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T. Scott Rupp, Xi Chen, Mark Olson, and A. David McGuire

. 1992 ; Lamontagne et al. 2000 ; Schindler et al. 1980 ). A more frequent fire regime also has the potential to release carbon to the atmosphere from high-latitude soils that are rich in carbon ( McGuire et al. 2004 ). Therefore, it is important to couple ecological models of fire regime into climate models to better understand how future responses of the fire regime in high latitudes may influence hydrologic and trace gas feedbacks to the climate system. Global climate models (GCMs) agree that

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J. S. Kimball, K. C. McDonald, and M. Zhao

310 : 657 – 660 . Cihlar , J. , J. M. Chen , Z. Li , F. Huang , R. Latifovic , and R. Dixon . 1998 . Can interannual land surface signal be discerned in composite AVHRR data? J. Geophys. Res. 103D : 23163 – 23172 . Comiso , J. C. 2003 . Warming trends in the Arctic from clear sky satellite observations. J. Climate 16 : 3498 – 3510 . DeFries , R. S. , M. Hansen , J. R. G. Townshend , and R. Sohlberg . 1998 . Global land cover classifications at 8 km spatial

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J. S. Kimball, M. Zhao, A. D. McGuire, F. A. Heinsch, J. Clein, M. Calef, W. M. Jolly, S. Kang, S. E. Euskirchen, K. C. McDonald, and S. W. Running

nitrogen for terrestrial biomes ranging from individual plots to global scales. The model has been successfully applied over a range of diverse biomes, spatial scales, and climate regimes including boreal forests of Alaska and Canada ( Keyser et al. 2000 ; Kimball et al. 1997 ; Kimball et al. 2000 ; Amthor et al. 2001 ). Details of the model are presented elsewhere and include applications for multiple biome types and spatial scales (e.g., Thornton et al. 2002 ; White et al. 2000 ), while a

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