Knowledge of how water stress impacts the carbon and water cycles is a key uncertainty in terrestrial biosphere models. We tested a new profit maximization model, where photosynthetic uptake of CO2 is optimally traded against plant hydraulic function, as an alternative to the empirical functions commonly used in models to regulate gas exchange during periods of water stress. We conducted a multi-site evaluation of this model at the ecosystem scale, before and during major droughts in Europe. Additionally, we asked whether the maximum hydraulic conductance in the soil-plant continuum k(max) (a key model parameter which is not commonly measured) could be predicted from long-term site climate. Compared with a control model with an empirical so...
The current generation of dynamic global vegetation models (DGVMs) lacks a mechanistic representatio...
Soil moisture supply and atmospheric demand for water independently limit—and profoundly affect—vege...
This is the final version of the article. Available from the European Geosciences Union (EGU) via th...
- Knowledge of how water stress impacts the carbon and water cycles is a key uncertainty in terrestr...
Knowledge of how water stress impacts the carbon and water cycles is a key uncertainty in terrestria...
Terrestrial ecosystems are facing unprecedented threats from climate change. Projected increases in ...
Current land surface schemes in weather and climate models make use of the so-called coupled photosy...
The global carbon and water cycles are strongly governed by the simultaneous diffusion of CO2 and wa...
Predicting species-level responses to drought at the landscape scale is critical to reducing uncerta...
This is the final version. Available on open access from the Royal Society via the DOI in this recor...
Uncertainty in the representation of vegetation in Earth System Models is a major contributor to the...
Current land surface schemes in weather and climate models make use of the so-called coupled photosy...
Water stress is a defining characteristic of Mediterranean ecosystems, and is likely to become more ...
Climate change is expected to lead to increases in drought frequency and severity, with deleterious ...
Drought is predicted to increase in the future due to climate change, bringing with it myriad impact...
The current generation of dynamic global vegetation models (DGVMs) lacks a mechanistic representatio...
Soil moisture supply and atmospheric demand for water independently limit—and profoundly affect—vege...
This is the final version of the article. Available from the European Geosciences Union (EGU) via th...
- Knowledge of how water stress impacts the carbon and water cycles is a key uncertainty in terrestr...
Knowledge of how water stress impacts the carbon and water cycles is a key uncertainty in terrestria...
Terrestrial ecosystems are facing unprecedented threats from climate change. Projected increases in ...
Current land surface schemes in weather and climate models make use of the so-called coupled photosy...
The global carbon and water cycles are strongly governed by the simultaneous diffusion of CO2 and wa...
Predicting species-level responses to drought at the landscape scale is critical to reducing uncerta...
This is the final version. Available on open access from the Royal Society via the DOI in this recor...
Uncertainty in the representation of vegetation in Earth System Models is a major contributor to the...
Current land surface schemes in weather and climate models make use of the so-called coupled photosy...
Water stress is a defining characteristic of Mediterranean ecosystems, and is likely to become more ...
Climate change is expected to lead to increases in drought frequency and severity, with deleterious ...
Drought is predicted to increase in the future due to climate change, bringing with it myriad impact...
The current generation of dynamic global vegetation models (DGVMs) lacks a mechanistic representatio...
Soil moisture supply and atmospheric demand for water independently limit—and profoundly affect—vege...
This is the final version of the article. Available from the European Geosciences Union (EGU) via th...