4.6 Article

Water stress limits transpiration and growth of European larch up to the lower subalpine belt in an inner-alpine dry valley

Journal

NEW PHYTOLOGIST
Volume 220, Issue 2, Pages 460-475

Publisher

WILEY
DOI: 10.1111/nph.15348

Keywords

climate change; dendrometer; elevation transect; radial stem variations; sap flow; tree ring width; tree water status

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Funding

  1. Austrian Federal Ministry of Science, Research and Economy
  2. project KLIMAGRO

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Climate change will further constrain water availability in dry inner-alpine environments and affect water relations and growth conditions in mountain forests, including the widespread larch forests. To estimate the effects of climate conditions on water balance and growth, variation in sap flow and stem radius of European larch was measured for 3yr along an elevation transect from 1070 to 2250m above sea level (asl) in an inner-alpine dry valley in South Tyrol/Italy. Additionally, long-term climate-growth relations were derived from tree cores. Sap flow and radial growth were reduced in dry periods up to an elevation of 1715m, leading to maximum annual growth at 2000m. In a wet year no growth difference between elevations was observed. Long-term tree ring data showed a positive growth response to precipitation up to 1715m and to temperature only above 2000m. Our results demonstrate that reduced water availability and higher atmospheric water demand limit larch at low elevation within dry Alpine regions. This indicates a general upward shift of this species' elevational amplitude upon climate change, and respective negative effects on future silvicultural use and ecosystem services at lower elevations in the European Alps.

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