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Buy Topography- and species-dependent growth responses of Sabina przewalskii and Picea crassifolia to climate on the northeast Tibetan Plateau [An article from: Forest Ecology and Management] by E. Liang, X. Shao, D. Eckstein, L. Huang, X. Liu available and for sale on Brightsurf
| View Larger Image | Topography- and species-dependent growth responses of Sabina przewalskii and Picea crassifolia to climate on the northeast Tibetan Plateau [An article from: Forest Ecology and Management] by E. Liang, X. Shao, D. Eckstein, L. Huang, X. Liu
| | List Price: | $10.95 |  | | Available: | Available for download now |  | |  | | Studio: | Elsevier |  | | Binding: | Digital | | Publication Date: | December 01, 2006 | | Publisher: | Elsevier |
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EDITORIAL REVIEWS | Product Description This digital document is a journal article from Forest Ecology and Management, published by Elsevier in 2006. 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: Dendroecological techniques were used to examine the relationships between topographic aspects, climatic variation and radial growth of Qilian juniper (Sabina przewalskii Kom.) and Qinghai spruce (Picea crassifolia Kom.) on the northeast Tibetan Plateau. Both tree species exhibit a lower growth rate, a larger interannual growth variability and a higher percentage of missing rings on the west- than east-facing slopes. The two tree-ring chronologies of the west-facing slope are positively correlated with monthly precipitation and relative air humidity, but negatively correlated with monthly maximum temperature in prior July-September and current May-June, suggesting a severe limitation of moisture availability on tree growth. On both topographic aspects, the two tree species show a significant and positive correlation with winter temperature. In comparison, the two tree-ring chronologies of the east-facing slope are positively related to July temperature. Interspecific differences in climatic responses can only be seen by a different strength of the climatic signal. Overall, the biophysical setting is critical in determining the nature of growth responses to climate. This study might provide useful information for looking forward in ecological forecasting of where and how possible future climate change will affect subalpine forests on the northeast Tibetan Plateau. |
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