Articles | Volume 16, issue 3
https://doi.org/10.5194/essd-16-1523-2024
https://doi.org/10.5194/essd-16-1523-2024
Data description paper
 | 
20 Mar 2024
Data description paper |  | 20 Mar 2024

Meteorological, snow and soil data, CO2, water and energy fluxes from a low-Arctic valley of Northern Quebec

Florent Domine, Denis Sarrazin, Daniel F. Nadeau, Georg Lackner, and Maria Belke-Brea

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Cited articles

Abramowitz, G.: Towards a benchmark for land surface models, Geophys. Res. Lett., 32, L22702, https://doi.org/10.1029/2005GL024419, 2005. 
Barrere, M., Domine, F., Decharme, B., Morin, S., Vionnet, V., and Lafaysse, M.: Evaluating the performance of coupled snow–soil models in SURFEXv8 to simulate the permafrost thermal regime at a high Arctic site, Geosci. Model Dev., 10, 3461–3479, https://doi.org/10.5194/gmd-10-3461-2017, 2017. 
Bhiry, N., Delwaide, A., Allard, M., Bégin, Y., Filion, L., Lavoie, M., Nozais, C., Payette, S., Pienitz, R., Saulnier-Talbot, E., and Vincent, W. F.: Environmental change in the Great Whale River region, Hudson Bay: Five decades of multidisciplinary research by Centre d'études nordiques (CEN), Écoscience, 18, 182–203, https://doi.org/10.2980/18-3-3469, 2011. 
Boisvert, L. N., Wu, D. L., Vihma, T., and Susskind, J.: Verification of air/surface humidity differences from AIRS and ERA- Interim in support of turbulent flux estimation in the Arctic, J. Geophys. Res.-Atmos., 120, 945–963, https://doi.org/10.1002/2014JD021666, 2015. 
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The forest–tundra ecotone is the transition region between the boreal forest and Arctic tundra. It spans over 13 000 km across the Arctic and is evolving rapidly because of climate change. We provide extensive data sets of two sites 850 m apart, one in tundra and one in forest in this ecotone for use in various models. Data include meteorological and flux data and unique snow and soil physics data.
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