Carbon and Water Fluxes of the Boreal Evergreen Needleleaf Forest Biome Constrained by Assimilating Ecosystem Carbonyl Sulfide Flux Observations

Author:

Abadie Camille1ORCID,Maignan Fabienne1ORCID,Remaud Marine1,Kohonen Kukka‐Maaria23ORCID,Sun Wu4ORCID,Kooijmans Linda5,Vesala Timo26ORCID,Seibt Ulli7,Raoult Nina1ORCID,Bastrikov Vladislav1ORCID,Belviso Sauveur1ORCID,Peylin Philippe1

Affiliation:

1. Laboratoire des Sciences du Climat et de l’Environnement LSCE/IPSL CEA‐CNRS‐UVSQ Université Paris‐Saclay Gif‐sur‐Yvette France

2. Institute for Atmospheric and Earth System Research/Physics Faculty of Science University of Helsinki Helsinki Finland

3. Department of Environmental Systems Science Institute of Agricultural Sciences ETH Zurich Zurich Switzerland

4. Department of Global Ecology Carnegie Institution for Science Stanford CA USA

5. Meteorology and Air Quality Wageningen University and Research Centre Wageningen The Netherlands

6. Institute for Atmospheric and Earth System Research/Forest Sciences Faculty of Agriculture and Forestry University of Helsinki Helsinki Finland

7. Department of Atmospheric & Oceanic Sciences UCLA Los Angeles CA USA

Abstract

AbstractGross primary production (GPP) by boreal forests is highly sensitive to environmental changes. However, GPP simulated by land surface models (LSMs) remains highly uncertain due to the lack of direct photosynthesis observations at large scales. Carbonyl sulfide (COS) has emerged as a promising proxy to improve the representation of GPP in LSMs. Because COS is absorbed by vegetation following the same diffusion pathway as CO2 during photosynthesis and not emitted back to the atmosphere, incorporating a mechanistic representation of vegetation COS uptake in LSMs allows using COS observations to refine GPP representation. Here, we perform ecosystem COS flux and GPP data assimilations to constrain the COS‐ and GPP‐related parameters in the ORCHIDEE LSM for boreal evergreen needleleaf forests (BorENF). Assimilating ecosystem COS fluxes at Hyytiälä forest increases the simulated net ecosystem COS uptake by 14%. This increase largely results from changes in the internal conductance to COS, highlighting the need to improve the representation of COS internal diffusion and consumption. Moreover, joint assimilation of ecosystem COS flux and GPP at Hyytiälä improves the simulated latent heat flux, contrary to the GPP‐only data assimilation, which fails to do so. Finally, we scaled this assimilation framework up to the boreal region and find that the joint assimilation of COS at Hyytiälä and GPP fluxes at 10 BorENF sites increases the modeled vegetation COS uptake up to 18%, but not GPP. Therefore, this study encourages the use of COS flux observations to inform GPP and latent heat flux representations in LSMs.

Funder

HORIZON EUROPE Framework Programme

Helsingin Yliopisto

Publisher

American Geophysical Union (AGU)

Subject

Paleontology,Atmospheric Science,Soil Science,Water Science and Technology,Ecology,Aquatic Science,Forestry

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