Air and Surface Temperatures Differently Drive Terrestrial Carbon and Water Cycles in the High Latitudes

Abstract High‐latitude vegetation experience different temperatures than the ambient air temperature. While lacking a regional plant temperature product, we drove the dynamic ecosystem model, LPJ‐GUESS, with widely used ERA5‐land surface temperature (T surf , at radiative equilibrium) and air temperature to understand ecosystem process responses to these two temperatures. We show that tundra plants' growth is stimulated by warmer T surf in the summer, but in the boreal forests, colder T surf in the non‐summer months constrains leaf development and enzyme activity the following growing season. T surf drives higher productivity of tundra plant individuals but leads to less productive individuals in the boreal forest, although with compensatory changes (almost 68%) in vegetation structure. We demonstrate the importance of forcing temperature in simulating high‐latitude ecosystem processes and call for a community effort to measure plant temperatures across canopy heights and seasons to reduce uncertainties in estimating high‐latitude plant responses and feedback to climate.

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Publication Details

Journal
Geophysical Research Letters
Published
2024-10-03
DOI
https://doi.org/10.1029/2024gl110652
Citations
4
Primary Topic
Atmospheric and Environmental Gas Dynamics
Type
article
Field-Weighted Citation Impact
1.13

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article

Air and Surface Temperatures Differently Drive Terrestrial Carbon and Water Cycles in the High Latitudes

David Martín Belda, Jing Tang, Yongshuo H. Fu, Riikka Rinnan et al.
4 citations
Geophysical Research Letters
Atmospheric and Environmental Gas Dynamics
1.13
article

Air and Surface Temperatures Differently Drive Terrestrial Carbon and Water Cycles in the High Latitudes

David Martín Belda, Jing Tang, Yongshuo H. Fu, Riikka Rinnan, Shouzhi Chen, Christian Körner
article en
4 citations

Abstract

Abstract High‐latitude vegetation experience different temperatures than the ambient air temperature. While lacking a regional plant temperature product, we drove the dynamic ecosystem model, LPJ‐GUESS, with widely used ERA5‐land surface temperature (T surf , at radiative equilibrium) and air temperature to understand ecosystem process responses to these two temperatures. We show that tundra plants' growth is stimulated by warmer T surf in the summer, but in the boreal forests, colder T surf in the non‐summer months constrains leaf development and enzyme activity the following growing season. T surf drives higher productivity of tundra plant individuals but leads to less productive individuals in the boreal forest, although with compensatory changes (almost 68%) in vegetation structure. We demonstrate the importance of forcing temperature in simulating high‐latitude ecosystem processes and call for a community effort to measure plant temperatures across canopy heights and seasons to reduce uncertainties in estimating high‐latitude plant responses and feedback to climate.

Geophysical Research LettersVol. 51(19)
Karlsruhe Institute of Technology (DE), University of Copenhagen (DK), University of Antwerp (BE), University of Basel (CH), Lund University (SE), Beijing Normal University (CN)
Villum Fonden, European Resuscitation Council, European Commission, National Research Foundation, Swedish Foundation for International Cooperation in Research and Higher Education, Danmarks Grundforskningsfond, National Natural Science Foundation of China, Svenska Forskningsrådet Formas, Lunds Universitet, Higher Education Discipline Innovation Project, International Cooperation and Exchange Programme, National Key Research and Development Program of China, National Science Fund for Distinguished Young Scholars, H2020 Marie Skłodowska-Curie Actions
Openalex Percentile: Top 23%
Atmospheric and Environmental Gas Dynamics
1.13
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