Publication Search
Moran, M. S., Hamerlynck, E. P., Scott, R. L., Stone, J. J., Holifield Collins, C. D., Keefer, T. O., Bryant, R., DeYoung, L., Nearing, G. S., Sugg, Z., Hymer, D. C.
Observations of the temporal and spatial distribution of poststorm soil moisture in open shrublands and savannas are limited, yet they are critical to understanding the interaction and feedback between moisture distribution and canopies. The objective of this analysis was to study the hydrologic impacts of precipitation pulses on …
Journal: Water Resources Research, Volume 46 (W10509): n/a-n/a (2010). DOI: 10.1029/2009WR008842 Sites: US-Whs
Perez-Ruiz, E. R., Garatuza-Payan, J., Watts, C. J., Rodriguez, J. C., Yepez, E. A., Scott, R. L.
Journal: Journal Of Arid Environments, Volume 74 (5): 556-563 (2010). DOI: https://doi.org/10.1016/j.jaridenv.2009.09.029 Sites: MX-Tes
Iwata, H., Harazono, Y., and Ueyama, M.
Journal: Boundary Layer Meteorol., Volume 136: 391-405 (2010). DOI: Sites: US-Uaf
Griffis, T. J., Sargent, S. D., Lee, X., Baker, J. M., Greene, J., Erickson, M., Zhang, X., Billmark, K., Schultz, N., Xiao, W., Hu, N.
The oxygen isotope composition of evapotranspiration (δF) represents an important tracer in the study of biosphere–atmosphere interactions, hydrology, paleoclimate, and carbon cycling. Here, we demonstrate direct measurement of Journal: Boundary-Layer Meteorology, Volume 137 (2): 307-326 (2010). DOI: 10.1007/s10546-010-9529-5
Sites: US-Ro1Barr, J. G., Engel, V., Fuentes, J. D., Zieman, J. C., O'Halloran, T. L., Smith, T. J., Anderson, G. H.
We report on net ecosystem production (NEP) and key environmental controls on net ecosystem exchange (NEE) of carbon dioxide (CO2) between a mangrove forest and the atmosphere in the coastal Florida Everglades. An eddy covariance system deployed above the canopy was used to determine NEE during January 2004 through August …
Journal: Journal Of Geophysical Research: Biogeosciences, Volume 115 (G2): n/a-n/a (2010). DOI: 10.1029/2009JG001186 Sites: US-Skr
Miller, R. L., Fujii, R.
Wetland restoration can mitigate aerobic decomposition of subsided organic soils, as well as re-establish conditions favorable for carbon storage. Rates of carbon storage result from the balance of inputs and losses, both of which are affected by wetland …
Journal: Wetlands Ecology And Management, Volume 18 (1): 1-16 (2010). DOI: 10.1007/s11273-009-9143-9 Sites: US-Tw1
Ueyama, M., Harazono, Y., and Ichii, K. 2010.
Journal: Earth Interactions, Volume 14: 1-27 (2010). DOI: Sites:
Ryu, Y., Nilson, T., Kobayashi, H., Sonnentag, O., Law, B. E., Baldocchi, D. D.
Effective leaf area index is routinely quantified with optical instruments that measure gap fraction through the probability of beam penetration of sunlight through the vegetation. However, there have been few efforts to obtain theoretically consistent effective leaf area …
Journal: Agricultural And Forest Meteorology, Volume 150 (3): 463-472 (2010). DOI: 10.1016/j.agrformet.2010.01.009 Sites: US-Ton
Miller, G. R., Chen, X., Rubin, Y., Ma, S., Baldocchi, D. D.
Groundwater can serve as an important resource for woody vegetation in semiarid landscapes, particularly when soil water is functionally depleted and unavailable to plants. This study examines the uptake of groundwater by deciduous blue oak trees (Quercus douglasii) in a California oak savanna. Here we present a suite of …
Journal: Water Resources Research, Volume 46 (10): n/a-n/a (2010). DOI: 10.1029/2009wr008902 Sites: US-Ton
Smith, P., Lanigan, G., Kutsch, W. L., Buchmann, N., Eugster, W., Aubinet, M., Ceschia, E., Béziat, P., Yeluripati, J. B., Osborne, B., Moors, E. J., Brut, A., Wattenbach, M., Saunders, M., Jones, M.
There are a number of methods that can be used to help assess carbon budgets at the site to continental scales. Eddy covariance (EC) networks have been developed over the last decade and have been used to make many advances in our understanding. However, eddy covariance …
Journal: Agriculture, Ecosystems & Environment, Volume 139 (3): 302-315 (2010). DOI: 10.1016/j.agee.2010.04.004 Sites: BR-Ma2
