Large-scale climatic variability and radial increment variation of Picea abies (L.) Karst. in central and northern Europe

被引:0
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作者
Harri Mäkinen
Pekka Nöjd
Hans-Peter Kahle
Ulrich Neumann
Björn Tveite
Kari Mielikäinen
Heinz Röhle
Heinrich Spiecker
机构
[1] Finnish Forest Research Institute,
[2] P.O. Box 18,undefined
[3] 01301 Vantaa,undefined
[4] Finland,undefined
[5] Institute for Forest Growth,undefined
[6] University of Freiburg,undefined
[7] Tennenbacherstrasse 4,undefined
[8] 79085 Freiburg,undefined
[9] Germany,undefined
[10] Institute of Forest Growth and Forest Informatics,undefined
[11] University of Dresden,undefined
[12] Wilsdrufferstrasse 18,undefined
[13] 01737 Tharandt,undefined
[14] Germany,undefined
[15] Norwegian Forest Research Institute,undefined
[16] Hoegskolevn. 12,undefined
[17] 1432 Ås,undefined
[18] Norway,undefined
[19] Finnish Forest Research Institute,undefined
[20] Unioninkatu 40,undefined
[21] 00170 Helsinki,undefined
[22] Finland,undefined
来源
Trees | 2003年 / 17卷
关键词
North Atlantic Oscillation Picea abies Precipitation Radial increment variation Temperature;
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摘要
High-frequency variation of Norway spruce radial increment [Picea abies (L.) Karst.] and its dependence on various climatic variables was compared in stands across latitudinal and altitudinal transects in southwestern and eastern Germany, Norway, and Finland. The tested variables included local temperature and precipitation, northern hemisphere temperature anomalies, and the climatic teleconnection patterns (North Atlantic Oscillation, East Atlantic, East Atlantic Jet, East Atlantic/West Russia, and Scandinavian patterns). Climatic impact on radial increment increased towards minimum and maximum values of the long-term temperature and precipitation regimes, i.e. trees growing under average conditions respond less strongly to climatic variation. Increment variation was clearly correlated with temperature. Warm Mays promoted radial increments in all regions. If the long-term average temperature sum at a stand was below 1,200–1,300 degree days, above average summer temperature increased radial increment. In regions with more temperate climate, water availability was also a growth-limiting factor. However, in those cases where absolute precipitation sum was clearly related to radial increment variation, its effect was dependent on temperature-induced water stress. The estimated dates of initiation and cessation of growing season and growing season length were not clearly related to annual radial increment. Significant correlations were found between radial increment and climatic teleconnection indices, especially with the winter, May and August North Atlantic Oscillation indices, but it is not easy to find a physiological interpretation for these findings.
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页码:173 / 184
页数:11
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