A year-long eddy covariance dataset over an Alpine Steppe on the central Tibetan Plateau: a landscape perspective on carbon and energy fluxes

Abstract. The Tibetan Plateau (TP) is warming rapidly, with future projections suggesting continued warming that may amplify climate–carbon feedbacks. However, sparse in-situ observations and pronounced spatial heterogeneity in vegetation, soil moisture, and climate have limited our understanding of these ecosystem responses. Here, we present a continuous record of carbon and energy fluxes measured at a landscape scale (∼30 ha (0.3 km2)) in an alpine steppe ecosystem on the TP from July 2018 to June 2019. The dataset yields a cumulative net ecosystem exchange (NEE) of -12.6±16.4 g C m−2, indicating a near carbon-neutral budget. Flux measurements were quality-filtered, retaining 33 %–44 % of high-quality data across fluxes, and gap-filled to produce a complete seasonal record using two complementary approaches, marginal distribution sampling (MDS) and random forest (RF), with RF outperforming MDS for all the fluxes. Eddy covariance measurements represent integrated fluxes over their footprint area, which are often much smaller than most model grids or remote sensing pixels, particularly in grassland ecosystems. Owing to the higher measurement height (19 m) at this site, the footprint climatology (90 % source area ≈ 280 000 m2) closely aligns with the spatial coverage of a Moderate Resolution Imaging Spectroradiometer (MODIS) 500 m pixel (∼250 000 m2), making this dataset particularly suitable for future landscape-scale comparisons and satellite product validation. The data include quality flags indicating observed or gap-filled values, uncertainty estimates, footprint diagnostics, and auxiliary meteorological variables (air and soil temperature, soil moisture, radiation, relative humidity, vapour pressure deficit). The data described in this manuscript provides a robust foundation for examining carbon–climate interactions in alpine environments and supporting ecosystem modeling (https://doi.org/10.5880/GFZ.TKVR.2026.001, Pillai et al., 2026).

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Publication Details

Journal
Earth system science data
Published
2026-07-30
DOI
https://doi.org/10.5194/essd-18-5627-2026
Primary Topic
Plant Water Relations and Carbon Dynamics
Type
article
Field-Weighted Citation Impact
0.00

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article

A year-long eddy covariance dataset over an Alpine Steppe on the central Tibetan Plateau: a landscape perspective on carbon and energy fluxes

Torsten Sachs, Felix Nieberding, Manuel Helbig, Nithin D. Pillai et al.
Earth system science data
Plant Water Relations and Carbon Dynamics
article

A year-long eddy covariance dataset over an Alpine Steppe on the central Tibetan Plateau: a landscape perspective on carbon and energy fluxes

Torsten Sachs, Felix Nieberding, Manuel Helbig, Nithin D. Pillai, Christian Wille
article en

Abstract

Abstract. The Tibetan Plateau (TP) is warming rapidly, with future projections suggesting continued warming that may amplify climate–carbon feedbacks. However, sparse in-situ observations and pronounced spatial heterogeneity in vegetation, soil moisture, and climate have limited our understanding of these ecosystem responses. Here, we present a continuous record of carbon and energy fluxes measured at a landscape scale (∼30 ha (0.3 km2)) in an alpine steppe ecosystem on the TP from July 2018 to June 2019. The dataset yields a cumulative net ecosystem exchange (NEE) of -12.6±16.4 g C m−2, indicating a near carbon-neutral budget. Flux measurements were quality-filtered, retaining 33 %–44 % of high-quality data across fluxes, and gap-filled to produce a complete seasonal record using two complementary approaches, marginal distribution sampling (MDS) and random forest (RF), with RF outperforming MDS for all the fluxes. Eddy covariance measurements represent integrated fluxes over their footprint area, which are often much smaller than most model grids or remote sensing pixels, particularly in grassland ecosystems. Owing to the higher measurement height (19 m) at this site, the footprint climatology (90 % source area ≈ 280 000 m2) closely aligns with the spatial coverage of a Moderate Resolution Imaging Spectroradiometer (MODIS) 500 m pixel (∼250 000 m2), making this dataset particularly suitable for future landscape-scale comparisons and satellite product validation. The data include quality flags indicating observed or gap-filled values, uncertainty estimates, footprint diagnostics, and auxiliary meteorological variables (air and soil temperature, soil moisture, radiation, relative humidity, vapour pressure deficit). The data described in this manuscript provides a robust foundation for examining carbon–climate interactions in alpine environments and supporting ecosystem modeling (https://doi.org/10.5880/GFZ.TKVR.2026.001, Pillai et al., 2026).

Earth system science dataVol. 18(7)
Dalhousie University (CA), Forschungszentrum Jülich (DE), Sphere Institute (US), GFZ Helmholtz Centre for Geosciences (DE), Technische Universität Braunschweig (DE)
Deutsche Forschungsgemeinschaft, German Academic Exchange Service New Delhi
Climate action
Openalex Percentile: Top 11%
Plant Water Relations and Carbon Dynamics
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