The dendroclimatic signal in Douglas-fir and ponderosa pine tree-ring chronologies from the southern Canadian Cordillera

By E. Watson, B. Luckman. 2002

93 citations recorded by the source corpus.

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

View Paper: https://www.semanticscholar.org/paper/41e0652b41717927cc4cf5bea0d608d79a13da72

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. E. Hogg
2. M. Case
3. David L. Peterson

In Global and Planetary Change

1. E. Hogg
2. M. Case
3. David L. Peterson

In Nature and Landscape Conservation

1. M. Case
2. David L. Peterson

Citations in the corpus

• Factors affecting interannual variation in growth of western Canadian aspen forests during 1951-2000 (2005, background): “2002a, 2002b) and other tree species in the region (e.g., Case and MacDonald 1995; Watson and Luckman 2002; St. George and Nielsen 2002).”
• Variation in radial growth patterns of Pseudotsuga menziesii on the central coast of British Columbia, Canada (2004, background): “Dendroclimatic studies of Douglas-fir in the southern Canadian Cordillera (Watson and Luckman 2002) also showed that the radial growth of trees is most strongly related to water availability during the growing season months, and the precipitation signal is slightly weaker in the chronologies from…”
• Fine-scale variability in growth-climate relationships of Douglas-fir, North Cascade Range, Washington. (2005, background): “Similar results have been found between Douglas-fir and PDSI at other locations (Little et al. 1995; Watson and Luckman 2002; Nakawatase 2003).”