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Publications Found: 1437

Land Surface Phenology Derived From Normalized Difference Vegetation Index (Ndvi) At Global Fluxnet Sites
Wu, C., Peng, D., Soudani, K., Siebicke, L., Gough, C. M., Arain, M. A., Bohrer, G., Lafleur, P. M., Peichl, M., Gonsamo, A., Xu, S., Fang, B., Ge, Q.

Journal: Agricultural And Forest Meteorology, Volume 233: 171-182 (2017). DOI: 10.1016/j.agrformet.2016.11.193 Sites: US-UMB

Chlorophyll Fluorescence Tracks Seasonal Variations Of Photosynthesis From Leaf To Canopy In A Temperate Forest
Yang, H., Yang, X., Zhang, Y., Heskel, M. A., Lu, X., Munger, J. W., Sun, S., Tang, J.

Journal: Global Change Biology, Volume 23 (7): 2874-2886 (2017). DOI: 10.1111/gcb.13590 Sites: US-Ha1

Co2 Exchange And Evapotranspiration Across Dryland Ecosystems Of Southwestern North America
Biederman, J. A., Scott, R. L., Bell, T. W., Bowling, D. R., Dore, S., Garatuza-Payan, J., Kolb, T. E., Krishnan, P., Krofcheck, D. J., Litvak, M. E., Maurer, G. E., Meyers, T. P., Oechel, W. C., Papuga, S. A., Ponce-Campos, G. E., Rodriguez, J. C., Smith, W. K., Vargas, R., Watts, C. J., Yepez, E. A., Goulden, M. L.

Journal: Global Change Biology, Volume 23 (10): 4204-4221 (2017). DOI: 10.1111/gcb.13686 Sites: US-Mpj, US-Seg, US-Ses, US-Vcm, US-Vcp, US-Wjs

CO2 And N2O Flux Balance On Soybean Fields During Growth And Fallow Periods In The Argentine Pampas—A Study Case
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

Evaluating The Effect Of Alternative Carbon Allocation Schemes In A Land Surface Model (Clm4.5) On Carbon Fluxes, Pools, And Turnover In Temperate Forests
Montané, F., Fox, A. M., Arellano, A. F., MacBean, N., Alexander, M. R., Dye, A., Bishop, D. A., Trouet, V., Babst, F., Hessl, A. E., Pederson, N., Blanken, P. D., Bohrer, G., Gough, C. M., Litvak, M. E., Novick, K. A., Phillips, R. P., Wood, J. D., Moore, D. J.

Journal: Geoscientific Model Development, Volume 10 (9): 3499-3517 (2017). DOI: 10.5194/gmd-10-3499-2017 Sites: US-MOz

Do Dynamic Global Vegetation Models Capture The Seasonality Of Carbon Fluxes In The Amazon Basin? A Data‐Model Intercomparison
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

Potential Bias Of Daily Soil Co2 Efflux Estimates Due To Sampling Time
Cueva, A., Bullock, S. H., López-Reyes, E., Vargas, R.

Soil respiration (Rs) has been usually measured during daylight hours using manual chambers. This approach assumes that measurements made during a typical time interval (e.g., 9 to 11 am) represent the mean daily value; locally, this may not always be correct and could result in systematic bias of daily and annual Rs budgets. We …

Journal: Scientific Reports, Volume 7 (1): (2017). DOI: 10.1038/s41598-017-11849-y Sites: MX-EMg

Direct And Indirect Climate Change Effects On Carbon Dioxide Fluxes In A Thawing Boreal Forest-Wetland Landscape
Helbig, M., Chasmer, L. E., Desai, A. R., Kljun, N., Quinton, W. L., Sonnentag, O.

In the sporadic permafrost zone of northwestern Canada, boreal forest carbon dioxide (CO2 ) fluxes will be altered directly by climate change through changing meteorological forcing and indirectly through changes in landscape functioning associated with thaw-induced collapse-scar bog (‘wetland’) expansion. However, their combined …

Journal: Global Change Biology, Volume 23 (8): 3231-3248 (2017). DOI: 10.1111/gcb.13638 Sites: CA-SCC

Multi-scale analyses of solar induced fluorescence and gross primary production
Wood, J.D., Griffis, T.J., Baker, J.M., Frankenberg, C., Verma, M., Yuen, K.

Journal: Geophysical Research Letters, Volume 44: 533-541 (2017). DOI: doi: 10.1002/2016GL070775 Sites: US-KCM

Short‐Term Selective Thinning Effects On Hydraulic Functionality Of A Temperate Pine Forest In Eastern Canada
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

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