Water balance analysis of the Morava River floodplain in the Kostice-Lanžhot transect using the WBCM-7 model
The study area of the Morava River floodplain is situated between the rivers Morava and Kyjovka in the reach from Hodonín to Lanžhot. This experimental area was chosen because during the last 30 years, there has been a serious problem with the frequent occurrence of hydrological extremes, such as fl...
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| Veröffentlicht in: | Environmental monitoring and assessment 2016-02, Vol.188 (2), p.74-74, Article 74 |
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| creator | Kovář, Pavel Heřmanovská, Darina Hadaš, Pavel Hrabalíková, Michaela Pešková, Jitka |
| description | The study area of the Morava River floodplain is situated between the rivers Morava and Kyjovka in the reach from Hodonín to Lanžhot. This experimental area was chosen because during the last 30 years, there has been a serious problem with the frequent occurrence of hydrological extremes, such as floods and droughts. Dry seasons have a very negative impact on the floodplain forest and have been caused mainly by regulation of the Morava River channel in the 1970s. Since flooding in the catastrophic year 1977, a part of this area has served as a polder for flood impact mitigation of the urbanised area of the town of Lanžhot. Management and farming practices have been heavily affected by the enormous economic and ecological damage due to long-term flooding of agricultural land. The purpose of this study is to assess the extent to which the precipitation in the growing season of the dry years 2003 and 2011 was deficient, in comparison with the normal year 2009, through a study of the actual evapotranspiration caused by the significant drought in the Morava floodplain. A similar but converse situation in the wet year 2010 was also analysed, with the aim to show the differences in the components of the water balance equation in the growing seasons of all the extreme years tested here. The daily data from the Kostice climatological station were processed using the WBCM-7 model, where the input parameters were calibrated by the fluctuation of the groundwater table in the control borehole. |
| doi_str_mv | 10.1007/s10661-015-5080-7 |
| format | Article |
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This experimental area was chosen because during the last 30 years, there has been a serious problem with the frequent occurrence of hydrological extremes, such as floods and droughts. Dry seasons have a very negative impact on the floodplain forest and have been caused mainly by regulation of the Morava River channel in the 1970s. Since flooding in the catastrophic year 1977, a part of this area has served as a polder for flood impact mitigation of the urbanised area of the town of Lanžhot. Management and farming practices have been heavily affected by the enormous economic and ecological damage due to long-term flooding of agricultural land. The purpose of this study is to assess the extent to which the precipitation in the growing season of the dry years 2003 and 2011 was deficient, in comparison with the normal year 2009, through a study of the actual evapotranspiration caused by the significant drought in the Morava floodplain. A similar but converse situation in the wet year 2010 was also analysed, with the aim to show the differences in the components of the water balance equation in the growing seasons of all the extreme years tested here. The daily data from the Kostice climatological station were processed using the WBCM-7 model, where the input parameters were calibrated by the fluctuation of the groundwater table in the control borehole.</description><identifier>ISSN: 0167-6369</identifier><identifier>EISSN: 1573-2959</identifier><identifier>DOI: 10.1007/s10661-015-5080-7</identifier><identifier>PMID: 26733468</identifier><language>eng</language><publisher>Cham: Springer International Publishing</publisher><subject>Agricultural land ; Agricultural practices ; Agriculture ; Atmospheric Protection/Air Quality Control/Air Pollution ; Boreholes ; Drought ; Droughts - statistics & numerical data ; Dry season ; Earth and Environmental Science ; Ecology ; Ecotoxicology ; Environment ; Environmental Management ; Environmental Monitoring ; equations ; Evapotranspiration ; farming systems ; Flood damage ; Flooding ; Floodplains ; Floods ; Floods - statistics & numerical data ; forests ; Groundwater ; Groundwater - analysis ; Growing season ; Hydrology ; Models, Theoretical ; Monitoring/Environmental Analysis ; Polders ; Precipitation ; Rain ; Rivers ; Rivers - chemistry ; Seasons ; Storm damage ; Studies ; urbanization ; Water balance ; Water shortages ; Water Supply - statistics & numerical data ; Water table</subject><ispartof>Environmental monitoring and assessment, 2016-02, Vol.188 (2), p.74-74, Article 74</ispartof><rights>Springer International Publishing Switzerland 2016</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c396t-a0a7c6df84fd178afb57478ac28ae527aa7cae4e4c37ae0773afea3dd165482b3</citedby><cites>FETCH-LOGICAL-c396t-a0a7c6df84fd178afb57478ac28ae527aa7cae4e4c37ae0773afea3dd165482b3</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1007/s10661-015-5080-7$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1007/s10661-015-5080-7$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,780,784,27924,27925,41488,42557,51319</link.rule.ids><backlink>$$Uhttps://www.ncbi.nlm.nih.gov/pubmed/26733468$$D View this record in MEDLINE/PubMed$$Hfree_for_read</backlink></links><search><creatorcontrib>Kovář, Pavel</creatorcontrib><creatorcontrib>Heřmanovská, Darina</creatorcontrib><creatorcontrib>Hadaš, Pavel</creatorcontrib><creatorcontrib>Hrabalíková, Michaela</creatorcontrib><creatorcontrib>Pešková, Jitka</creatorcontrib><title>Water balance analysis of the Morava River floodplain in the Kostice-Lanžhot transect using the WBCM-7 model</title><title>Environmental monitoring and assessment</title><addtitle>Environ Monit Assess</addtitle><addtitle>Environ Monit Assess</addtitle><description>The study area of the Morava River floodplain is situated between the rivers Morava and Kyjovka in the reach from Hodonín to Lanžhot. This experimental area was chosen because during the last 30 years, there has been a serious problem with the frequent occurrence of hydrological extremes, such as floods and droughts. Dry seasons have a very negative impact on the floodplain forest and have been caused mainly by regulation of the Morava River channel in the 1970s. Since flooding in the catastrophic year 1977, a part of this area has served as a polder for flood impact mitigation of the urbanised area of the town of Lanžhot. Management and farming practices have been heavily affected by the enormous economic and ecological damage due to long-term flooding of agricultural land. The purpose of this study is to assess the extent to which the precipitation in the growing season of the dry years 2003 and 2011 was deficient, in comparison with the normal year 2009, through a study of the actual evapotranspiration caused by the significant drought in the Morava floodplain. A similar but converse situation in the wet year 2010 was also analysed, with the aim to show the differences in the components of the water balance equation in the growing seasons of all the extreme years tested here. The daily data from the Kostice climatological station were processed using the WBCM-7 model, where the input parameters were calibrated by the fluctuation of the groundwater table in the control borehole.</description><subject>Agricultural land</subject><subject>Agricultural practices</subject><subject>Agriculture</subject><subject>Atmospheric Protection/Air Quality Control/Air Pollution</subject><subject>Boreholes</subject><subject>Drought</subject><subject>Droughts - statistics & numerical data</subject><subject>Dry season</subject><subject>Earth and Environmental Science</subject><subject>Ecology</subject><subject>Ecotoxicology</subject><subject>Environment</subject><subject>Environmental Management</subject><subject>Environmental Monitoring</subject><subject>equations</subject><subject>Evapotranspiration</subject><subject>farming systems</subject><subject>Flood damage</subject><subject>Flooding</subject><subject>Floodplains</subject><subject>Floods</subject><subject>Floods - statistics & numerical data</subject><subject>forests</subject><subject>Groundwater</subject><subject>Groundwater - analysis</subject><subject>Growing season</subject><subject>Hydrology</subject><subject>Models, Theoretical</subject><subject>Monitoring/Environmental Analysis</subject><subject>Polders</subject><subject>Precipitation</subject><subject>Rain</subject><subject>Rivers</subject><subject>Rivers - chemistry</subject><subject>Seasons</subject><subject>Storm damage</subject><subject>Studies</subject><subject>urbanization</subject><subject>Water balance</subject><subject>Water shortages</subject><subject>Water Supply - statistics & numerical data</subject><subject>Water table</subject><issn>0167-6369</issn><issn>1573-2959</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2016</creationdate><recordtype>article</recordtype><sourceid>EIF</sourceid><sourceid>ABUWG</sourceid><sourceid>AFKRA</sourceid><sourceid>AZQEC</sourceid><sourceid>BENPR</sourceid><sourceid>CCPQU</sourceid><sourceid>DWQXO</sourceid><sourceid>GNUQQ</sourceid><recordid>eNp9kUFv1DAQhS0EokvhB3ABS1y4GMZ2bCdHWEFBbIUEVD1as469TZXEWzup1D_XG_8Lb1MQ4oBkaQ7zvWfNe4Q85_CGA5i3mYPWnAFXTEENzDwgK66MZKJRzUOyAq4N01I3R-RJzpcA0JiqeUyOhDZSVrpekeEcJ5_oFnscnac4Yn-Tu0xjoNOFp6cx4TXSb911gUIfY7vvsRtpeYf1l5inznm2wfHn7UWc6JRwzN5NdM7duLtjzt-vT5mhQ2x9_5Q8Cthn_-x-HpOzjx9-rD-xzdeTz-t3G-ZkoyeGgMbpNtRVaLmpMWyVqcp0okavhMGyRl_5ykmDHoyRGDzKtuVaVbXYymPyevHdp3g1-zzZocvO9-VIH-dsuVGVEkJwXtBX_6CXcU4lhjtKyhIYQKH4QrkUc04-2H3qBkw3loM9dGGXLmzpwh66sKZoXtw7z9vBt38Uv8MvgFiAXFbjzqe_vv6P68tFFDBa3KUu27PvojQNwIXmwshf06ueBw</recordid><startdate>20160201</startdate><enddate>20160201</enddate><creator>Kovář, Pavel</creator><creator>Heřmanovská, Darina</creator><creator>Hadaš, Pavel</creator><creator>Hrabalíková, Michaela</creator><creator>Pešková, Jitka</creator><general>Springer International Publishing</general><general>Springer Nature B.V</general><scope>FBQ</scope><scope>CGR</scope><scope>CUY</scope><scope>CVF</scope><scope>ECM</scope><scope>EIF</scope><scope>NPM</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>3V.</scope><scope>7QH</scope><scope>7QL</scope><scope>7SN</scope><scope>7ST</scope><scope>7T7</scope><scope>7TG</scope><scope>7TN</scope><scope>7U7</scope><scope>7UA</scope><scope>7WY</scope><scope>7WZ</scope><scope>7X7</scope><scope>7XB</scope><scope>87Z</scope><scope>88E</scope><scope>88I</scope><scope>8AO</scope><scope>8C1</scope><scope>8FD</scope><scope>8FI</scope><scope>8FJ</scope><scope>8FK</scope><scope>8FL</scope><scope>ABUWG</scope><scope>AFKRA</scope><scope>ATCPS</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>BEZIV</scope><scope>BHPHI</scope><scope>C1K</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>F1W</scope><scope>FR3</scope><scope>FRNLG</scope><scope>FYUFA</scope><scope>F~G</scope><scope>GHDGH</scope><scope>GNUQQ</scope><scope>H97</scope><scope>HCIFZ</scope><scope>K60</scope><scope>K6~</scope><scope>K9.</scope><scope>KL.</scope><scope>L.-</scope><scope>L.G</scope><scope>M0C</scope><scope>M0S</scope><scope>M1P</scope><scope>M2P</scope><scope>M7N</scope><scope>P64</scope><scope>PATMY</scope><scope>PQBIZ</scope><scope>PQBZA</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PYCSY</scope><scope>Q9U</scope><scope>SOI</scope><scope>7X8</scope></search><sort><creationdate>20160201</creationdate><title>Water balance analysis of the Morava River floodplain in the Kostice-Lanžhot transect using the WBCM-7 model</title><author>Kovář, Pavel ; Heřmanovská, Darina ; Hadaš, Pavel ; Hrabalíková, Michaela ; Pešková, Jitka</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c396t-a0a7c6df84fd178afb57478ac28ae527aa7cae4e4c37ae0773afea3dd165482b3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2016</creationdate><topic>Agricultural land</topic><topic>Agricultural practices</topic><topic>Agriculture</topic><topic>Atmospheric Protection/Air Quality Control/Air Pollution</topic><topic>Boreholes</topic><topic>Drought</topic><topic>Droughts - 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Academic</collection><jtitle>Environmental monitoring and assessment</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Kovář, Pavel</au><au>Heřmanovská, Darina</au><au>Hadaš, Pavel</au><au>Hrabalíková, Michaela</au><au>Pešková, Jitka</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Water balance analysis of the Morava River floodplain in the Kostice-Lanžhot transect using the WBCM-7 model</atitle><jtitle>Environmental monitoring and assessment</jtitle><stitle>Environ Monit Assess</stitle><addtitle>Environ Monit Assess</addtitle><date>2016-02-01</date><risdate>2016</risdate><volume>188</volume><issue>2</issue><spage>74</spage><epage>74</epage><pages>74-74</pages><artnum>74</artnum><issn>0167-6369</issn><eissn>1573-2959</eissn><abstract>The study area of the Morava River floodplain is situated between the rivers Morava and Kyjovka in the reach from Hodonín to Lanžhot. This experimental area was chosen because during the last 30 years, there has been a serious problem with the frequent occurrence of hydrological extremes, such as floods and droughts. Dry seasons have a very negative impact on the floodplain forest and have been caused mainly by regulation of the Morava River channel in the 1970s. Since flooding in the catastrophic year 1977, a part of this area has served as a polder for flood impact mitigation of the urbanised area of the town of Lanžhot. Management and farming practices have been heavily affected by the enormous economic and ecological damage due to long-term flooding of agricultural land. The purpose of this study is to assess the extent to which the precipitation in the growing season of the dry years 2003 and 2011 was deficient, in comparison with the normal year 2009, through a study of the actual evapotranspiration caused by the significant drought in the Morava floodplain. A similar but converse situation in the wet year 2010 was also analysed, with the aim to show the differences in the components of the water balance equation in the growing seasons of all the extreme years tested here. The daily data from the Kostice climatological station were processed using the WBCM-7 model, where the input parameters were calibrated by the fluctuation of the groundwater table in the control borehole.</abstract><cop>Cham</cop><pub>Springer International Publishing</pub><pmid>26733468</pmid><doi>10.1007/s10661-015-5080-7</doi><tpages>1</tpages></addata></record> |
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| ispartof | Environmental monitoring and assessment, 2016-02, Vol.188 (2), p.74-74, Article 74 |
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| source | MEDLINE; Springer Nature - Complete Springer Journals |
| subjects | Agricultural land Agricultural practices Agriculture Atmospheric Protection/Air Quality Control/Air Pollution Boreholes Drought Droughts - statistics & numerical data Dry season Earth and Environmental Science Ecology Ecotoxicology Environment Environmental Management Environmental Monitoring equations Evapotranspiration farming systems Flood damage Flooding Floodplains Floods Floods - statistics & numerical data forests Groundwater Groundwater - analysis Growing season Hydrology Models, Theoretical Monitoring/Environmental Analysis Polders Precipitation Rain Rivers Rivers - chemistry Seasons Storm damage Studies urbanization Water balance Water shortages Water Supply - statistics & numerical data Water table |
| title | Water balance analysis of the Morava River floodplain in the Kostice-Lanžhot transect using the WBCM-7 model |
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