Reduced growth of Alaskan white spruce in the twentieth century from temperature-induced drought stress

By V. Barber, Glenn P. Juday, B. Finney. Nature, 2000

1,050 citations recorded by the source corpus.

Subfields: Atmospheric Science, Global and Planetary Change

View Paper: https://www.semanticscholar.org/paper/05c7c2234b6d7bdcdbbd93e27a8372d113ee5066

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

In Global and Planetary Change

Citations in the corpus

Satellite observations of high northern latitude vegetation productivity changes between 1982 and 2008: ecological variability and regional differences (2011, background): “Field measurements since the 1990s support these interpretations, showing increases in shrub growth in Alaskan tundra (Tape et al 2006), and historically low growth rates in black and white spruce trees in Alaskan boreal forests (Barber et al 2000, Beck et al 2011c).”
Response of plant pathogens and herbivores to a warming experiment (2004, background): “Drought stress in plants, for example, is expected to increase with warming (IPCC 1998, Barber et al. 2000).”
STRUCTURALLY NOVEL BIOMES: A RESPONSE TO PAST WARMING IN BERINGIA (2005, background): “Even if precipitation increases, warmer temperatures may lead to greater evapotranspiration and drier conditions for plant growth, especially in rain-shadow regions such as interior Alaska (Barber et al. 2000).”
Climate increases regional tree‐growth variability in Iberian pine forests (2007, background): “In this context, the intensification of warming in a longer term could lead to the elimination of droughtsusceptible trees (Barber et al., 2000) through stressrelated mortality (Wilmking et al.”
Massive mortality of aspen following severe drought along the southern edge of the Canadian boreal forest (2011, background): “To date, much of the global focus on drought impacts has focused on semiarid regions at low latitudes, but drought also poses a serious threat to high-latitude regions such as the boreal forests of Alaska, Canada, and Eurasia (Barber et al., 2000; Hogg & Bernier, 2005; Soja et al., 2007).”
Spruce beetles and forest ecosystems in south-central alaska : A review of 30 years of research (2006, background): “Boreal forests in much of interior and south-central Alaska have come under increasing stress because of a warming trend (Barber et al., 2000; ACIA, 2004) that has fueled outbreaks of forest insect pests and considerably altered forest ecosystems in the region (Werner, 1996).”
Bioclimatology of beech (Fagus sylvatica L.) in the Eastern Alps: spatial and altitudinal climatic signals identified through a tree‐ring network (2007, background): “In Alaska, recent increases in air temperature are not reflected in tree-ring thickness because water (that is, drought stress) has become the limiting factor (Barber et al., 2000; Lloyd & Fastie, 2002; Wilmking & Juday, 2005).”
Contribution of permafrost soils to the global carbon budget (2013, background): “Negative response of tree growth and increased forest mortality to warming and drought stress have already been reported for the past by Barber et al (2000), Wilmking et al (2004), Dulamsuren et al (2009), and Dulamsuren et al (2010).”
A mathematical analysis of the divergence problem in dendroclimatology (2009, background): “…Improvement, Inc. (NCASI), 552 South Washington Street, Suite 224, Naperville, IL 60540, USA e-mail: cloehle@ncasi.org as the divergence problem (Barber et al. 2000; Briffa 2000; Briffa et al. 1998a, b, 2004; Bungten et al. 2006; Carrer and Urbinati 2006; D’Arrigo et al. 2004, 2007; Driscoll et…”