Publication Search
Pancotto, V., Holl, D., Escobar, J., Castagnani, M. F., Kutzbach, L.
Journal: Biogeosciences, Volume 18 (16): 4817-4839 (2021). DOI: 10.5194/bg-18-4817-2021 Sites: AR-TF1
Hill, A. C., Vázquez-Lule, A., Vargas, R.
Salt marshes constitute an important terrestrial-aquatic interface that remains underrepresented in Earth System Models due to constraining biophysical controls and spatially limited land cover. One promising approach to improve representativeness is the application of proximal remote sensing to generate phenological information, …
Journal: Agricultural And Forest Meteorology, Volume 307: 108481 (2021). DOI: 10.1016/j.agrformet.2021.108481 Sites: US-StJ
Burns, S. P., Frank, J. M., Massman, W. J., Patton, E. G., Blanken, P. D.
Journal: Agricultural And Forest Meteorology, Volume 306: 108402 (2021). DOI: 10.1016/j.agrformet.2021.108402 Sites: US-GLE, US-NR1
Restrepo‐Coupe, N., Albert, L. P., Longo, M., Baker, I., Levine, N. M., Mercado, L. M., da Araujo, A. C., Christoffersen, B. O., Costa, M. H., Fitzjarrald, D. R., Galbraith, D., Imbuzeiro, H., Malhi, Y., von Randow, C., Zeng, X., Moorcroft, P., Saleska, S. R.
Tropical forests are an important part of global water and energy cycles, but the mechanisms that drive seasonality of their land-atmosphere exchanges have proven challenging to capture in models. Here, we (1) report the seasonality of fluxes of latent heat (LE), sensible heat (H), and outgoing short and longwave radiation at four …
Journal: Global Change Biology, Volume 27 (9): 1802-1819 (2021). DOI: https://doi.org/10.1111/gcb.15555 Sites: BR-Cax, BR-Ji3, BR-Ma2, BR-Sa1
Baldocchi, D., Ma, S., Verfaillie, J.
Journal: Global Change Biology, Volume 27 (2): 359-375 (2021). DOI: 10.1111/gcb.15414 Sites: US-Ton, US-Var
Acuña-Acosta, D. M., Castellanos-Villegas, A. E., Llano-Sotelo, J. M., Romo-León, J. R.
Background: Plants in drylands have developed several water use efficiency (WUE) adaptations, although nutrient limitations and excess irradiances affect also their performance. Previous findings of high photosynthetic rates and nitrogen concentration in leaves, may contradict the known low productivity in their communities.
Questions: …
Journal: Botanical Sciences, Volume 99 (2): 257-278 (2021). DOI: https://doi.org/10.17129/botsci.2708 Sites: MX-CHN
Vázquez-Lule, A., Vargas, R.
Salt marshes are large carbon reservoirs as part of blue carbon ecosystems. Unfortunately, there is limited information about the net ecosystem (NEE) and methane (CH4) exchange between salt marshes and the atmosphere to fully understand their carbon dynamics. We tested the influence of biophysical drivers by plant phenological phases …
Journal: Agricultural And Forest Meteorology, Volume 300: 108309 (2021). DOI: 10.1016/j.agrformet.2020.108309 Sites: US-StJ
Minick, K. J., Mitra, B., Li, X., Fischer, M., Aguilos, M., Prajapati, P., Noormets, A., King, J. S.
Coastal wetlands store significant amounts of carbon (C) belowground, which may be altered through effects of rising temperature and changing hydrology on CO2 and CH4 fluxes and related microbial activities. Wetland microtopography (hummock-hollow) also plays a critical role in mediating plant growth, microbial activity, and thus …
Journal: Geoderma, Volume 402: 115367 (2021). DOI: 10.1016/j.geoderma.2021.115367 Sites: US-NC4
McKenzie, S. M., Pisaric, M. F., Arain, M. A.
Forests play a major role in the global carbon cycle. Understanding the dynamics of the forest carbon cycle and its driving factors is challenging. This study utilized dendrochronology and long-term (2003 to 2017) eddy covariance (EC) carbon flux data to investigate the relationships between tree growth and gross and net ecosystem …
Journal: Trees, Volume 35 (2): 583-595 (2021). DOI: 10.1007/s00468-020-02061-z Sites: CA-TP1, CA-TP3, CA-TP4
Valach, A. C., Kasak, K., Hemes, K. S., Anthony, T. L., Dronova, I., Taddeo, S., Silver, W. L., Szutu, D., Verfaillie, J., Baldocchi, D. D.
Journal: Plos One, Volume 16 (3): e0248398 (2021). DOI: 10.1371/journal.pone.0248398 Sites: US-Myb, US-Sne, US-Tw1, US-Tw4
