Termiczne pory roku w Szymbarku (1968 – 2013)
The article contains an analysis of the duration and the dates of the start of thermal seasons of the year, distinguished on the basis of the average daily air temperature at the Institute of Geography and Spatial Organization Research Station at Szymbark over a period of 46 years ( 1968–2013 ). To...
Gespeichert in:
Veröffentlicht in: | Prace geograficzne (Kraków, Poland) Poland), 2016 (147), p.67-80 |
---|---|
1. Verfasser: | |
Format: | Artikel |
Sprache: | pol |
Schlagworte: | |
Online-Zugang: | Volltext |
Tags: |
Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
|
container_end_page | 80 |
---|---|
container_issue | 147 |
container_start_page | 67 |
container_title | Prace geograficzne (Kraków, Poland) |
container_volume | |
creator | Bochenek , Witold |
description | The article contains an analysis of the duration and the dates of the start of thermal seasons of the year, distinguished on the basis of the average daily air temperature at the Institute of Geography and Spatial Organization Research Station at Szymbark over a period of 46 years ( 1968–2013 ). To determine the initial dates of thermal seasons a method proposed by Makowiec (1983 ) was used. According to this method, the year was divided into eight thermal seasons, with temperature threshold values : 0, 5, 10 and 15 °C. The classification by Makowiec is based on the growth or fall of cumulative ranks of air temperature diminished by the temperature threshold value for a particular season. The determination of the initial dates enabled the calculation of the length of the seasons. The long-term analysis involved also the tendencies of length and changes of the initial date of a given season. The location of the meteorological station enables to expand the area of the interpretation of results into the borderland of the Beskid Niski Mts and the Carpathian Foothills. A high variability of the dates of the start and the duration of seasons was observed. The trends of duration and starting dates are multidirectional. The longest season is summer ( 89 days ), which starts increasingly earlier and lasts increasingly longer. An increase in duration also refers to pre-spring and autumn. Increasingly shorter winters and springs were also observed within the multi-year period. |
doi_str_mv | 10.4467/20833113PG.16.022.6084 |
format | Article |
fullrecord | <record><control><sourceid>ceeol_proqu</sourceid><recordid>TN_cdi_proquest_journals_2057259668</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><ceeol_id>510033</ceeol_id><sourcerecordid>510033</sourcerecordid><originalsourceid>FETCH-LOGICAL-c498-4f894becd131cbf057a516159b0c6529a9b5fc5675f2ce8b0d9a33b648aaaf483</originalsourceid><addsrcrecordid>eNpFjc9KAzEYxIMoWGrfQCTgRQ-7_b78-TY5SrFVKCi495KkCVjbbt11kfbkO_iGPom7VHAuMzA_Zhi7QsiVomIswEiJKJ9nOVIOQuQERp2wQV9kfXPKBkhKZVIbOmejpllBJzKaQAzYuIz15jUctpHvqnrP6-qt5Z_85bDfeFd3-QYtGf7z9c0FoLy9YGfJrZs4-vMhK6f35eQhmz_NHid38ywoazKVjFU-hiVKDD6BLpxGQm09BNLCOut1CpoKnUSIxsPSOik9KeOcS8rIIbs-zu7q6r2NzcdiVbX1tntciG5NaEvUU5dHKsRYrf8RjQBSyl_hNE5p</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>2057259668</pqid></control><display><type>article</type><title>Termiczne pory roku w Szymbarku (1968 – 2013)</title><source>Alma/SFX Local Collection</source><creator>Bochenek , Witold</creator><creatorcontrib>Bochenek , Witold</creatorcontrib><description>The article contains an analysis of the duration and the dates of the start of thermal seasons of the year, distinguished on the basis of the average daily air temperature at the Institute of Geography and Spatial Organization Research Station at Szymbark over a period of 46 years ( 1968–2013 ). To determine the initial dates of thermal seasons a method proposed by Makowiec (1983 ) was used. According to this method, the year was divided into eight thermal seasons, with temperature threshold values : 0, 5, 10 and 15 °C. The classification by Makowiec is based on the growth or fall of cumulative ranks of air temperature diminished by the temperature threshold value for a particular season. The determination of the initial dates enabled the calculation of the length of the seasons. The long-term analysis involved also the tendencies of length and changes of the initial date of a given season. The location of the meteorological station enables to expand the area of the interpretation of results into the borderland of the Beskid Niski Mts and the Carpathian Foothills. A high variability of the dates of the start and the duration of seasons was observed. The trends of duration and starting dates are multidirectional. The longest season is summer ( 89 days ), which starts increasingly earlier and lasts increasingly longer. An increase in duration also refers to pre-spring and autumn. Increasingly shorter winters and springs were also observed within the multi-year period.</description><identifier>ISSN: 1644-3586</identifier><identifier>EISSN: 2083-3113</identifier><identifier>DOI: 10.4467/20833113PG.16.022.6084</identifier><language>pol</language><publisher>Kraków: Wydawnictwo Uniwersytetu Jagiellońskiego</publisher><subject>Air temperature ; Classification ; Geography ; Geography, Regional studies ; Historical Geography ; History ; Physical Geopgraphy ; Recent History (1900 till today) ; Seasons ; Temperature ; Variability</subject><ispartof>Prace geograficzne (Kraków, Poland), 2016 (147), p.67-80</ispartof><rights>Copyright Jagiellonian University-Jagiellonian University Press 2016</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Uhttps://www.ceeol.com//api/image/getissuecoverimage?id=picture_2016_30710.jpg</thumbnail><link.rule.ids>314,776,780,4010,27900,27901,27902</link.rule.ids></links><search><creatorcontrib>Bochenek , Witold</creatorcontrib><title>Termiczne pory roku w Szymbarku (1968 – 2013)</title><title>Prace geograficzne (Kraków, Poland)</title><addtitle>Geographical Studies</addtitle><description>The article contains an analysis of the duration and the dates of the start of thermal seasons of the year, distinguished on the basis of the average daily air temperature at the Institute of Geography and Spatial Organization Research Station at Szymbark over a period of 46 years ( 1968–2013 ). To determine the initial dates of thermal seasons a method proposed by Makowiec (1983 ) was used. According to this method, the year was divided into eight thermal seasons, with temperature threshold values : 0, 5, 10 and 15 °C. The classification by Makowiec is based on the growth or fall of cumulative ranks of air temperature diminished by the temperature threshold value for a particular season. The determination of the initial dates enabled the calculation of the length of the seasons. The long-term analysis involved also the tendencies of length and changes of the initial date of a given season. The location of the meteorological station enables to expand the area of the interpretation of results into the borderland of the Beskid Niski Mts and the Carpathian Foothills. A high variability of the dates of the start and the duration of seasons was observed. The trends of duration and starting dates are multidirectional. The longest season is summer ( 89 days ), which starts increasingly earlier and lasts increasingly longer. An increase in duration also refers to pre-spring and autumn. Increasingly shorter winters and springs were also observed within the multi-year period.</description><subject>Air temperature</subject><subject>Classification</subject><subject>Geography</subject><subject>Geography, Regional studies</subject><subject>Historical Geography</subject><subject>History</subject><subject>Physical Geopgraphy</subject><subject>Recent History (1900 till today)</subject><subject>Seasons</subject><subject>Temperature</subject><subject>Variability</subject><issn>1644-3586</issn><issn>2083-3113</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2016</creationdate><recordtype>article</recordtype><sourceid>REL</sourceid><sourceid>8G5</sourceid><sourceid>BENPR</sourceid><sourceid>GUQSH</sourceid><sourceid>M2O</sourceid><recordid>eNpFjc9KAzEYxIMoWGrfQCTgRQ-7_b78-TY5SrFVKCi495KkCVjbbt11kfbkO_iGPom7VHAuMzA_Zhi7QsiVomIswEiJKJ9nOVIOQuQERp2wQV9kfXPKBkhKZVIbOmejpllBJzKaQAzYuIz15jUctpHvqnrP6-qt5Z_85bDfeFd3-QYtGf7z9c0FoLy9YGfJrZs4-vMhK6f35eQhmz_NHid38ywoazKVjFU-hiVKDD6BLpxGQm09BNLCOut1CpoKnUSIxsPSOik9KeOcS8rIIbs-zu7q6r2NzcdiVbX1tntciG5NaEvUU5dHKsRYrf8RjQBSyl_hNE5p</recordid><startdate>2016</startdate><enddate>2016</enddate><creator>Bochenek , Witold</creator><general>Wydawnictwo Uniwersytetu Jagiellońskiego</general><general>Jagiellonian University Press</general><general>Jagiellonian University-Jagiellonian University Press</general><scope>AE2</scope><scope>BIXPP</scope><scope>REL</scope><scope>3V.</scope><scope>7XB</scope><scope>8BJ</scope><scope>8FK</scope><scope>8G5</scope><scope>ABUWG</scope><scope>AEUYN</scope><scope>AFKRA</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>BHPHI</scope><scope>BKSAR</scope><scope>BYOGL</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>FQK</scope><scope>GNUQQ</scope><scope>GUQSH</scope><scope>HCIFZ</scope><scope>JBE</scope><scope>M2O</scope><scope>MBDVC</scope><scope>PADUT</scope><scope>PCBAR</scope><scope>PHGZM</scope><scope>PHGZT</scope><scope>PKEHL</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PRINS</scope><scope>Q9U</scope></search><sort><creationdate>2016</creationdate><title>Termiczne pory roku w Szymbarku (1968 – 2013)</title><author>Bochenek , Witold</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c498-4f894becd131cbf057a516159b0c6529a9b5fc5675f2ce8b0d9a33b648aaaf483</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>pol</language><creationdate>2016</creationdate><topic>Air temperature</topic><topic>Classification</topic><topic>Geography</topic><topic>Geography, Regional studies</topic><topic>Historical Geography</topic><topic>History</topic><topic>Physical Geopgraphy</topic><topic>Recent History (1900 till today)</topic><topic>Seasons</topic><topic>Temperature</topic><topic>Variability</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Bochenek , Witold</creatorcontrib><collection>Central and Eastern European Online Library (C.E.E.O.L.) (DFG Nationallizenzen)</collection><collection>CEEOL: Open Access</collection><collection>Central and Eastern European Online Library</collection><collection>ProQuest Central (Corporate)</collection><collection>ProQuest Central (purchase pre-March 2016)</collection><collection>International Bibliography of the Social Sciences (IBSS)</collection><collection>ProQuest Central (Alumni) (purchase pre-March 2016)</collection><collection>Research Library (Alumni Edition)</collection><collection>ProQuest Central (Alumni Edition)</collection><collection>ProQuest One Sustainability</collection><collection>ProQuest Central UK/Ireland</collection><collection>ProQuest Central Essentials</collection><collection>ProQuest Central</collection><collection>Natural Science Collection</collection><collection>Earth, Atmospheric & Aquatic Science Collection</collection><collection>East Europe, Central Europe Database</collection><collection>ProQuest One Community College</collection><collection>ProQuest Central Korea</collection><collection>International Bibliography of the Social Sciences</collection><collection>ProQuest Central Student</collection><collection>Research Library Prep</collection><collection>SciTech Premium Collection</collection><collection>International Bibliography of the Social Sciences</collection><collection>Research Library</collection><collection>Research Library (Corporate)</collection><collection>Research Library China</collection><collection>Earth, Atmospheric & Aquatic Science Database</collection><collection>ProQuest Central (New)</collection><collection>ProQuest One Academic (New)</collection><collection>ProQuest One Academic Middle East (New)</collection><collection>ProQuest One Academic Eastern Edition (DO NOT USE)</collection><collection>ProQuest One Academic</collection><collection>ProQuest One Academic UKI Edition</collection><collection>ProQuest Central China</collection><collection>ProQuest Central Basic</collection><jtitle>Prace geograficzne (Kraków, Poland)</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Bochenek , Witold</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Termiczne pory roku w Szymbarku (1968 – 2013)</atitle><jtitle>Prace geograficzne (Kraków, Poland)</jtitle><addtitle>Geographical Studies</addtitle><date>2016</date><risdate>2016</risdate><issue>147</issue><spage>67</spage><epage>80</epage><pages>67-80</pages><issn>1644-3586</issn><eissn>2083-3113</eissn><abstract>The article contains an analysis of the duration and the dates of the start of thermal seasons of the year, distinguished on the basis of the average daily air temperature at the Institute of Geography and Spatial Organization Research Station at Szymbark over a period of 46 years ( 1968–2013 ). To determine the initial dates of thermal seasons a method proposed by Makowiec (1983 ) was used. According to this method, the year was divided into eight thermal seasons, with temperature threshold values : 0, 5, 10 and 15 °C. The classification by Makowiec is based on the growth or fall of cumulative ranks of air temperature diminished by the temperature threshold value for a particular season. The determination of the initial dates enabled the calculation of the length of the seasons. The long-term analysis involved also the tendencies of length and changes of the initial date of a given season. The location of the meteorological station enables to expand the area of the interpretation of results into the borderland of the Beskid Niski Mts and the Carpathian Foothills. A high variability of the dates of the start and the duration of seasons was observed. The trends of duration and starting dates are multidirectional. The longest season is summer ( 89 days ), which starts increasingly earlier and lasts increasingly longer. An increase in duration also refers to pre-spring and autumn. Increasingly shorter winters and springs were also observed within the multi-year period.</abstract><cop>Kraków</cop><pub>Wydawnictwo Uniwersytetu Jagiellońskiego</pub><doi>10.4467/20833113PG.16.022.6084</doi><tpages>14</tpages><oa>free_for_read</oa></addata></record> |
fulltext | fulltext |
identifier | ISSN: 1644-3586 |
ispartof | Prace geograficzne (Kraków, Poland), 2016 (147), p.67-80 |
issn | 1644-3586 2083-3113 |
language | pol |
recordid | cdi_proquest_journals_2057259668 |
source | Alma/SFX Local Collection |
subjects | Air temperature Classification Geography Geography, Regional studies Historical Geography History Physical Geopgraphy Recent History (1900 till today) Seasons Temperature Variability |
title | Termiczne pory roku w Szymbarku (1968 – 2013) |
url | https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-02-16T11%3A13%3A47IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-ceeol_proqu&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=Termiczne%20pory%20roku%20w%20Szymbarku%20(1968%20%E2%80%93%202013)&rft.jtitle=Prace%20geograficzne%20(Krak%C3%B3w,%20Poland)&rft.au=Bochenek%20,%20Witold&rft.date=2016&rft.issue=147&rft.spage=67&rft.epage=80&rft.pages=67-80&rft.issn=1644-3586&rft.eissn=2083-3113&rft_id=info:doi/10.4467/20833113PG.16.022.6084&rft_dat=%3Cceeol_proqu%3E510033%3C/ceeol_proqu%3E%3Curl%3E%3C/url%3E&disable_directlink=true&sfx.directlink=off&sfx.report_link=0&rft_id=info:oai/&rft_pqid=2057259668&rft_id=info:pmid/&rft_ceeol_id=510033&rfr_iscdi=true |