Influence of topographic aspect, precipitation and drought on radial growth of four major tree species in an Appalachian watershed

By D. Fekedulegn, R. Hicks, J. J. Colbert. 2003

213 citations recorded by the source corpus.

Subfields: Atmospheric Science, Global and Planetary Change, Nature and Landscape Conservation

View Paper: https://www.semanticscholar.org/paper/5a881baf49fcd8f8d3f6f407702b21f4bf7fd383

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

In Atmospheric Science

1. P. Weber
2. A. Rigling
3. Harald Bugmann
4. D. Martin‐Benito
5. H. Adams
6. M. Río
7. N. Pederson
8. A. R. Pluess

In Global and Planetary Change

1. Harald Bugmann
2. P. Weber
3. A. Rigling
4. M. Río
5. Isabel Cañellas
6. D. Martin‐Benito
7. H. Adams
8. N. Pederson

In Nature and Landscape Conservation

1. P. Weber
2. A. Rigling
3. Harald Bugmann
4. M. Río
5. Isabel Cañellas
6. D. Martin‐Benito
7. H. Adams
8. Thomas E. Kolb

Citations in the corpus

• Growth response to climate and drought in Pinus nigra Arn. trees of different crown classes (2008, methodology): “Raw ring width values during drought years were compared to the years before and after the drought to quantitatively analyze growth decreases and recoveries (Fekedulegn et al. 2003).”
• Radial growth responses to drought of Pinus sylvestris and Quercus pubescens in an inner-Alpine dry valley (2007, background): “In a study by Fekedulegn et al. (2003) in the Appalachian mountains, the adaptive capacity to drought of individual Liriodendron tulipifera trees was interpreted as also depending on their root:shoot ratio, besides the species-specific growth strategy.”
• Drought response and changing mean sensitivity of European beech close to the dry distribution limit (2013, background): “In the pairs North of the Alps, the differences in topographic aspect may also play a role for the different growth responses at dry and mesic plots (Fekedulegn et al. 2003).”
• Convergence in drought stress, but a divergence of climatic drivers across a latitudinal gradient in a temperate broadleaf forest (2015, background): “Despite adaptations of Q. rubra to low resource availability (including drought) and its weaker response to climate than the other North American oaks (Fekedulegn et al., 2003; Speer et al., 2009), Q. rubra showed similar latitudinal trends in climate responses to other species in our network.”
• Tree growth response to drought and temperature in a mountain landscape in northern Arizona, USA (2005, methodology): “The ratio of RWI in wet years to dry years (W : D) was calculated by dividing the average RWI for the eight wet years by the average RWI for the eight dry years for each tree (Fekedulegn et al., 2003).”