Regionally strong feedbacks between the atmosphere and terrestrial biosphere
Julia K Green1, Alexandra G Konings1,2, Seyed Hamed Alemohammad1,3
1Department of Earth and Environmental Engineering, Columbia University, New York, NY.
Biosphere-atmosphere feedbacks are globally significant, influencing up to 30% of precipitation and radiation variance. These interactions, particularly strong in transitional climates, are underestimated by current Earth system models.
Area of Science:
- Earth System Science
- Ecology
- Atmospheric Science
Background:
- Terrestrial biosphere and atmosphere interact via feedback loops.
- Vegetation dynamics influence water and energy fluxes, affecting climate.
- Climate, in turn, regulates vegetation growth and phenology.
Purpose of the Study:
- Analyze satellite data to quantify biosphere-atmosphere feedbacks.
- Investigate the global extent and regional strength of these feedbacks.
- Identify climatic regions where these feedbacks are prominent.
Main Methods:
- Utilized satellite observations of solar-induced fluorescence, precipitation, and radiation.
- Employed a multivariate statistical technique for analysis.
- Compared findings with Earth system model simulations.
Main Results:
- Biosphere-atmosphere feedbacks are globally widespread and regionally strong, explaining up to 30% of precipitation and surface radiation variance.
- Strong feedbacks identified in transitional regions (semi-arid, monsoonal) and Mediterranean climates.
- Earth system models underestimate biosphere responses to radiation and water availability, thus underestimating feedbacks.
Conclusions:
- Biosphere-atmosphere feedbacks are crucial components of Earth's climate system.
- These feedbacks are concentrated in specific climatic zones, impacting the net CO2 balance.
- Accurate modeling of biosphere responses is essential for understanding climate dynamics.
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