Publication Search
Hayek, M. N., Longo, M., Wu, J., Smith, M. N., Restrepo-Coupe, N., Tapajós, R., da Silva, R., Fitzjarrald, D. R., Camargo, P. B., Hutyra, L. R., Alves, L. F., Daube, B., Munger, J. W., Wiedemann, K. T., Saleska, S. R., Wofsy, S. C.
In Amazon forests, the relative contributions of climate, phenology, and disturbance to net ecosystem exchange of carbon (NEE) are not well understood. To partition influences across various timescales, we use a statistical model to represent eddy-covariance-derived NEE in an evergreen eastern Amazon forest as a constant response …
Journal: Biogeosciences, Volume 15 (15): 4833-4848 (2018). DOI: https://doi.org/10.5194/bg-15-4833-2018 Sites: BR-Sa1
Besnard, S., Carvalhais, N., Arain, M. A., Black, A., de Bruin, S., Buchmann, N., Cescatti, A., Chen, J., Clevers, J. G., Desai, A. R., Gough, C. M., Havrankova, K., Herold, M., Hörtnagl, L., Jung, M., Knohl, A., Kruijt, B., Krupkova, L., Law, B. E., Lindroth, A., Noormets, A., Roupsard, O., Steinbrecher, R., Varlagin, A., Vincke, C., Reichstein, M.
Journal: Environmental Research Letters, Volume 13 (12): 124018 (2018). DOI: 10.1088/1748-9326/aaeaeb Sites: US-UMB
Rastogi, B., Berkelhammer, M., Wharton, S., Whelan, M. E., Meinzer, F. C., Noone, D., Still, C. J.
Carbonyl sulfide (OCS) has recently emerged as a tracer for terrestrial carbon uptake. While physiological studies relating OCS fluxes to leaf stomatal dynamics have been established at leaf and branch scales and incorporated into global carbon cycle models, the quantity of data from ecosystem-scale field studies remains limited. …
Journal: Biogeosciences, Volume 15 (23): 7127-7139 (2018). DOI: 10.5194/bg-15-7127-2018 Sites: US-Wrc
Berryman, E. M., Vanderhoof, M. K., Bradford, J. B., Hawbaker, T. J., Henne, P. D., Burns, S. P., Frank, J. M., Birdsey, R. A., Ryan, M. G.
Landscape carbon (C) flux estimates help assess the ability of terrestrial ecosystems to buffer further increases in anthropogenic carbon dioxide (CO2) emissions. Advances in remote sensing have led to coarse‐scale estimates of gross primary productivity (GPP; e.g., MODIS 17), yet efforts to develop spatial respiration products …
Journal: Journal Of Geophysical Research: Biogeosciences, Volume 123 (10): 3231-3249 (2018). DOI: 10.1029/2018JG004613 Sites: US-NR1
Besnard, S., Carvalhais, N., Arain, M. A., Black, A., de Bruin, S., Buchmann, N., Cescatti, A., Chen, J., Clevers, J. G., Desai, A. R., Gough, C. M., Havrankova, K., Herold, M., Hörtnagl, L., Jung, M., Knohl, A., Kruijt, B., Krupkova, L., Law, B. E., Lindroth, A., Noormets, A., Roupsard, O., Steinbrecher, R., Varlagin, A., Vincke, C., Reichstein, M.
Journal: Environmental Research Letters, Volume 13 (12): 124018 (2018). DOI: 10.1088/1748-9326/aaeaeb Sites: US-Syv, US-WCr
Knowles, J. F., Molotch, N. P., Trujillo, E., Litvak, M. E.
Journal: Geophysical Research Letters, Volume 45 (7): 3087-3096 (2018). DOI: 10.1002/2017GL076504 Sites: US-Vcm, US-Vcp
Chang, L., Dwivedi, R., Knowles, J. F., Fang, Y., Niu, G., Pelletier, J. D., Rasmussen, C., Durcik, M., Barron-Gafford, G. A., Meixner, T.
Most land surface models (LSMs) used in Earth System Models produce a lower ratio of transpiration (T) to evapotranspiration (ET) than field observations, degrading the credibility of Earth System Model-projected ecosystem responses and feedbacks to climate change. To interpret this model deficiency, we conducted a pair of model …
Journal: Journal Of Geophysical Research: Atmospheres, Volume 123 (17): 9109-9130 (2018). DOI: 10.1029/2018JD029159 Sites: US-MtB
Ouimette, A. P., Ollinger, S. V., Richardson, A. D., Hollinger, D. Y., Keenan, T. F., Lepine, L. C., Vadeboncoeur, M. A.
Journal: Agricultural And Forest Meteorology, Volume 256-257: 420-430 (2018). DOI: 10.1016/j.agrformet.2018.03.017 Sites: US-Bar
Sihi, D, Davidson, E.A., Chen, M, Savage, K.E., Richardson, A.D., Keenan, T.F., Hollinger, D. Y.
Heterotrophic respiration (Rh), microbial processing of soil organic matter to carbon dioxide (CO2), is a major, yet highly uncertain, carbon (C) flux from terrestrial systems to the atmosphere. Temperature sensitivity of Rh is often represented with a simple Q10 function in ecosystem models and earth system models (ESMs), sometimes …
Journal: Agricultural and Forest Meteorology, Volume 252: 155-166 (2018). DOI: https://doi.org/10.1016/j.agrformet.2018.01.026 Sites: US-Ha1, US-Ho1
Bond-Lamberty, B., Bailey, V. L., Chen, M., Gough, C. M., Vargas, R.
Journal: Nature, Volume 560 (7716): 80-83 (2018). DOI: 10.1038/s41586-018-0358-x Sites: US-UMB, US-UMd
