Influence of air–soil temperature on leaf expansion and LAI of Carpinus betulus trees in a temperate urban forest patch

•Maximum leaf area and leaf area index were achieved in early and late May, respectively.•Soil temperature had a significant influence on LA and LAI.•Influence of current year's air temperature was significant only for LAI.•Preceding year's mean air temperature was also effective on LA.•Th...

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Veröffentlicht in:Agricultural and forest meteorology 2015-01, Vol.200, p.185-191
Hauptverfasser: Oeztuerk, Melih, Bolat, Ilyas, Erguen, Ahmet
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Erguen, Ahmet
description •Maximum leaf area and leaf area index were achieved in early and late May, respectively.•Soil temperature had a significant influence on LA and LAI.•Influence of current year's air temperature was significant only for LAI.•Preceding year's mean air temperature was also effective on LA.•There was a significant correlation between the preceding year's sunlight duration and LA. Air temperature is effective meteorological parameter in overall leaf phenology of deciduous temperate forests. Not only the air temperature but also the soil temperature influences seasonal leaf development of deciduous trees. In order to determine the extent of air and soil temperature impact on the Carpinus betulus leaves, we analyzed two significant parameters; leaf area (LA) and leaf area index (LAI) as an indicator of leaf development. We monitored LA expansion through leaf harvesting with about weekly intervals from early April to late May, and LAI through hemispherical photographing from mid-March and mid-June. After the budburst and leaf unfolding between late March and early April, mean LAI and LA consecutively exhibited increasing patterns until their maximums (2.70 and 28.60cm2) in late May and early May, respectively. Both the LA and LAI trends were in accordance particularly with the soil temperatures of all layers. Namely, the coefficients (r) were at least 0.88 indicating high significance (P
doi_str_mv 10.1016/j.agrformet.2014.09.014
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Air temperature is effective meteorological parameter in overall leaf phenology of deciduous temperate forests. Not only the air temperature but also the soil temperature influences seasonal leaf development of deciduous trees. In order to determine the extent of air and soil temperature impact on the Carpinus betulus leaves, we analyzed two significant parameters; leaf area (LA) and leaf area index (LAI) as an indicator of leaf development. We monitored LA expansion through leaf harvesting with about weekly intervals from early April to late May, and LAI through hemispherical photographing from mid-March and mid-June. After the budburst and leaf unfolding between late March and early April, mean LAI and LA consecutively exhibited increasing patterns until their maximums (2.70 and 28.60cm2) in late May and early May, respectively. Both the LA and LAI trends were in accordance particularly with the soil temperatures of all layers. Namely, the coefficients (r) were at least 0.88 indicating high significance (P&lt;0.01) for all correlations. The correlations between LAI and air temperatures were also significant (P&lt;0.01) i.e. r=0.76, 0.82 and 0.88 for maximum, mean and minimum air temperatures, respectively. However, the correlations between LA and air temperatures were insignificant. Unlike the current year, there were significant correlations of the LA with both the preceding year's mean air temperature (P=0.05) and sunlight duration (P=0.02). 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Air temperature is effective meteorological parameter in overall leaf phenology of deciduous temperate forests. Not only the air temperature but also the soil temperature influences seasonal leaf development of deciduous trees. In order to determine the extent of air and soil temperature impact on the Carpinus betulus leaves, we analyzed two significant parameters; leaf area (LA) and leaf area index (LAI) as an indicator of leaf development. We monitored LA expansion through leaf harvesting with about weekly intervals from early April to late May, and LAI through hemispherical photographing from mid-March and mid-June. After the budburst and leaf unfolding between late March and early April, mean LAI and LA consecutively exhibited increasing patterns until their maximums (2.70 and 28.60cm2) in late May and early May, respectively. Both the LA and LAI trends were in accordance particularly with the soil temperatures of all layers. Namely, the coefficients (r) were at least 0.88 indicating high significance (P&lt;0.01) for all correlations. The correlations between LAI and air temperatures were also significant (P&lt;0.01) i.e. r=0.76, 0.82 and 0.88 for maximum, mean and minimum air temperatures, respectively. However, the correlations between LA and air temperatures were insignificant. Unlike the current year, there were significant correlations of the LA with both the preceding year's mean air temperature (P=0.05) and sunlight duration (P=0.02). Consequently, the results revealed the importance of relatively less referred parameter; soil temperature, primarily for the urban forest trees which are susceptible to anthropogenic climate warming.</description><subject>Carpinus betulus</subject><subject>Climate</subject><subject>Climate change</subject><subject>Correlation</subject><subject>Ecophysiology</subject><subject>European hornbeam</subject><subject>Forests</subject><subject>Hemispherical photographing</subject><subject>Impact analysis</subject><subject>Intervals</subject><subject>Leaf area index</subject><subject>Phenology</subject><subject>Soil temperature</subject><subject>Trees</subject><issn>0168-1923</issn><issn>1873-2240</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2015</creationdate><recordtype>article</recordtype><recordid>eNqNUctu2zAQJIoWqJPmG8JjLlJ2SZmUjobRJgYM5NKeCZpapTRkSSGporn1H_qH_ZJQcJBrehosdmb2MYxdI5QIqG6PpX0M3RhOlEoBWJXQlBk-sBXWWhZCVPCRrTKzLrAR8jO7iPEIgELrZsWed0PXzzQ44mPHrQ___vyNo-95otNEwaY55M7Ae7Idp9-THaLPpR1avt_sFs3WhskPc-QHSnOfMQWiyH0mvZkQn8PBDjyvSTHxySb38wv71Nk-0tUrXrIf375-394X-4e73XazL5ysMRVoZWdrsVZOV0h4kHUnlNCVUrJdr13lsG2VI2oBAaBu1hJqJ7WTwmqLlZKX7ObsO4Xxac7jzclHR31vBxrnaFApgErml_0HtdIACnFx1WeqC2OMgTozBX-y4dkgmCUXczRvuZglFwONOQ_ZnJWUj_7lKZjo_BJA6wO5ZNrRv-vxAtANnCE</recordid><startdate>20150101</startdate><enddate>20150101</enddate><creator>Oeztuerk, Melih</creator><creator>Bolat, Ilyas</creator><creator>Erguen, Ahmet</creator><general>Elsevier B.V</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7ST</scope><scope>7TG</scope><scope>7U6</scope><scope>7UA</scope><scope>C1K</scope><scope>KL.</scope><scope>SOI</scope><scope>8FD</scope><scope>FR3</scope><scope>H8D</scope><scope>KR7</scope><scope>L7M</scope></search><sort><creationdate>20150101</creationdate><title>Influence of air–soil temperature on leaf expansion and LAI of Carpinus betulus trees in a temperate urban forest patch</title><author>Oeztuerk, Melih ; Bolat, Ilyas ; Erguen, Ahmet</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c381t-1a3fa8256c741e1b38f26274663d55c4c1dd6ceed01000895308c37c32a7a1463</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2015</creationdate><topic>Carpinus betulus</topic><topic>Climate</topic><topic>Climate change</topic><topic>Correlation</topic><topic>Ecophysiology</topic><topic>European hornbeam</topic><topic>Forests</topic><topic>Hemispherical photographing</topic><topic>Impact analysis</topic><topic>Intervals</topic><topic>Leaf area index</topic><topic>Phenology</topic><topic>Soil temperature</topic><topic>Trees</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Oeztuerk, Melih</creatorcontrib><creatorcontrib>Bolat, Ilyas</creatorcontrib><creatorcontrib>Erguen, Ahmet</creatorcontrib><collection>CrossRef</collection><collection>Environment Abstracts</collection><collection>Meteorological &amp; Geoastrophysical Abstracts</collection><collection>Sustainability Science Abstracts</collection><collection>Water Resources Abstracts</collection><collection>Environmental Sciences and Pollution Management</collection><collection>Meteorological &amp; Geoastrophysical Abstracts - Academic</collection><collection>Environment Abstracts</collection><collection>Technology Research Database</collection><collection>Engineering Research Database</collection><collection>Aerospace Database</collection><collection>Civil Engineering Abstracts</collection><collection>Advanced Technologies Database with Aerospace</collection><jtitle>Agricultural and forest meteorology</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Oeztuerk, Melih</au><au>Bolat, Ilyas</au><au>Erguen, Ahmet</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Influence of air–soil temperature on leaf expansion and LAI of Carpinus betulus trees in a temperate urban forest patch</atitle><jtitle>Agricultural and forest meteorology</jtitle><date>2015-01-01</date><risdate>2015</risdate><volume>200</volume><spage>185</spage><epage>191</epage><pages>185-191</pages><issn>0168-1923</issn><eissn>1873-2240</eissn><abstract>•Maximum leaf area and leaf area index were achieved in early and late May, respectively.•Soil temperature had a significant influence on LA and LAI.•Influence of current year's air temperature was significant only for LAI.•Preceding year's mean air temperature was also effective on LA.•There was a significant correlation between the preceding year's sunlight duration and LA. Air temperature is effective meteorological parameter in overall leaf phenology of deciduous temperate forests. Not only the air temperature but also the soil temperature influences seasonal leaf development of deciduous trees. In order to determine the extent of air and soil temperature impact on the Carpinus betulus leaves, we analyzed two significant parameters; leaf area (LA) and leaf area index (LAI) as an indicator of leaf development. We monitored LA expansion through leaf harvesting with about weekly intervals from early April to late May, and LAI through hemispherical photographing from mid-March and mid-June. After the budburst and leaf unfolding between late March and early April, mean LAI and LA consecutively exhibited increasing patterns until their maximums (2.70 and 28.60cm2) in late May and early May, respectively. Both the LA and LAI trends were in accordance particularly with the soil temperatures of all layers. Namely, the coefficients (r) were at least 0.88 indicating high significance (P&lt;0.01) for all correlations. The correlations between LAI and air temperatures were also significant (P&lt;0.01) i.e. r=0.76, 0.82 and 0.88 for maximum, mean and minimum air temperatures, respectively. However, the correlations between LA and air temperatures were insignificant. Unlike the current year, there were significant correlations of the LA with both the preceding year's mean air temperature (P=0.05) and sunlight duration (P=0.02). Consequently, the results revealed the importance of relatively less referred parameter; soil temperature, primarily for the urban forest trees which are susceptible to anthropogenic climate warming.</abstract><pub>Elsevier B.V</pub><doi>10.1016/j.agrformet.2014.09.014</doi><tpages>7</tpages></addata></record>
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subjects Carpinus betulus
Climate
Climate change
Correlation
Ecophysiology
European hornbeam
Forests
Hemispherical photographing
Impact analysis
Intervals
Leaf area index
Phenology
Soil temperature
Trees
title Influence of air–soil temperature on leaf expansion and LAI of Carpinus betulus trees in a temperate urban forest patch
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