Publication Search
Stoy, P. C., Katul, G. G., Siqueira, M. B., Juang, J., Novick, K. A., Uebelherr, J. M., Oren, R.
We measured net ecosystem CO2 exchange (NEE) using the eddy covariance (EC) technique for 4 years at adjoining old field (OF), planted pine (PP) and hardwood forest (HW) ecosystems in the Duke Forest, NC. To compute annual sums of NEE and its components – gross …
Journal: Agricultural And Forest Meteorology, Volume 141 (1): 2-18 (2006). DOI: 10.1016/j.agrformet.2006.09.001 Sites: US-Dk3
Misson, L., Gershenson, A., Tang, J., McKay, M., Cheng, W., Goldstein, A.
Journal: Tree Physiology, Volume 26 (7): 833-844 (2006). DOI: 10.1093/treephys/26.7.833 Sites: US-Blo
Law, B. E., Turner, D., Campbell, J., Lefsky, M., Guzy, M., Sun, O., Tuyl, S. V., Cohen, W.
Journal: Scaling And Uncertainty Analysis In Ecology, Volume : 167-190 (2006). DOI: 10.1007/1-4020-4663-4_9 Sites: US-Me2
Goulden, M. L., Winston, G. C., McMillan, A. M., Litvak, M. E., Read, E. L., Rocha, A. V., Rob Elliot, J.
We deployed a mesonet of year-round eddy covariance towers in boreal forest stands that last burned in ∼1850, ∼1930, 1964, 1981, 1989, 1998, and 2003 to understand how CO2 exchange and evapotranspiration change during secondary succession. We used MODIS imagery to establish that the tower sites were representative …
Journal: Global Change Biology, Volume 12 (11): 2146-2162 (2006). DOI: 10.1111/j.1365-2486.2006.01251.x Sites: CA-NS1, CA-NS2, CA-NS3, CA-NS5, CA-NS6, CA-NS7
Sacks, W. J., Schimel, D. S., Monson, R. K., Braswell, B. H.
Eddy covariance records hold great promise for understanding the processes controlling the net ecosystem exchange of CO2 (NEE). However, NEE is the small difference …
Journal: Global Change Biology, Volume 12 (2): 240-259 (2006). DOI: 10.1111/j.1365-2486.2005.01059.x Sites: US-NR1
Monson, R. K., Lipson, D. L., Burns, S. P., Turnipseed, A. A., Delany, A. C., Williams, M. W., Schmidt, S. K.
Most terrestrial carbon sequestration at mid-latitudes in the Northern Hemisphere occurs in seasonal, montane forest ecosystems1. Winter respiratory carbon dioxide losses from these ecosystems are high, and over half of the carbon assimilated by photosynthesis in the summer can be lost the following winter2,3. The amount of winter …
Journal: Nature, Volume 439 (7077): 711-714 (2006). DOI: 10.1038/nature04555 Sites: US-NR1
Scott, R. L., Huxman, T. E., Cable, W. L., Emmerich, W. E.
Key to evaluating the consequences of woody plant encroachment on water and carbon cycling in semiarid ecosystems is a mechanistic understanding of how biological and non-biological processes influence water loss to the atmosphere. To better understand how precipitation is partitioned into the components of evapotranspiration (bare-soil …
Journal: Hydrological Processes, Volume 20 (15): 3227-3243 (2006). DOI: 10.1002/hyp.6329 Sites: US-Whs
Staebler, R. M., Fitzjarrald, D. R.
A better understanding of forest subcanopy flows is needed to evaluate their role in the horizontal movement of scalars, particularly in complex terrain. This paper describes detailed measurements of the canopy structure and its variability in both the horizontal …
Journal: Journal Of Applied Meteorology, Volume 44 (8): 1161-1179 (2005). DOI: 10.1175/jam2265.1 Sites: US-Ha1
Wick, B., Veldkamp, E., Mello, W. Z. De, Keller, M., Crill, P.
Journal: Biogeosciences, Volume 2 (2): 175-187 (2005). DOI: 10.5194/bg-2-175-2005 Sites: BR-Sa1, BR-Sa3
Restrepo, N. C., Arain, M. A.
This paper summarizes the energy and water vapour fluxes for the first 14 months at a newly initiated flux tower site at a 65-year-old temperate conifer forest (Pinus strobus …
Journal: Hydrological Processes, Volume 19 (1): 27-49 (2005). DOI: 10.1002/hyp.5758 Sites: CA-TP1, CA-TP3, CA-TP4
