2010
DOI: 10.1016/j.foreco.2009.09.003
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Analysis of potential impacts of climate change on forests of the United States Pacific Northwest

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Cited by 82 publications
(46 citation statements)
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“…However, this increase will not be uniform across elevations. Lower elevations will experience declines in productivity while an increase of productivity in many higher elevation forests partially offset those declines (Nakawatase & Peterson 2006;Latta et al 2010). For example, Douglas-fir is limited by high growing season temperatures and low growing season precipitation at low to mid elevations (495-1133m), but at high elevation (1036-1450m) current-year high temperatures lead to above-average growth (Case and Peterson 2005).…”
Section: Productivitymentioning
confidence: 99%
“…However, this increase will not be uniform across elevations. Lower elevations will experience declines in productivity while an increase of productivity in many higher elevation forests partially offset those declines (Nakawatase & Peterson 2006;Latta et al 2010). For example, Douglas-fir is limited by high growing season temperatures and low growing season precipitation at low to mid elevations (495-1133m), but at high elevation (1036-1450m) current-year high temperatures lead to above-average growth (Case and Peterson 2005).…”
Section: Productivitymentioning
confidence: 99%
“…Al respecto, estudios recientes muestran que las características climáticas influyen considerablemente sobre la productividad del bosque, donde las temperaturas juegan un papel importante en la generación de microambientes que aceleran la descomposición del material orgánico y la consecuente liberación de nutrientes; mientras que las relaciones entre la precipitación y las densidades de arbolado incrementan la disponibilidad de humedad en bosques secos (Deo, 2013;Raz-Yaseef et al, 2010;Karhu et al, 2010;Latta et al, 2010), como los de la región de estudio.…”
Section: Resultados Y Discusiónunclassified
“…Given that mean annual increment is related to temperature and moisture gradients within the Pacific Northwest (Latta et al, 2010), the presence of within region climate effects was not surprising, but the restriction of the intra-regional climate effects to the TSHEPISI and ABCOGR was unexpected. As the inclusion of intra-regional climate variables did not appear related to the broader climatic gradients represented by the vegetation zones (i.e., stronger effect in wet vs. dry or warm vs. wet vegetation zones), our results may indicate that other non-climatic factors are necessary to set the stage for intra-regional climatic controls.…”
Section: Discussionmentioning
confidence: 99%