FP7Individual fellowship2009–2011

MTVEGMOD · Advancing dynamic vegetation modeling for mountain systems vulnerable to climate and land-use change

FP7 — People (Marie Curie Actions)

Duration
2009-07-01 → 2011-06-30
EU contribution
€180,629
Participants
1
Scheme
MC-IIF

Lines connect the coordinator with its partners.

Results in brief

Advancing dynamic vegetation modeling for mountain systems vulnerable to climate and land-use change

Project context and objectives Assessing the impact of climate change on terrestrial ecosystems is confronted with many challenges, including those associated with the handling of scale and complexity. Ecosystem models used to evaluate vegetation response to climate change consist of either locally applicable forest gap models or globally generalised dynamic global vegetation models (DGVM). At regional scales, assumptions from local and global models are not easily scalable and few studies exist to evaluate the consequences of scaling assumptions on ecosystem vulnerability to climate. Climate change is also a complex issue that involves not only changes to temperature and precipitation, but also changes to land use, disturbance and atmospheric chemistry, in particular, ozone formation. Here, we designed an experiment to evaluate the challenges for modelling climate impacts in mountain systems using the dynamic global vegetation model approach. Project methodology Three tasks were defined for the project duration: Task 1 was concerned with the development of regional-scale plant functional types, Task 2 concentrated on developing a new module to represent a regional global change driver (in this case, ozone); and Task 3 implemented a series of dynamic numerical simulations of climate change and interactions with local drivers on ecosystem biogeography and biogeochemistry. A proposal was submitted to the TRY Global Plant Traits database requesting data on shrub and grass species relevant to the Yunnan region of China, where the model simulations took place (Task 1). An ozone module was implemented to the Lund-Potsdam-Jena (LPJ) DGVM based on the concept that uptake of ozone is a function of stomatal conductance, and that damage to photosystems and productivity is related to ozone uptake (Task 2). A downscaling technique was applied to Fourth Assessment Report (AR4) models of the Intergovernmental Panel on Climate Change (IPCC) to provide 1 km resolution temperature, precipitation, and cloud-cover forcing (Task 3). Project results Most of the AR4 IPCC climate projections agree that both temperature and precipitation will increase. This suggests that vegetation will move toward higher elevations as well as becoming more productive in the mid-elevational belt, increasing the uptake of ozone and countering the effects of elevated CO2. Task 1 enabled us to access data for regional-model species fitting, but missing data for the shrubs of regional interest prevented detailed species parameterisation and we opted for a sensitivity-analysis approach. The ozone module was successfully implemented and calibrated with observations of ozone damage and productivity. In comparison to previous work with different models, LPJ produced consistent ozone-damage responses. Regional simulations with climate and ozone forcing produced upslope vegetation shifts and increases in productivity, but the effect of ozone on plant production was greatest in the midrange of species distributions (coinciding with the optimal growth conditions and highest stomatal conductance). Conclusion Our work illustrates that regional climate impacts can be assessed with global vegetation models that are updated to include forcings of local significance, whereas the parameterisation of regional species traits remains challenging. The downscaling of coarse-scale climate data to local scales is relatively well founded, but adaptation of model drivers to handle large file sizes, and parallel computer processing, is critical. The research developed here also suggests that monitoring of contemporary climate effects should expand from treeline sites to mid-range sites because these will be most sensitive to indirect global-change forcing, such as ozone. Complementary research is recommended to support databases of plant structure and environmental response.

Data: CORDIS, © European Union

Project objective

Significant uncertainties on the response of ecosystems to climate change remain to be addressed to advance the progress of the Intergovernmental Panel on Climate Change. We propose to investigate several of these uncertainties by improving regional-scale dynamic vegetation modeling for montane systems vulnerable to climate and land-use change. Our approach will modify a state-of-the-art dynamic global vegetation model (LPJ-DGVM) to include a new disturbance module for grazing, a key driver of alpine treeline dynamics. High-spatial resolution data for soils and climate (20th century and climate projections), essential for regional modeling, will be available from the Host institute and international collaborators based in the United States and China. The direct effects of grazing on seedling mortality and on light and water competition with grasses will be incorporated to the framework of LPJ. Model output, including net ecosystem exchange and species biogeography, will be evaluated for the Swiss Alps against databases from Swiss FluxNet, phenology observations from MeteoSwiss, and net primary productivity modeled from tree rings. Physiological parameters for plant functional types found in mountain habitat will be evaluated and adjusted following this assessment. The modified dynamic vegetation model, LPJ ‘Grazing’, will be applied with various climate scenarios to a biodiversity hotspot in the Hengduan Mountains in the Yunnan Province of China where little field-data exist and where the vulnerability to climate and land-use change is highly uncertain. The proposed research combines expertise and datasets of researchers from three continents to reduce uncertainties related to regional-scale climate attribution, impacts, and vulnerability. Our modifications to the LPJ-DGVM will have a significant impact globally for mountain biogeography and biogeochemical modeling because the model provides the basis for vegetation dynamics in many coupled global climate models.

Original text from CORDIS.

Participants

  • EIDGENOSSISCHE FORSCHUNGSANSTALT WSL · BirmensdorfCoordinatorSwitzerland

Links

Data: CORDIS, © European Union