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Climate Change in Grasslands, Shrublands, and Deserts of the Interior American West - A Review and Needs Assessment (Paperback)
Loot Price: R446
Discovery Miles 4 460
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Climate Change in Grasslands, Shrublands, and Deserts of the Interior American West - A Review and Needs Assessment (Paperback)
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Loot Price R446
Discovery Miles 4 460
Expected to ship within 10 - 15 working days
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Experimental research and species distribution modeling predict
that large changes in the distributions of species and vegetation
types will occur due to climate change. Species responses will
depend not only on their physiological tolerances but also on their
phenology, establishment properties, biotic interactions (Brown and
others 1997), and ability to evolve and migrate (Davis and Shaw
2001). The capacity of species and, thus, their distributions to
respond to a warming environment also will be affected by changing
disturbance regimes and other global change factors (Turner 2010).
Because individual species respond to climate variation and change
independently and differently, plant assemblages with no modern
analogs can be expected (Williams and Jackson 2007). New plant
assemblages might also arise in areas where novel climatic
conditions develop (Williams and Jackson 2007). Support for
predictions of novel climate regimes and corresponding plant
assemblages is found in studies examining relationships among
paleo-climate and plant community reconstructions. As Williams and
Jackson (2007) pointed out: (1) many past ecological communities
are compositionally unlike modern communities; (2) the formation
and dissolution of past "no-analog" communities appear to be
climatically driven and linked to climates without modern analogs;
(3) many future climate regimes will probably lack modern analogs;
and (4) novel communities and surprises should be expected in the
future. Novel climate conditions coupled with vegetation
communities that lack modern analogs pose significant challenges
for resource managers. Accurate predictions of how species
distributions will change under future warming are essential for
developing effective strategies for maintaining and restoring
sustainable ecosystems (Harris and others 2006). Several factors
make predicting how species distributions and vegetation
communities will change difficult. Global Circulation Models (GCMs)
exhibit significant variation in forecasts of future temperature
and especially precipitation (Christensen and others 2007). This
variation is often amplified for topographically variable areas
such as the Interior West (Rehfeldt 2006; Saenz-Romero and others
2010). In addition, information on species' relationships to
climate variables is often lacking and must be inferred from data
on current species distributions. And other factors such as
competitive interactions with other species and disturbance regimes
often obfuscate interpretation of species climate profiles in
projected future climate space. In grassland, shrubland, and desert
ecosystems, our understanding of likely changes in climate is
limited. Also, we lack information on the climate profiles of the
vast majority of species. Here, we provide (1) current forecasts
for changes in climate over the remainder of the century and (2)
available predictions for changes in regional vegetation types and
individual species distributions. We then discuss the types of
approaches that can be used to increase our predictive capacity and
the research needs for these ecosystems.
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