{"id":5433,"date":"2023-09-13T08:37:10","date_gmt":"2023-09-13T06:37:10","guid":{"rendered":"https:\/\/us.edu.pl\/instytut\/inoz\/?page_id=5433"},"modified":"2026-02-19T10:25:03","modified_gmt":"2026-02-19T09:25:03","slug":"kalendarz-typow-cyrkulacji","status":"publish","type":"page","link":"https:\/\/us.edu.pl\/instytut\/inoz\/en\/kalendarz-typow-cyrkulacji\/","title":{"rendered":"Calendar of circulation types"},"content":{"rendered":"
[vc_row][vc_column][vc_column_text el_class=”container”]<\/p>\n
Kalendarz typ\u00f3w cyrkulacji dla obszaru Polski Po\u0142udniowej:<\/strong> Citing: Nied\u017awied\u017a T., 2017,\u00a0Kalendarz typ\u00f3w cyrkulacji atmosfery dla Polski po\u0142udniowej<\/em>\u00a0\u2014 zbi\u00f3r komputerowy, Uniwersytet \u015al\u0105ski, Katedra Klimatologii, Sosnowiec.<\/strong><\/p>\n Kalendarz typ\u00f3w cyrkulacji dla obszaru Spitsbergenu:<\/strong> Citing: Nied\u017awied\u017a T., 2013,\u00a0Kalendarz typ\u00f3w cyrkulacji atmosfery dla Spitsbergenu<\/em>\u00a0\u2014 zbi\u00f3r komputerowy, Uniwersytet \u015al\u0105ski, Katedra Klimatologii, Sosnowiec.<\/strong><\/p>\n On the basis of synoptic maps of Europe, 21 types of synoptic situations (circulation types) were distinguished, taking into account the direction of air masses advection and the kind of pressure pattern (a \u2014 anticyclonic, c \u2014 cyclonic).<\/p>\n Kodowanie typ\u00f3w cyrkulacji w zbiorze \u2014 21 typ\u00f3w Typy cyklonalne (11\u201420) \u2044 Cyclonic situations (11\u201420):<\/strong> 21 \u2013 x<\/strong>\u00a0\u2014 unclassified situations or pressure col.<\/p>\n Kod skr\u00f3cony (poprzez po\u0142\u0105czenie typ\u00f3w pokrewnych) 11 typ\u00f3w Typy cyklonalne (6\u201410) \u2044 Cyclonic situations (6\u201410):<\/strong> 11 \u2013 x<\/strong>\u00a0\u2014 typ nieokre\u015blony<\/p>\n \u0179R\u00d3D\u0141A DANYCH\/Sources of Data:<\/strong><\/p>\n [\/vc_column_text][\/vc_column][\/vc_row]<\/p>","protected":false},"excerpt":{"rendered":" [vc_row][vc_column][vc_column_text el_class=”container”] Kalendarz Typ\u00f3w Cyrkulacji \u2013 Calendar of circulation types Kalendarz typ\u00f3w cyrkulacji dla obszaru Polski Po\u0142udniowej: Area: 49\u201351 N 18\u201324 E Okres 01.09.1873 \u2014 10.01.2026 Tadeusz Nied\u017awied\u017a Data under the CC BY 4.0 license (https:\/\/creativecommons.org\/licenses\/by\/4.0\/) POBIERZ \/ DOWNLOAD\u00a0 \u00a0Kalendarz Typ\u00f3w Cyrkulacji dla Polski Po\u0142udniowej Citing: Nied\u017awied\u017a T., 2017,\u00a0Kalendarz typ\u00f3w cyrkulacji atmosfery dla Polski po\u0142udniowej\u00a0\u2014 […]<\/p>\n
\nArea: 49\u201351 N 18\u201324 E
\nOkres 01.09.1873 \u2014 10.01.2026
\nTadeusz Nied\u017awied\u017a<\/p>\n
<\/a>
\nData under the CC BY 4.0 license<\/strong> (https:\/\/creativecommons.org\/licenses\/by\/4.0\/<\/a>)
\nPOBIERZ \/ DOWNLOAD<\/a>\u00a0 \u00a0<\/strong><\/span>Kalendarz Typ\u00f3w Cyrkulacji dla Polski Po\u0142udniowej<\/p>\n
\nOkres 12.1897 \u2014 10.01.2025
\nTadeusz Nied\u017awied\u017a<\/p>\n
<\/a>
\nData under the CC BY 4.0 license<\/strong> (https:\/\/creativecommons.org\/licenses\/by\/4.0\/<\/a>)
\nPOBIERZ \/ DOWNLOAD<\/a>\u00a0 \u00a0<\/strong><\/span>Kalendarz Typ\u00f3w Cyrkulacji dla Spitsbergenu<\/p>\n
\nCode Type Description tc21<\/strong>
\nTypy antycyklonalne (1\u201410) \u2044 Anticyclonic situations (1\u201410):<\/strong>
\n1 \u2013 Na<\/strong>\u00a0\u2014 North (direction of air masses advection, geostrophic wind),
\n2 \u2013 NEa<\/strong>\u00a0\u2014 North\u2013East
\n3 \u2013 Ea<\/strong>\u00a0\u2014 East
\n4 \u2013 SEa<\/strong>\u00a0\u2014 South\u2013East
\n5 \u2013 Sa<\/strong>\u00a0\u2014 South
\n6 \u2013 SWa<\/strong>\u00a0\u2014 South\u2013West
\n7 \u2013 Wa<\/strong>\u00a0\u2014 West
\n8 \u2013 NW<\/strong>\u00a0\u2014 North\u2013West
\n9 \u2013 Ca<\/strong>\u00a0\u2014 central anticyclone situation (high center)
\n10 \u2013 Ka<\/strong>\u00a0\u2014 anticyclonic wedge or ridge of high pressure<\/p>\n
\n11 \u2013 Nc<\/strong>\u00a0\u2014 North
\n12 \u2013 NEc<\/strong>\u00a0\u2014 North\u2013East
\n13 \u2013 Ec<\/strong>\u00a0\u2014 East
\n14 \u2013 SEc<\/strong>\u00a0\u2014 South\u2013East
\n15 \u2013 Sc<\/strong>\u00a0\u2014 South
\n16 \u2013 SWc<\/strong>\u00a0\u2014 South\u2013West
\n17 \u2013 Wc<\/strong>\u00a0\u2014 West
\n18 \u2013 NWc<\/strong>\u00a0\u2014 North\u2013West
\n19 \u2013 Cc<\/strong>\u00a0\u2014 central cyclonic, center of low
\n20 \u2013 Bc<\/strong>\u00a0\u2014 through of low pressure (different directions of air flow and frontal system in the axis of through)<\/p>\n
\nCode Type Description tc11
\n<\/strong>Typy antycyklonalne (1\u20145) \u2044 Anticyclonic situations (1\u20145):<\/strong>
\n1 \u2013 N+NEa<\/strong>
\n2 \u2013 E+SEa<\/strong>
\n3 \u2013 S+SWa<\/strong>
\n4 \u2013 W+NWa<\/strong>
\n5 \u2013 Ca+Ka<\/strong><\/p>\n
\n6 \u2013 N+NEc<\/strong>
\n7 \u2013 E+SEc<\/strong>
\n8 \u2013 S+SWc<\/strong>
\n9 \u2013 W+NWc<\/strong>
\n10 \u2013 Cc+Bc<\/strong><\/p>\n\n\n
\n \n \n