The Influence of Temperature and Precipitation on Ring Widths of Oak (Quercus Robur L.) in the Niepolomice Forest Near Cracow, Southern Poland
dc.contributor.author | Bednarz, Z. | |
dc.contributor.author | Ptak, J. | |
dc.date.accessioned | 2012-12-12T23:04:13Z | |
dc.date.available | 2012-12-12T23:04:13Z | |
dc.date.issued | 1990 | |
dc.identifier.citation | Bednarz, Z., Ptak, J. 1990. The influence of temperature and precipitation on ring widths of oak (Quercus robur L.) in the Niepolomice forest near Cracow, Southern Poland. Tree-Ring Bulletin 50:1-10. | en_US |
dc.identifier.issn | 0041-2198 | |
dc.identifier.uri | http://hdl.handle.net/10150/261919 | |
dc.description.abstract | Analysis of the relationship between ring-width indices of pedunculate oaks (Quercus robur L.) in the Niepotomice Forest with average monthly air temperatures (1826-1980) and total monthly precipitation (1881-1985) in Cracow revealed a strict relationship between tree -growth and the precipitation of June-July, May-July, and June-August. These relationships are described by a high percentage of agreement, at or around 70 %, and coefficients of correlation (rx) of 0.40 (June-July), 0.36 (May-July) and 0.30 (June-August). The group of 10 oaks with the highest coefficients between growth and precipitation yielded still higher correlations: 0.50, 0.50, and 0.41, respectively. High total monthly precipitation in June and July favors radial growth, while low precipitation reduces radial growth. The influence of air temperature on oak ring-width indices is less significant. The highest positive correlation occurs for January to April of the preceding year. Correlations for the years of radial growth have values close to or below (June) zero except for August. | |
dc.language.iso | en_US | en_US |
dc.publisher | Tree-Ring Society | en_US |
dc.relation.url | http://www.treeringsociety.org | en_US |
dc.rights | Copyright © Tree-Ring Society. All rights reserved. | en_US |
dc.subject | Dendrochronology | en_US |
dc.subject | Tree Rings | en_US |
dc.subject | Air Temperature | en_US |
dc.subject | Dendroclimatology | en_US |
dc.subject | Forest Trees | en_US |
dc.subject | Growth Rings | en_US |
dc.subject | Precipitation | en_US |
dc.subject | Trees | en_US |
dc.subject | Woody Plants | en_US |
dc.title | The Influence of Temperature and Precipitation on Ring Widths of Oak (Quercus Robur L.) in the Niepolomice Forest Near Cracow, Southern Poland | en_US |
dc.type | Article | en_US |
dc.contributor.department | Department of Forest Botany and Nature Protection, Academy of Agriculture, Kraków, Poland | en_US |
dc.contributor.department | Computer Centre Academy of Agriculture, Kraków, Poland | en_US |
dc.identifier.journal | Tree-Ring Bulletin | en_US |
dc.description.collectioninformation | This item is part of the Tree-Ring Research (formerly Tree-Ring Bulletin) archive. It was digitized from a physical copy provided by the Laboratory of Tree-Ring research at The University of Arizona. For more information about this peer-reviewed scholarly journal, please email the Editor of Tree-Ring Research at editor@treeringsociety.org. | en_US |
refterms.dateFOA | 2018-06-26T23:51:45Z | |
html.description.abstract | Analysis of the relationship between ring-width indices of pedunculate oaks (Quercus robur L.) in the Niepotomice Forest with average monthly air temperatures (1826-1980) and total monthly precipitation (1881-1985) in Cracow revealed a strict relationship between tree -growth and the precipitation of June-July, May-July, and June-August. These relationships are described by a high percentage of agreement, at or around 70 %, and coefficients of correlation (rx) of 0.40 (June-July), 0.36 (May-July) and 0.30 (June-August). The group of 10 oaks with the highest coefficients between growth and precipitation yielded still higher correlations: 0.50, 0.50, and 0.41, respectively. High total monthly precipitation in June and July favors radial growth, while low precipitation reduces radial growth. The influence of air temperature on oak ring-width indices is less significant. The highest positive correlation occurs for January to April of the preceding year. Correlations for the years of radial growth have values close to or below (June) zero except for August. |