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Andrej Varlagin

Researcher at Russian Academy of Sciences

Publications -  80
Citations -  6688

Andrej Varlagin is an academic researcher from Russian Academy of Sciences. The author has contributed to research in topics: Eddy covariance & Ecosystem respiration. The author has an hindex of 34, co-authored 76 publications receiving 4661 citations. Previous affiliations of Andrej Varlagin include Russian Academy.

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The FLUXNET2015 dataset and the ONEFlux processing pipeline for eddy covariance data

Gilberto Pastorello, +303 more
- 09 Jul 2020 - 
TL;DR: The FLUXNET2015 dataset provides ecosystem-scale data on CO 2 , water, and energy exchange between the biosphere and the atmosphere, and other meteorological and biological measurements, from 212 sites around the globe, and is detailed in this paper.
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A data-driven analysis of energy balance closure across FLUXNET research sites: The role of landscape-scale heterogeneity

TL;DR: In this article, the authors explored the relationship between energy balance closure and landscape heterogeneity using MODIS products and GLOBEstat elevation data and found that landscape-level heterogeneity in vegetation and topography cannot be ignored as a contributor to incomplete energy balance closures at the surface-atmosphere exchange measurements.
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Land management and land-cover change have impacts of similar magnitude on surface temperature

TL;DR: In this paper, the authors investigated the biophysical effects of temperate land-management changes and revealed a net warming effect of similar magnitude to that driven by changing land cover, and found that potential surface cooling from increased albedo is typically offset by warming from decreased sensible heat fluxes.
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Productivity of forests in the Eurosiberian boreal region and their potential to act as a carbon sink –- a synthesis

TL;DR: In this paper, carbon pools and fluxes of Siberian and European forests (600 and 300 million ha, respectively) were investigated based on review and original data, and the productivity of ecosystems, expressed as positive rate when the amount of carbon in the ecosystem increases, while (following micrometeorological convention) downward fluxes from the atmosphere to the vegetation (NEE) are expressed as negative numbers.