Tropical Peatland Hydrology Simulated With a Global Land Surface Model.
S Apers1, G J M De Lannoy1, A J Baird2
1Department of Earth and Environmental Sciences KU Leuven Heverlee Belgium.
Summary
Tropical peatlands store significant carbon, but their unique hydrology is missing in global models. This study integrates tropical peat hydrology into a land surface model, improving carbon stock predictions.
Area of Science:
- Earth and Environmental Sciences
- Climate Science
- Ecosystem Modeling
Background:
- Tropical peatlands are critical carbon sinks, with water dynamics influencing carbon storage.
- Existing global land surface models (LSMs) do not accurately represent tropical peatland hydrology, which differs from northern peatlands.
Purpose of the Study:
- To integrate tropical peat-specific hydrology modules into a global LSM for the first time.
- To improve the representation of tropical peatland hydrological processes in Earth system models.
- To assess the model's performance against in situ data for natural and drained tropical peatlands.
Main Methods:
- Developed and integrated tropical peat-specific hydrology modules (PEATCLSM) into the NASA Catchment Land Surface Model (CLSM).
- Created literature-based parameter sets for natural (PEATCLSMTrop,Nat) and drained (PEATCLSMTrop,Drain) tropical peatlands.
- Forced simulations with global meteorological reanalysis data across major tropical peatland regions and evaluated against in situ water level and evapotranspiration data.
Main Results:
- The new model (PEATCLSMTrop,Nat) demonstrated improved bias and correlation compared to the default CLSM.
- PEATCLSMTrop,Drain significantly outperformed other model versions over drained peatland sites in Southeast Asia.
- Model performance varied across regions, suggesting the need to capture more nuanced peatland hydrologic responses.
Conclusions:
- Integrating tropical peat-specific hydrology into LSMs is crucial for accurately simulating these carbon-dense ecosystems.
- The developed model shows promise but requires further refinement to account for regional hydrological variations.
- Future work should focus on improving meteorological forcing data and incorporating more complex peatland hydrological processes.
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