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The sensitivity of wet and dry tropical forests to climate change in Bolivia
Author(s) -
Seiler C.,
Hutjes R. W. A.,
Kruijt B.,
Hickler T.
Publication year - 2015
Publication title -
journal of geophysical research: biogeosciences
Language(s) - English
Resource type - Journals
eISSN - 2169-8961
pISSN - 2169-8953
DOI - 10.1002/2014jg002749
Subject(s) - environmental science , climate change , precipitation , water cycle , tropical and subtropical dry broadleaf forests , vegetation (pathology) , atmospheric sciences , primary production , canopy conductance , deforestation (computer science) , carbon cycle , carbon dioxide , ecosystem , dry season , climatology , transpiration , agroforestry , photosynthesis , ecology , vapour pressure deficit , geography , biology , botany , meteorology , geology , medicine , pathology , computer science , programming language
Bolivia's forests contribute to the global carbon and water cycle, as well as to global biodiversity. The survival of these forests may be at risk due to climate change. To explore the associated mechanisms and uncertainties, a regionally adapted dynamic vegetation model was implemented for the Bolivian case, and forced with two contrasting climate change projections. Changes in carbon stocks and fluxes were evaluated, factoring out the individual contributions of atmospheric carbon dioxide ([CO 2 ]), temperature, and precipitation. Impacts ranged from a strong increase to a severe loss of vegetation carbon ( c v ), depending on differences in climate projections, as well as the physiological response to rising [CO 2 ]. The loss of c v simulated for an extremely dry projection was primarily driven by a reduction in gross primary productivity, and secondarily by enhanced emissions from fires and autotrophic respiration. In the wet forest, less precipitation and higher temperatures equally reduced c v , while in the dry forest, the impact of precipitation was dominating. The temperature‐related reduction of c v was mainly due to a decrease in photosynthesis and only to lesser extent because of more autotrophic respiration and less stomatal conductance as a response to an increasing atmospheric evaporative demand. Under an extremely dry projection, tropical dry forests were simulated to virtually disappear, regardless of the potential fertilizing effect of rising [CO 2 ]. This suggests a higher risk for forest loss along the drier southern fringe of the Amazon if annual precipitation will decrease substantially.