Modelling the Effect of Temperature on Height Increment of Scots Pine at High Latitudes

The effect of temperature and precipitation on the height increment of Pinus sylvestris (L.) was modelled using data gathered from a total of 49 felled sample trees from five stands of Scots pine located along a latitudinal transect from the Arctic Circle up to the northern timberline in Finland. A...

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Main Authors: Hannu Salminen, Risto Jalkanen
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Published: 2005
Subjects:
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.520.5132
http://www.metla.fi/silvafennica/full/sf39/sf394497.pdf
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spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.520.5132 2023-05-15T15:09:45+02:00 Modelling the Effect of Temperature on Height Increment of Scots Pine at High Latitudes Hannu Salminen Risto Jalkanen The Pennsylvania State University CiteSeerX Archives 2005 application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.520.5132 http://www.metla.fi/silvafennica/full/sf39/sf394497.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.520.5132 http://www.metla.fi/silvafennica/full/sf39/sf394497.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.metla.fi/silvafennica/full/sf39/sf394497.pdf temperature dendroclimatology precipitation Pinus sylves text 2005 ftciteseerx 2016-01-08T10:06:23Z The effect of temperature and precipitation on the height increment of Pinus sylvestris (L.) was modelled using data gathered from a total of 49 felled sample trees from five stands of Scots pine located along a latitudinal transect from the Arctic Circle up to the northern timberline in Finland. A multilevel mixed effects model and cross-correlation analysis of prewhitened time series was used to analyse the dependence between height increment and monthly meteorological observations. The effect of the mean July temperature of the previ-ous year on height increment proved to be very strong at high latitudes (r> 0.7). The mean November temperature of the year before the previous affected statistically significantly on height increment in the three northernmost stands. There was no correlation between height increment and precipitation in any of the sites. The final height increment model based on all stands included tree age, long-term mean temperature sum of site, and the mean July temperature of the previous year as independent variables. According to the model, one degree’s change in July temperature results on average in 1.8 cm change in the next year’s height increment. There was a modest but significant polynomial age-effect. The proportion of explained variance (at the year level) was 74%. The July temperature dependence on height increment was shown to be very strong, suggesting a high value of height increment in climate modelling at the tree line. Text Arctic Unknown Arctic
institution Open Polar
collection Unknown
op_collection_id ftciteseerx
language English
topic temperature
dendroclimatology
precipitation
Pinus sylves
spellingShingle temperature
dendroclimatology
precipitation
Pinus sylves
Hannu Salminen
Risto Jalkanen
Modelling the Effect of Temperature on Height Increment of Scots Pine at High Latitudes
topic_facet temperature
dendroclimatology
precipitation
Pinus sylves
description The effect of temperature and precipitation on the height increment of Pinus sylvestris (L.) was modelled using data gathered from a total of 49 felled sample trees from five stands of Scots pine located along a latitudinal transect from the Arctic Circle up to the northern timberline in Finland. A multilevel mixed effects model and cross-correlation analysis of prewhitened time series was used to analyse the dependence between height increment and monthly meteorological observations. The effect of the mean July temperature of the previ-ous year on height increment proved to be very strong at high latitudes (r> 0.7). The mean November temperature of the year before the previous affected statistically significantly on height increment in the three northernmost stands. There was no correlation between height increment and precipitation in any of the sites. The final height increment model based on all stands included tree age, long-term mean temperature sum of site, and the mean July temperature of the previous year as independent variables. According to the model, one degree’s change in July temperature results on average in 1.8 cm change in the next year’s height increment. There was a modest but significant polynomial age-effect. The proportion of explained variance (at the year level) was 74%. The July temperature dependence on height increment was shown to be very strong, suggesting a high value of height increment in climate modelling at the tree line.
author2 The Pennsylvania State University CiteSeerX Archives
format Text
author Hannu Salminen
Risto Jalkanen
author_facet Hannu Salminen
Risto Jalkanen
author_sort Hannu Salminen
title Modelling the Effect of Temperature on Height Increment of Scots Pine at High Latitudes
title_short Modelling the Effect of Temperature on Height Increment of Scots Pine at High Latitudes
title_full Modelling the Effect of Temperature on Height Increment of Scots Pine at High Latitudes
title_fullStr Modelling the Effect of Temperature on Height Increment of Scots Pine at High Latitudes
title_full_unstemmed Modelling the Effect of Temperature on Height Increment of Scots Pine at High Latitudes
title_sort modelling the effect of temperature on height increment of scots pine at high latitudes
publishDate 2005
url http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.520.5132
http://www.metla.fi/silvafennica/full/sf39/sf394497.pdf
geographic Arctic
geographic_facet Arctic
genre Arctic
genre_facet Arctic
op_source http://www.metla.fi/silvafennica/full/sf39/sf394497.pdf
op_relation http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.520.5132
http://www.metla.fi/silvafennica/full/sf39/sf394497.pdf
op_rights Metadata may be used without restrictions as long as the oai identifier remains attached to it.
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