Related Experiment Video
Updated: Aug 15, 2025

06:27
Simulating Impacts of Ice Storms on Forest Ecosystems
Published on: June 30, 2020
7.1K
Amazon windthrow disturbances are likely to increase with storm frequency under global warming
Yanlei Feng1, Robinson I Negrón-Juárez2, David M Romps2,3
1Department of Geography, University of California, Berkeley, CA, USA. ylfeng@berkeley.edu.
Nature Communications
|January 7, 2023
Summary
Amazonian forests face increased windthrow risk due to severe convective storms. Our study links storm energy to tree mortality, projecting a significant rise in storm-prone areas and windthrow density by 2100 under high emissions.
Area of Science:
- Climatology and Tropical Ecology
- Earth System Science
Background:
- Convective storms (windthrow) are a major cause of forest mortality in the Amazon.
- The connection between atmospheric convective storms and surface-level windthrows is not well understood.
- Existing Earth system models (ESMs) do not mechanistically link convective wind events to tree mortality.
Purpose of the Study:
- To establish an empirical relationship between convective available potential energy and the spatial patterns of large windthrow events in the Amazon.
- To connect atmospheric storm dynamics with Amazonian forest dynamics.
- To project future changes in windthrow risk under climate change scenarios.
Main Methods:
- Developed an empirical relationship mapping convective available potential energy (simulated by ESMs) to windthrow patterns.
- Utilized climate model projections under the high-emission scenario (SSP 585).
Main Results:
- Identified a quantifiable link between convective storm energy and windthrow occurrence.
- Projected a 51% increase in areas prone to extreme storms in the Amazon by 2100.
- Projected a 43% increase in windthrow density within the Amazon by the end of the century.
Conclusions:
- Climate change is expected to intensify convective storms, increasing forest mortality via windthrow in the Amazon.
- These changes will significantly impact tropical forest composition and carbon cycle dynamics.
- The established relationship provides a crucial link for improving ESMs and understanding forest-climate interactions.
Related Concept Videos
Global Climate Change
24.6K
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.
24.6K
What is Weather?
18.4K
Overview
18.4K
Ecological Disturbance
17.4K
An ecological disturbance is a temporary disruption in the environment resulting from abiotic, biotic, or anthropogenic factors, causing a pronounced change in an ecosystem. The impact of an ecological disturbance, which can depend on its intensity, frequency, and spatial distribution, plays a significant role in shaping the species diversity within the ecosystem.
17.4K
What is Climate?
18.8K
Climate refers to the prevailing weather conditions in a specific area over an extended period. As the saying goes, “Climate is what you expect. Weather is what you get.” Climate is influenced by geographic factors, such as latitude, terrain, and proximity to bodies of water.
18.8K
Threats to Biodiversity
22.6K
There have been five major extinction events throughout geological history, resulting in the elimination of biodiversity, followed by a rebound of species that adapted to the new conditions. In the current geological epoch, the Holocene, there is a sixth extinction event in progress. This mass extinction has been attributed to human activities and is thus provisionally called the Anthropocene. In 2019 the human population reached 7.7 billion people and is projected to comprise 10 billion by...
22.6K
Variation of Atmospheric Pressure
2.7K
Change in atmospheric pressure with height is particularly interesting. The decrease in atmospheric pressure with increasing altitude is due to the decreasing gravitational force per unit area as we move away from the surface of the earth.
Assuming the air temperature is constant at a given altitude and that the ideal gas law of thermodynamics describes the atmosphere to a good approximation, one can find the variation of atmospheric pressure with height.
Let p(y) be the atmospheric pressure at...
Assuming the air temperature is constant at a given altitude and that the ideal gas law of thermodynamics describes the atmosphere to a good approximation, one can find the variation of atmospheric pressure with height.
Let p(y) be the atmospheric pressure at...
2.7K

