Biogeosciences www.biogeosciences.net 1726-4170 1726-4189 6 6 2009 10.5194/bg-6-969-2009 http://www.biogeosciences.net/6/969/2009/ http://www.biogeosciences.net/6/969/2009/bg-6-969-2009.html http://www.biogeosciences.net/6/969/2009/bg-6-969-2009.pdf 969 986 2009-06-12 Incorporation of crop phenology in Simple Biosphere Model (SiBcrop) to improve land-atmosphere carbon exchanges from croplands E. Lokupitiya erandi@atmos.colostate.edu S. Denning K. Paustian I. Baker K. Schaefer S. Verma T. Meyers C. J. Bernacchi A. Suyker M. Fischer Department of Atmospheric Science, Colorado State University, Fort Collins, CO 80523, USA Department of Soil and Crop Sciences, Colorado State University, Fort Collins, CO 80523, USA Natural Resource Ecology Laboratory, Colorado State University, Fort Collins, CO 80523, USA National Snow and Ice Data Center, University of Colorado, Boulder, CO 80309, USA School of Natural Resources, University of Nebraska-Lincoln, Lincoln, NE 68583-0978, USA NOAA/ARL/ATDD, Oak Ridge, TN 37830-2456, USA Department of Plant Biology, University of Illinois at Urbana-Champaign, Champaign, IL 61820, USA Lawrence Berkeley National Laboratory, Environmental Energy Technologies Division, Atmospheric Science Department, Berkeley, CA 94720, USA Croplands are man-made ecosystems that have high net primary productivity during the growing season of crops, thus impacting carbon and other exchanges with the atmosphere. These exchanges play a major role in nutrient cycling and climate change related issues. An accurate representation of crop phenology and physiology is important in land-atmosphere carbon models being used to predict these exchanges. To better estimate time-varying exchanges of carbon, water, and energy of croplands using the Simple Biosphere (SiB) model, we developed crop-specific phenology models and coupled them to SiB. The coupled SiB-phenology model (SiBcrop) replaces remotely-sensed NDVI information, on which SiB originally relied for deriving Leaf Area Index (LAI) and the fraction of Photosynthetically Active Radiation (fPAR) for estimating carbon dynamics. The use of the new phenology scheme within SiB substantially improved the prediction of LAI and carbon fluxes for maize, soybean, and wheat crops, as compared with the observed data at several AmeriFlux eddy covariance flux tower sites in the US mid continent region. 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