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Publications Found: 2

A Comparison Of Methods Reveals That Enhanced Diffusion Helps Explain Cold-Season Soil Co2 Efflux In A Lodgepole Pine Ecosystem
Rains, F. A., Stoy, P. C., Welch, C. M., Montagne, C., McGlynn, B. L.

Wintertime respiration contributes significantly to the annual loss of carbon from terrestrial ecosystems to the atmosphere, but the magnitude and physical transport mechanisms of this flux through snow remain unclear. Here, we quantify wintertime soil CO2 efflux in a Lodgepole pine (Pinus contorta Dougl.) forest by comparing chamber, …


Journal: Cold Regions Science And Technology, Volume 121: 16-24 (2016). DOI: 10.1016/j.coldregions.2015.10.003 Sites: US-TEF

Land–atmosphere carbon and water flux relationships to vapor pressure deficit, soil moisture, and stream flow
Mitchell, S.R., Emanuel, R.E., McGlynn, B.L.

Climatic change is exerting considerable influence on the hydrologic and biogeochemical cycles of snow dominated montane forest ecosystems. Growing season drought stress is a common occurrence after snowmelt-derived soil water content (WC) and stream flow (Q) have declined, leading to an increase in atmospheric water demand (i.e., …


Journal: Agricultural and Forest Meteorology, Volume 208: 108-117 (2015). DOI: 10.1016/j.agrformet.2015.04.003 Sites: US-TEF