Using simulation results from five GCMs and the full range of RCPs, we have characterized the range of
terrestrial vegetation responses to future conditions across seven different global vegetation model formulations.
Not exact matches
This study highlights the key role of
vegetation in controlling future
terrestrial hydrologic
response and emphasizes that the continental carbon and water cycles are intimately coupled over land and must be studied as an interconnected system.
«Our finding that
vegetation plays a key role future in
terrestrial hydrologic
response and water stress is of utmost importance to properly predict future dryness and water resources,» says Gentine, whose research focuses on the relationship between hydrology and atmospheric science, land / atmosphere interaction, and its impact on climate change.
Current research focusing on
terrestrial animals includes several studies on the island fox, one on the role of deer mice in affecting
vegetation community recovery, and one on the
response of lizards to the removal of rats on Anacapa.
Therefore, it is imperative that we are capable of anticipating the potential
responses of global
terrestrial vegetation to future changes in climate and atmospheric chemistry.
Here seven GVMs are used to investigate possible
responses of global natural
terrestrial vegetation to a major new set of future climate and atmospheric CO2 projections generated as part of the fifth phase of the Coupled Model Intercomparison Project (CMIP5)(6), the primary climate modeling contribution to the latest Intergovernmental Panel on Climate Change assessment.
Global
response of
terrestrial ecosystem structure and function to CO2 and climate change: results from six dynamic global
vegetation models.
Vegetation / ecosystem modelling and analysis project: comparing biogeography and biogeochemistry models in a continental - scale study of
terrestrial responses to climate change and CO2 doubling.
When done so, proxy records and climate models indicate that the
response to past global warming was profound, with evidence for global reorganisation of the hydrological cycle and profound local increases and decreases in rainfall; combined with elevated temperatures and
terrestrial vegetation change, this appears to often result in warming - enhanced soil organic matter oxidation, chemical weathering and nutrient cycling.