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Related Concept Videos

Global Climate Change01:50

Global Climate Change

Throughout its ~4.5 billion year history, the Earth has experienced periods of warming and cooling. However, the current drastic increase in global temperatures is well outside of the Earth’s cyclic norms, and evidence for human-caused global climate change is compelling. Paleoclimatology, the study of ancient climate conditions, provides ample evidence for human-caused global climate change by comparing recent conditions with those in the past.
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Exponential models are essential for describing rapid, multiplicative changes in natural systems, such as population growth. When a population doubles at regular intervals, the process can be modeled using a suitable base. For instance, a bacterial culture that doubles every three hours follows the model n(t)=n0⋅2t/3, where n(t) is the population at the time t.A more general model uses the natural base e, especially for continuous growth. This takes the form n(t)=n0⋅ert, where r is the relative...

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Development of an Individual-Tree Basal Area Increment Model using a Linear Mixed-Effects Approach
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Forecasting alpine vegetation change using repeat sampling and a novel modeling approach.

David R Johnson1, Diane Ebert-May, Patrick J Webber

  • 1Department of Biology, University of Texas at El Paso, 79968-0519, USA. drjohnson2@utep.edu

Ambio
|September 30, 2011
PubMed
Summary
This summary is machine-generated.

Alpine plant communities are shifting due to global change. This study forecasts a decrease in snowbed vegetation and an increase in shrub tundra over 100 years, driven by temperature and nitrogen deposition.

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Area of Science:

  • Ecology
  • Climate Change Research
  • Vegetation Dynamics

Background:

  • Global change significantly impacts alpine ecosystems, altering plant distributions and community composition.
  • Forecasting alpine vegetation change is difficult due to limited long-term studies on fixed plots.
  • Decadal-scale data is crucial for understanding and predicting shifts in alpine plant communities.

Purpose of the Study:

  • To develop and apply a probabilistic modeling approach to forecast alpine vegetation change.
  • To predict vegetation shifts on Niwot Ridge, Colorado, over a 100-year period.
  • To identify key environmental drivers influencing observed and predicted plant community changes.

Main Methods:

  • Utilized plant abundance data from marked plots established in 1971 and resurveyed in 1991 and 2001.
  • Employed a probabilistic modeling approach to extrapolate vegetation change from 1971 onwards for 100 years.
  • Correlated plant community trends with time-series environmental data from 1971-2001.

Main Results:

  • Models predict a significant decrease in the extent of Snowbed vegetation by 2071.
  • Models forecast an increase in the extent of Shrub Tundra by 2071.
  • Mean annual maximum temperature and nitrogen deposition were identified as primary correlates of plant community change.

Conclusions:

  • The probabilistic modeling approach provides valuable hypotheses for future alpine vegetation change.
  • Long-term monitoring data is essential for validating and refining vegetation change predictions.
  • Understanding the impact of climate change and nitrogen deposition is critical for alpine ecosystem management.