe presioko guneek ekaitzak sor ditzakete eta, orobat, urakanak eta zikloiak lurralde tropikaletan. Une dépression est une zone fermée de basse pression atmosphérique relative à celle du voisinage au même niveau. Sur une carte synoptique de surface, cela donne un système d'isobares dont la pression est minimale au centre. Les dépressions peuvent se retrouver en altitude ou en surface, dans le premier cas elles sont notées par un minimum de géopotentiel, alors que dans le second la pression est ajustée au niveau de la mer et donne généralement une valeur de moins de 1013,25 hPa. Wilayah bertekanan rendah atau depresi, atau siklon, wilayah tekanan rendah, pusat tekanan rendah, atau sistem tekanan rendah adalah sebagaian wilayah atmosfer Bumi yang memiliki tekanan udara lebih rendah dibandingkan wilayah di sekitarnya pada ketinggian yang sama. Wilayah tekanan rendah dapat digambarkan pada peta sebagai sebuah wilayah tertutup dengan nilai yang semakin menurun mendekati ke pusatnya. Wilayah tekanan rendah merupakan lawan dari wilayah tekanan tinggi. Angin akan bergerak dari wilayah tekanan tinggi menuju wilayah tekanan rendah dan akan berbelok mengikuti rotasi Bumi. Pergerakan angin ke arah pusat dari wilayah tekanan rendah dapat memperbanyak uap air yang terkumpul dan terbentuk di wilayah tersebut sehingga menaikkan tingkat kelembapan dan presipitasinya. 低気圧（ていきあつ、英語: low pressure）とは、周囲より気圧の低い部分をいう。周囲より気圧が低いと定義されるので、中心気圧が1気圧（1013hPa）より高い低気圧も珍しくない。冬季にシベリア高気圧の圏内に発生する低気圧の中には1030hPa以上のものもしばしば見られる。一般に、低気圧は雲を伴い、雨や雪や風をもたらす。 Malalta aeropremo aŭ depresio estas meteologia fenomeno. Ĝi estas regiono kun aeropremo pli malalta ol en la ĉirkaŭaĵo. La malalta aeropremo emas kunporti aŭ pluvon, aŭ nubon, aŭ tondron, aŭ venton.
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dbo:abstract: Wilayah bertekanan rendah atau depresi, atau siklon, wilayah tekanan rendah, pusat tekanan rendah, atau sistem tekanan rendah adalah sebagaian wilayah atmosfer Bumi yang memiliki tekanan udara lebih rendah dibandingkan wilayah di sekitarnya pada ketinggian yang sama. Wilayah tekanan rendah dapat digambarkan pada peta sebagai sebuah wilayah tertutup dengan nilai yang semakin menurun mendekati ke pusatnya. Wilayah tekanan rendah merupakan lawan dari wilayah tekanan tinggi. Angin akan bergerak dari wilayah tekanan tinggi menuju wilayah tekanan rendah dan akan berbelok mengikuti rotasi Bumi. Pergerakan angin ke arah pusat dari wilayah tekanan rendah dapat memperbanyak uap air yang terkumpul dan terbentuk di wilayah tersebut sehingga menaikkan tingkat kelembapan dan presipitasinya. Une dépression est une zone fermée de basse pression atmosphérique relative à celle du voisinage au même niveau. Sur une carte synoptique de surface, cela donne un système d'isobares dont la pression est minimale au centre. Les dépressions peuvent se retrouver en altitude ou en surface, dans le premier cas elles sont notées par un minimum de géopotentiel, alors que dans le second la pression est ajustée au niveau de la mer et donne généralement une valeur de moins de 1013,25 hPa. Les dépressions sont souvent associées au mauvais temps, car la dynamique qui entoure une dépression présuppose l'existence de courants ascendants qui provoquent des nuages et des précipitations. De plus, le gradient horizontal de pression autour d'une dépression peut engendrer de forts vents. Comme pour les anticyclones, il existe des dépressions à caractère semi-permanent qui sont des centres d'action étant donné qu'elles ont un impact sur le mouvement des perturbations et sur la circulation atmosphérique régionale des vents. Les dépressions se prolongent souvent en étirant un creux barométrique, ou talweg, à caractère temporaire mais ayant les mêmes effets que les dépressions à la seule différence que leur circulation n'est pas fermée. Lågtryck, motsatsen till högtryck (anticyklon), är ett område där lufttrycket är lägre än omgivningen. På mellanbredderna och högre latituder blåser vinden i en virvel (cyklon) kring och in mot lågtryckets centrum. Corioliseffekten gör att vindarna blåser moturs på det norra halvklotet och medurs på det södra. Ju högre lufttrycksgradienten är, desto kraftigare blir vindarna. Längs den intertropiska konvergenszonen (ITCZ), där corioliseffekten är svag, bildas istället långsträckta lågtrycksområden, vilka, i samverkan med det subtropiska högtrycksbältet , ger upphov till monsuner och passadvindar. När ITCZ närmar sig vändkretsarna (där corioliseffekten är starkare) under sommar och höst (då havsvattnet är varmt) kan små, men mycket kraftiga, tropiska cykloner "knoppas av" från våglika störningar i detta lågtrycksbälte. Dessa tropiska cykloner kan sedan förflytta sig mot högre latituder, böja av mot nordost på norra halvklotet (sydost på det södra) och därvid omvandlas till "vanliga mellanbreddscykloner", vilka ibland kan orsaka kraftiga oväder. Det finns flera olika sorters lågtryck. På sommaren bildas värmelågtryck över kontinenter. Dessa ger ofta stora nederbördsmängder i form av regn- och åskskurar. Dessa är så kallade halvstationära lågtryck. Rörliga lågtryck hör samman med västvindsbältets vädersystem på bägge hemisfärernas mellanbreddgrader. Dessa så kallade mellanbreddslågtryck uppstår vid gränsen mellan varmare och kallare luftmassor.På skiljeytan mellan de oliktempererade luftmassorna bildas fronter och längs fronterna kan moln och nederbörd uppstå. Dessa lågtryck förekommer i olika omfattning i världen beroende på fördelningen av kontinenter och hav. De rörliga lågtrycken är en bidragande orsak till väderleksförändringarna i Sverige. I Europa styrs vädret ofta av rörliga lågtryck från Atlanten som rör sig i en väst-ostlig riktning. Dessa lågtryck föregås vanligen av en varmfront, vilket ger varma vindar innan lågtrycket passerat, och följs av en kallfront som ger kalla vindar då det passerat. Cykloner/lågtryck har olika namn utifrån dess diametermått. Mesocyklon är benämningen på små cykloner/lågtryck (10-300 km i diameter). De ytterst små kallas misocykloner (tromber). På väderkartan betecknas lågtryck med det nationella ordets begynnelsebokstav i versal. I Sverige och engelskspråkiga länder således med ett L och i Finland med ett M (matalan keskus). Sa mheitéareolaíocht, córas brú ísil ag domhanleithid arda is mheánacha. Tugtar cioclón air ag domhanleithid ísle. De ghnáth, téann an córas trí staideanna réasúnta dea-shainithe lena bpatrúin aimsire féin. Tosaíonn lagrach nuair a fhásann tonn ar fhronta idir mais aeir fhuair is mais aeir the. Titeann an brú ag círín na toinne. Bíonn fronta te i dtosach an lagraigh, agus ina dhiaidh sin an fronta fuar, le teascán te eatarthu. Ach taistealaíonn an fronta fuar ar luas níos mó ná luas an fhronta the, agus mar sin tagann suas leis an bhfronta te chun fronta oclúidithe a chruthú. Nuair a tharlaíonn sé seo, méadaíonn an brú agus cailleann an lagrach luas. Gluaiseann gaotha dromchlacha ar tuathal timpeall an lagraigh sa leathsféar thuaidh (ar deiseal sa leathsféar theas). Bíonn lagraigh 1,000-2,000 km ar leithead de ghnáth, ach ní mhaireann ach 4-7 lá. Cruthaítear go rialta iad i réigiúin áirithe (mar shampla, ar feadh frontaí Molacha an Aigéin Atlantaigh is an Aigéin Chiúin, agus sa Mheánmhuir). Cruthaítear na lagraigh is déine sa gheimhreadh. 저기압(低氣壓)은 주위에 비해 기압이 낮은 곳을 말하며, 일기도에서 보면 중심의 주위에 막힌 등압선이 그려져 있다. 기호는 'L'이다. المنخفض الجوي هو منطقة مغلقة بخطوط ضغط متساوية حيث تكون أقل قيمة للضغط الجوي في المركز وتزداد كلما ابتعدنا عن المركز، اتجاه الرياح حول المنخفض الجوي عكس عقارب الساعة في نصف الكرة الشمالي والعكس في نصف الكرة الجنوبي. عادة يكون الطقس المصاحب للمنخفض الجوي ظهور الغيوم وحدوث الهطول بأشكاله المختلفة (يعتمد على الفترة الزمنية وعلى مصدر الكتلة الهوائية المصاحبة له ومسارها), اتجاه الرياح حول المنخفض الجوي في نصف الكرة الشمالي عكس عقارب الساعة والحرارة تعتمد على الكتلة الهوائية المصاحبة له فالرياح الجنوبية والجنوبية الغربية تؤدي إلى ارتفاع على درجات الحرارة. الرياح الغربية والشمالية الغربية وكذلك الشمالية تؤدي إلى حدوث انخفاض على درجات الحرارة. Niż baryczny, cyklon – układ baryczny, w którym występują zazwyczaj układy frontalne. Nacisk jest tutaj położony na to, że niż baryczny jest zjawiskiem pogodowym, a nie obszarem niskiego ciśnienia. Wraz z przyjściem centrum niżu obserwuje się spadek ciśnienia i zazwyczaj zmianę innych parametrów, takich jak temperatura czy zachmurzenie. Wbrew potocznym oczekiwaniom wiatr, w rozwiniętym (czasowo) niżu barycznym, nie wieje od obszaru ciśnienia wysokiego do niskiego, lecz prawie równolegle do linii stałego ciśnienia. W niżu wiatry wieją cyklonalnie, czyli na półkuli północnej przeciwnie do wskazówek zegara. Niż (ciśnienie) i cyklon (kierunek wiatru) są synonimami. Em meteorologia, uma área de baixa pressão, área baixa ou baixa é uma região onde a pressão atmosférica é menor do que a das localidades vizinhas. Os sistemas de baixa pressão se formam sob áreas de divergência do vento que ocorrem nos níveis superiores da atmosfera. O processo de formação de uma área de baixa pressão é conhecido como ciclogênese. No campo da meteorologia, a divergência atmosférica no alto ocorre em duas áreas. A primeira área está no lado leste dos vales superiores, que formam a metade de uma onda de Rossby dentro dos ventos do oeste (uma crista com grande comprimento de onda que se estende pela troposfera). Uma segunda área de divergência do vento no alto ocorre à frente dos cristas de ondas curtas embutidas, que são de comprimento de onda menor. Ventos divergentes no alto à frente dessas depressões causam elevação atmosférica na troposfera abaixo, o que reduz as pressões na superfície, pois o movimento ascendente neutraliza parcialmente a força da gravidade. Uma área de baixa pressão é comumente associada a clima inclemente, enquanto uma área de alta pressão está associada a ventos fracos e céu limpo. As baixas térmicas formam-se devido ao aquecimento localizado causado pela maior insolação sobre desertos e outras massas de terra. Como as áreas localizadas de ar quente são menos densas do que seus arredores, esse ar mais quente sobe, o que diminui a pressão atmosférica perto daquela parte da superfície da Terra. Baixas térmicas em grande escala nos continentes ajudam a impulsionar as circulações das monções. As áreas de baixa pressão também podem se formar devido à atividade organizada da tempestade sobre a água quente. Quando isso ocorre nos trópicos em conjunto com a Zona de convergência intertropical, é conhecido como Cavado de monção. Os cavados das monções atingem a sua extensão ao norte em agosto e a sua extensão ao sul em fevereiro. Quando uma baixa convectiva adquire uma circulação bem quente nos trópicos, é denominado ciclone tropical. Os ciclones tropicais podem se formar durante qualquer mês do ano globalmente, mas podem ocorrer no hemisfério norte ou sul durante dezembro. A elevação atmosférica também geralmente produz cobertura de nuvens por meio do resfriamento adiabático, uma vez que o ar se torna saturado à medida que sobe, embora a área de baixa pressão normalmente traga céus nublados, que agem para minimizar os extremos diurnos de temperatura. Como as nuvens refletem a luz do sol, a irradiação solar de ondas curtas que chega diminui, o que causa temperaturas mais baixas durante o dia. À noite, o efeito de absorção das nuvens na radiação de onda longa que sai, como a energia térmica da superfície, permite baixas temperaturas diurnas mais quentes em todas as estações. Quanto mais forte for a área de baixa pressão, mais fortes serão os ventos experimentados nas proximidades. Globalmente, os sistemas de baixa pressão estão mais frequentemente localizados no planalto tibetano e a sotavento das montanhas rochosas. Na Europa (particularmente nas Ilhas Britânicas e na Holanda), os sistemas climáticos recorrentes de baixa pressão são normalmente conhecidos como "níveis baixos". Een lagedrukgebied, depressie of minimum is een gebied waarin de luchtdruk op zeeniveau laag is ten opzichte van de omgeving. Dit in tegenstelling tot een hogedrukgebied, waarin juist relatief hoge barometerstanden worden gemeten. Door de lage druk stroomt de lucht naar het centrum, door wrijving en het corioliseffect spiraalsgewijs. De isobaren naderen elkaar hier. Deze cyclonale circulatie is op het noordelijk halfrond tegen de klok in en op het zuidelijk halfrond met de klok mee. Door dit samenstromen van de lucht of convergentie moet de lucht naar boven uitwijken. Doordat de stijgende lucht afkoelt, zal er bij voldoende vochtigheid wolkenvorming optreden met mogelijke neerslag. Het symbool voor een lagedrukgebied is de letter L. Hiermee wordt op weerkaarten aangegeven waar een lagedrukgebied zich bevindt. Het geeft altijd de kern van een lagedrukgebied aan, waar de luchtdruk het laagst is. Ook de fronten van een lagedrukgebied worden op de weerkaart getoond, omdat dit slecht weer met zich meebrengt. Malalta aeropremo aŭ depresio estas meteologia fenomeno. Ĝi estas regiono kun aeropremo pli malalta ol en la ĉirkaŭaĵo. La malalta aeropremo emas kunporti aŭ pluvon, aŭ nubon, aŭ tondron, aŭ venton. Una depressió atmosfèrica és una zona amb la pressió atmosfèrica més baixa que les zones del voltant. A l'hemisferi nord les depressions giren en sentit contrari al de les agulles d'un rellotge, en canvi a l'hemisferi sud giren en sentit contrari en ambdós casos això ho motiva l'efecte de Coriolis. Les depressions s'originen a la Zona de convergència intertropical formant part de la circulació de la cèl·lula de Hadley. Les depressions, s'associen normalment amb vents forts i elevació atmosfèrica. Aquesta elevació sol produir cel cobert, a causa del gradient tèrmic quan l'aire es col·lapsa. Així, les depressions solen portar cels ennuvolats o coberts, que poden minimitzar la temperatura diürna tant a l'estiu com a l'hivern. Això es produeix per l'entrada de menys radiació solar d'ona curta i temperatures més baixes, ja que els núvols reflecteixen la llum solar. De nit, l'efecte d'absorció dels núvols en la radiació d'ona llarga, com la calor de la superfície, permet que les temperatures diürnes siguin més fresques en totes les estacions de l'any. Les són un fenomen de la zona temperada, i es desenvolupen al llarg de fronts polars com a resultat de la interacció entre el masses d'aire fred i calent. Les depressions tèrmiques també es formen en zones com Death Valley com a resultat de la intensa calor despresa des de la superfície; són molt més petites en extensió geogràfica que els fronts de convergència o les depressions frontals. Els sistemes de baixes pressions en superfície tendiran a ser petits en àrea i tenir vents en superfície més forts que un sistema anticiclònic, a causa de la suma de fricció en superfície per força del gradient de pressió, força centrífuga i l'efecte Coriolis que controlen la circulació. Als deserts, l'absència d'humitat i plantes en superfície que normalment proporcionarien refrigeració per evaporació pot dur a un augment ràpid i intens de la calor solar en les capes baixes de l'aire. L'aire calent és menys dens que l'aire fred d'al voltant. Això, combinat amb l'elevació d'aire calent, resulta en una depressió aïllada, anomenada . Депре́ссия в метеорологии — область сравнительно низкого атмосферного давления (низкого стояния барометра). Депрессии бывают периодически возникающие — Азиатская (центр над Афганистаном), Австралийская летняя депрессия — Австралия, Новая Гвинея, Индонезия, Алеутская — Алеутские острова; постоянные — экваториальные, субполярные.Циклон также представляет собой метеорологическую депрессию, только подвижную. 低壓區（英語：Low Pressure Area，符號為L）是大氣中氣壓較鄰近地區為低的地帶。一般都是成螺旋狀，是為氣旋。在北半球低氣壓區域內的空氣作逆時針方向旋轉，在南半球則順時針方向。偶爾也有一連串低壓區連在一起，稱為「低壓槽」，因該區的大氣壓力比其兩旁為低，所以稱為槽，是為槽線取其陷下的意思。低壓區一般都伴着雲，或會有風、雨（通常雨勢較大並夾雜着狂風雷暴） Ein Tiefdruckgebiet (kurz das Tief, auch die Störung) ist ein Teil der Erdatmosphäre mit niedrigerem Luftdruck gegenüber dessen großräumiger Umgebung. Ihm steht begrifflich und räumlich das Hochdruckgebiet gegenüber. Von einem Tiefdruckgebiet spricht man nur dann, wenn ein Zentrum ausgemacht werden kann, von dem aus gesehen der Druck horizontal in jede Richtung zunimmt. In anderen Fällen handelt es sich um einen Trog. Man unterscheidet thermische Tiefdruckgebiete und dynamische Tiefdruckgebiete (Zyklone). 低気圧（ていきあつ、英語: low pressure）とは、周囲より気圧の低い部分をいう。周囲より気圧が低いと定義されるので、中心気圧が1気圧（1013hPa）より高い低気圧も珍しくない。冬季にシベリア高気圧の圏内に発生する低気圧の中には1030hPa以上のものもしばしば見られる。一般に、低気圧は雲を伴い、雨や雪や風をもたらす。 In meteorology, a low-pressure area, low area or low is a region where the atmospheric pressure is lower than that of surrounding locations. Low-pressure areas are commonly associated with inclement weather (such as cloudy, windy, with possible rain or storms), while high-pressure areas are associated with lighter winds and clear skies. Winds circle anti-clockwise around lows in the northern hemisphere, and clockwise in the southern hemisphere, due to opposing Coriolis forces. Low-pressure systems form under areas of wind divergence that occur in the upper levels of the atmosphere (aloft). The formation process of a low-pressure area is known as cyclogenesis. In meteorology, atmospheric divergence aloft occurs in two kinds of places: * The first is in the area on the east side of upper troughs, which form half of a Rossby wave within the Westerlies (a trough with large wavelength that extends through the troposphere). * A second is an area where wind divergence aloft occurs ahead of embedded shortwave troughs, which are of smaller wavelength. Diverging winds aloft, ahead of these troughs, cause atmospheric lift within the troposphere below as air flows upwards away from the surface, which lowers surface pressures as this upward motion partially counteracts the force of gravity packing the air close to the ground. Thermal lows form due to localized heating caused by greater solar incidence over deserts and other land masses. Since localized areas of warm air are less dense than their surroundings, this warmer air rises, which lowers atmospheric pressure near that portion of the Earth's surface. Large-scale thermal lows over continents help drive monsoon circulations. Low-pressure areas can also form due to organized thunderstorm activity over warm water. When this occurs over the tropics in concert with the Intertropical Convergence Zone, it is known as a monsoon trough. Monsoon troughs reach their northerly extent in August and their southerly extent in February. When a convective low acquires a well-hot circulation in the tropics it is termed a tropical cyclone. Tropical cyclones can form during any month of the year globally but can occur in either the northern or southern hemisphere during December. Atmospheric lift will also generally produce cloud cover through adiabatic cooling once the air temperature drops below the dew point as it rises, although the low-pressure area typically brings cloudy skies, which act to dampen diurnal temperature extremes. Since clouds reflect sunlight, incoming shortwave solar radiation decreases, which causes lower temperatures during the day. At night the absorptive effect of clouds on outgoing longwave radiation, such as heat energy from the surface, allows for warmer night-time minimums in all seasons. The stronger the area of low pressure, the stronger the winds experienced in its vicinity. Globally, low-pressure systems are most frequently located over the Tibetan Plateau and in the lee of the Rocky mountains. In Europe (particularly in the British Isles and Netherlands), recurring low-pressure weather systems are typically known as "low levels". Meteorologian, depresioa, beheragunea edo behe presioko gunea, ingurunearen aldean, presio atmosferiko apala duen eremua da. Behe presioko guneek ekaitzak sor ditzakete eta, orobat, urakanak eta zikloiak lurralde tropikaletan. Una borrasca o zona de baja presión es una masa de aire donde la presión atmosférica es más baja que la del aire circundante. Las tormentas tropicales, ciclones extratropicales, y los ciclones polares y árticos, reciben el nombre de células de baja presión, especialmente en comunidades angloparlantes. Las borrascas se asocian normalmente con vientos fuertes y elevación atmosférica. Esta elevación suele producir cielo cubierto, debido al gradiente térmico cuando el aire se satura. Así, las borrascas suelen traer cielos nubosos o cubiertos, que pueden minimizar la temperatura diurna tanto en verano como en invierno. Esto se produce por la entrada de menos radiación solar de radiación de onda corta y temperaturas más bajas, ya que las nubes reflejan la luz solar. De noche, el efecto de absorción de las nubes en la onda larga, como el calor de la superficie, permite que las temperaturas diurnas sean más frescas en todas las estaciones del año. Climatológicamente, las borrascas se forman en la zona de convergencia intertropical, como parte de la circulación de la célula de Hadley. Muchos de los bosques de pluviselva o bosque tropical lluvioso están asociados con estos sistemas climatológicos de baja presión. Las borrascas frontales son un fenómeno de la zona templada, y se desarrollan a lo largo de frentes polares como resultado de la interacción entre las masas de aire frío y caliente. Las borrascas térmicas también se forman en zonas como el valle de la Muerte como resultado del intenso calor despedido desde la superficie; son mucho más pequeñas en extensión geográfica que los frentes de convergencia o las borrascas frontales. Los sistemas de baja presión en superficie tenderán a ser pequeños en área y tener vientos en superficie más fuertes que un sistema anticiclónico, debido a la fricción en superficie, al gradiente barométrico, fuerza centrífuga y efecto Coriolis que controlan la circulación. En los desiertos, la ausencia de humedad y plantas en superficie que normalmente proporcionarían refrigeración (por evaporación) puede llevar a un aumento rápido e intenso del calor solar en las capas bajas del aire. El aire caliente es menos denso que el aire frío de alrededor. Esto, combinado con la elevación de aire caliente, resulta en una borrasca aislada, llamada baja termal. Депре́сія — метеорологічна область порівняно слабкого атмосферного тиску або низького стояння барометра . Депресії бувають періодичні — Азійська (центр над Афганістаном), Австралійська річна депресія — Австралія, Нова Гвінея, Індонезія, Алеутська — Алеутські острови, постійні — екваторіальні, субполярні. Циклон також являє собою метеорологічну депресію, тільки рухливу.
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Subject Item: dbr:Tropical_Storm_Carlotta_(2018)
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Subject Item: dbr:Tropical_Storm_Cecil
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Subject Item: dbr:Tropical_Storm_Cindy_(1963)
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Subject Item: dbr:Tropical_Storm_Cindy_(2017)
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Subject Item: dbr:Tropical_Storm_Claudette_(2021)
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Subject Item: dbr:Tropical_Storm_Danny_(2021)
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Subject Item: dbr:Tropical_Storm_Hernan_(2020)
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Subject Item: dbr:Tropical_Storm_Ileana_(2018)
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Subject Item: dbr:Tropical_Storm_Ivo_(2019)
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Subject Item: dbr:Tropical_Storm_Koguma
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Subject Item: dbr:Tropical_Storm_Meari_(2011)
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Subject Item: dbr:Tropical_Storm_Philippe_(2017)
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Subject Item: dbr:Tropical_Storm_Rolf
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Subject Item: dbr:Tropical_Storm_Talas_(2017)
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Subject Item: dbr:Tropical_cyclones_in_2005
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Subject Item: dbr:Tropical_depressions_Wilma_and_BOB_05
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Subject Item: dbr:Typhoon_Maysak_(2020)
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Subject Item: dbr:Topographic_steering
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Subject Item: dbr:Tropical_Low_Fletcher
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Subject Item: dbr:Tropical_Storm_Hermine_(2022)
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Subject Item: dbr:Tropical_Storm_Agatha_(1992)
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Subject Item: dbr:Tropical_Storm_Olaf_(1997)
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Subject Item: dbr:Area_of_low_pressure
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Subject Item: dbr:Atlantic_depression
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Subject Item: dbr:Atmospheric_lows
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Subject Item: dbr:Low-pressure_cell
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Subject Item: dbr:Low-pressure_system
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Subject Item: dbr:Low-pressure_trough
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Subject Item: dbr:Low_(atmospheric)
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Subject Item: dbr:Low_Pressure
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Subject Item: dbr:Low_Pressure_Systems
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Subject Item: dbr:Low_pressure
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Subject Item: dbr:Low_pressure_area
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Subject Item: dbr:Low_pressure_system
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Subject Item: dbr:Low_pressure_systems
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Subject Item: dbr:Remnant-low_pressure_area
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Subject Item: dbr:Remnant_Low_Pressure_Area
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Subject Item: dbr:Depression_(meteorology)
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Subject Item: dbr:Weather_system
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Subject Item: wikipedia-en:Low-pressure_area
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