Publication Search
Wieder, W. R., Knowles, J. F., Blanken, P. D., Swenson, S. C., Suding, K. N.
Journal: Journal Of Geophysical Research: Biogeosciences, Volume 122 (4): 825-845 (2017). DOI: 10.1002/2016JG003704 Sites: US-NR3, US-NR4
Miao, G., Noormets, A., Domec, J., Fuentes, M., Trettin, C. C., Sun, G., McNulty, S. G., King, J. S.
Journal: Agricultural And Forest Meteorology, Volume 247: 343-355 (2017). DOI: 10.1016/j.agrformet.2017.08.022 Sites: US-NC4
Lewczuk. N.A., Posse, G., Richter, K., Achkar, A.
The estimation of the GHG balance of agroecosystems is essential to evaluate the impact of agriculture on the composition of the atmosphere. Cultivated soils may act as a sink or a source of CO2 and usually emit N2O. The aim of the present study was to assess the CO2 and N2O balances, and to analyze the
relationships between N2O …
Journal: Soil And Tillage Research, Volume 169: 65-70 (2017). DOI: http://dx.doi.org/10.1016/j.still.2017.01.017 Sites: AR-CCa
Skubel, R. A., Khomik, M., Brodeur, J. J., Thorne, R., Arain, M. A.
Forest plantations are commonly used to restore the ecological and hydrological functionality of landscapes. In this study, we investigated the hydrologic response of a 74-year old pine plantation forest in southern Ontario, Canada to a selective thinning, wherein 30% of trees were harvested in winter of 2012. Tree-level and ecosystem-level …
Journal: Ecohydrology, Volume 10 (1): e1780 (2017). DOI: 10.1002/eco.1780 Sites: CA-TP3, CA-TP4
Sayres, D. S., Dobosy, R., Healy, C., Dumas, E., Kochendorfer, J., Munster, J., Wilkerson, J., Baker, B., Anderson, J. G.
The Arctic terrestrial and sub-sea permafrost region contains approximately 30 % of the global carbon stock, and therefore understanding Arctic methane emissions and how they might change with a changing climate is important for quantifying the global methane budget and understanding its growth in the atmosphere. Here we present …
Journal: Atmospheric Chemistry And Physics, Volume 17 (13): 8619-8633 (2017). DOI: https://doi.org/10.5194/acp-17-8619-2017 Sites: US-Fo1
Restrepo‐Coupe, N., Levine, N. M., Christoffersen, B. O., Albert, L. P., Wu, J., Costa, M. H., Galbraith, D., Imbuzeiro, H., Martins, G., da Araujo, A. C., Malhi, Y. S., Zeng, X., Moorcroft, P., Saleska, S. R.
To predict forest response to long-term climate change with high confidence requires that dynamic global vegetation models (DGVMs) be successfully tested against ecosystem response to short-term variations in environmental drivers, including regular seasonal patterns. Here, we used an integrated dataset from four forests in the Brasil …
Journal: Global Change Biology, Volume 23 (1): 191-208 (2017). DOI: https://doi.org/10.1111/gcb.13442 Sites: BR-Cax, BR-Ji3, BR-Ma2, BR-Sa1
Manoli, G., Domec, J.C., Novick, K.A., Oishi, A.C., Noormets, A., Marani, M., Katul, G.
Loblolly pine trees (Pinus taeda L.) occupy more than 20% of the forested area in the Southern United States, represent more than 50%of the standing pine volume in this region, and remove from the atmosphere about 500 g C m−2 per year through net ecosystem CO2 exchange. Hence, their significance as a major regional carbon sink …
Journal: Global Change Biology, Volume 000: 000-000 (2016). DOI: 10.1011 Sites: US-Dk3
Wehr, R., Munger, J. W., McManus, J. B., Nelson, D. D., Zahniser, M. S., Davidson, E. A., Wofsy, S. C., Saleska, S. R.
Terrestrial ecosystems currently offset one-quarter of anthropogenic carbon dioxide (CO2) emissions because of a slight imbalance between global terrestrial photosynthesis and respiration. Understanding what controls these two biological fluxes is therefore crucial to predicting climate change. Yet there is no way of directly measuring …
Journal: Nature, Volume 534: 680-683 (2016). DOI: 10.1038/nature17966 Sites: US-Ha1
Ma, S, Baldocchi, D.D., Wolf, S., Verfaillie, J.
Many ecophysiological and biogeochemical processes respond rapidly to changes in biotic and abiotic conditions, while ecosystem-level responses develop much more slowly (e.g., over months, seasons, years, or decades). To better understand the role of the slow responses in regulating interannual variability in NEE, we partitioned …
Journal: Agricultural and Forest Meteorology, Volume : 252-264 (2016). DOI: 10.1016/j.agrformet.2016.07.016 Sites: US-Ton, US-Var
Wang, J., X. M. Xiao, P. Wagle, S. Y. Ma, D. Baldocchi, A. Carrara, Y. Zhang, J. W. Dong, and Y. W. Qin.
Journal: Agricultural and Forest Meteorology, Volume 226: 132-147 (2016). DOI: dx.doi.org/10.1016/j.agrformet.2016.05.020 Sites: US-Ton
