Dendroclimatic analysis of Betula ermanii forests at their upper limit of distribution in Changbai Mountain, Northeast China [An article from: Forest Ecology and Management]
Book Details
Author(s)D. Yu, G.G. Wang, L. Dai, Q. Wang
PublisherElsevier
ISBN / ASINB000PDT7LU
ISBN-13978B000PDT7L5
AvailabilityAvailable for download now
MarketplaceUnited States 🇺🇸
Description
This digital document is a journal article from Forest Ecology and Management, published by Elsevier in 2007. The article is delivered in HTML format and is available in your Amazon.com Media Library immediately after purchase. You can view it with any web browser.
Description:
In order to detect the effects of climate change on Erman's birch (Betula ermanii Charm.), we examined radial growth-climate relationships of Erman's birch forests at their upper limit of distribution in Changbai Mountain, Northeast China. Thirty Erman's birch trees from six stands were sampled at an elevation of about 1950m a.s.l. Correlation and response function coefficients indicated that radial growth of Erman's birch was positively influenced by previous August, October and current February temperature, and previous winter, and current March, June and September precipitation. In addition, radial growth showed a negative relationship to previous August and current June sunshine ratio. Precipitation and temperatures in annualization periods also positively affected the radial growth of Erman's birch. Regression analyses indicated that precipitation explained more variation in radial growth than minimum temperature. Together, these results suggested that climate affected radial growth of Erman's birch through altering soil water availability. Therefore, the radial growth of Erman's birch at the tree line in Changbai Mountain could not be predicted by temperature alone even under a scenario of global warming.
Description:
In order to detect the effects of climate change on Erman's birch (Betula ermanii Charm.), we examined radial growth-climate relationships of Erman's birch forests at their upper limit of distribution in Changbai Mountain, Northeast China. Thirty Erman's birch trees from six stands were sampled at an elevation of about 1950m a.s.l. Correlation and response function coefficients indicated that radial growth of Erman's birch was positively influenced by previous August, October and current February temperature, and previous winter, and current March, June and September precipitation. In addition, radial growth showed a negative relationship to previous August and current June sunshine ratio. Precipitation and temperatures in annualization periods also positively affected the radial growth of Erman's birch. Regression analyses indicated that precipitation explained more variation in radial growth than minimum temperature. Together, these results suggested that climate affected radial growth of Erman's birch through altering soil water availability. Therefore, the radial growth of Erman's birch at the tree line in Changbai Mountain could not be predicted by temperature alone even under a scenario of global warming.
