Full references and selected summaries
(in alphabetical order of first author name by data set):
Chinese Forests NPP Data Set References
Gao, Q. and X.S. Zhang (1997) A simulation study of responses of the northeast China transect to elevated CO2 and climate change. Ecological Applications 7, 470-483.
Gao Q. and M. Yu (1998) A model of regional vegetation dynamics and its application to the study of Northeast China Transect (NECT) responses to global change. Global Biogeochemical Cycles 12, 329-344.
Gao, Q., M. Yu and X-S. Yang (2000) A simulation analysis of the relationship between regional primary production and vegetation structure under climatic change scenarios. Ecological Modelling 131, 33-45.
Ni, J. and X.S. Zhang. in press. Climate variability, ecological gradient and the Northeast China Transect (NECT). Journal of Arid Environments 46.
Ni, J. in press. Modeling vegetation distribution and net primary production along a precipitation gradient, the Northeast China Transect (NECT). Ekologia (Bratislava).
Ni, J., M.T. Sykes, I.C. Prentice and W. Cramer. in press. Modeling the vegetation of China using the process-based equilibrium terrestrial biosphere model BIOME3. Global Ecology and Biogeography 9.
Jiang, H., C-H. Peng, M.J. Apps, Y-L. Zhang, P.M. Woodard and Z-M. Wang. (1999) Modelling the net primary productivity of temperate forest ecosystems in China with a GAP model. Ecological Modelling 122, 225-238.
Jiang, H., M.J. Apps, Y-L. Zhang, C-H. Peng and P.M. Woodard (1999) Modelling the spatial pattern of net primary productivity in Chinese forests. Ecological Modelling 122, 275-288.
Fang, J.Y., G.G. Wang, G.H. Liu and S.L. Xu (1998) Forest biomass of China: an estimate based on the biomass-volume relationship. Ecological Applications 8, 1084-1091.
Feng Z.W., X.K. Wang and G. Wu (1999) Biomass and Primary Productivity of Forest Ecosystems in China. Science Press, Beijing. 241 pp. (in Chinese).
IBP Woodlands Data Set References
Burgess, R.L. (1981) Physiognomy and phytosociology of the international woodlands research sites. pp. 1-35. In: Reichle, D.E., ed. Dynamics of forest ecosystems. Cambridge University Press, Cambridge. 683 pp.
DeAngelis, D.L., R.H. Gardner, and H.H. Shugart (1981) Productivity of forest ecosystems studied during the IBP: the woodlands data set. pp. 567-672. In: Reichle, D.E., ed. Dynamics of forest ecosystems. Cambridge University Press, Cambridge. 683 pp.
Van Wijk, W.R., and D.W. Scholte Ubing (1966) Physics of Plant Environment, Ed. W. R. Van Wijk, Northern-Holland Publishing, Amsterdam.
Osnabruck NPP Data Set References
Cannell, M.G.R. (1982) World Forest Biomass and Primary Production Data. Academic Press, London. 391 pp.
Cramer, W., D.W. Kicklighter, A. Fischer, B. Moore, III, G. Churkina, A. Ruimy and A. Schloss (1997) Comparing global models of terrestrial net primary productivity (NPP): Overview and key results. Global Change Biology (forthcoming).
DeAngelis, D.L., R.H. Gardner, and H.H. Shugart (1981) Productivity of forest ecosystems studied during the IBP: the woodlands data set. pp. 567-672. In Reichle, D.E., (ed.) Dynamics of Forest Ecosystems. IBP 23. Cambridge University Press. 683 pp.
Esser, G., I. Aselman, and H.F.H. Lieth (1982) Modelling the carbon reservoir in the system compartment "litter". Mitt. Geol-Palaeontol., Inst. Univ. Hamburg, SCOPE/UNEP Sonderband, Heft 52, 39-58.
Esser, G. (1984) The significance of biospheric carbon pools and fluxes for atmospheric CO2: A proposed model structure. Progress in Biometeorology 3, 253-294.
Esser, G. (1986) The carbon budget of the biosphere - structure and preliminary results of the Osnabrück Biosphere Model. Veroff. Naturf. Ges. zu Emden von 1814 7:1-160. (in German with English summary)
Esser, G. (1987) Sensitivity of Global Carbon Pools and Fluxes to Human and Potential Climatic Impacts. Tellus 39B, 245-260.
Esser, G. and H. Lieth (1989) Productivity Modelling. In: Kitani, O. and C. W. Hall (eds.). Biomass Handbook, Chap. 1.1.3, pp. 36-48. Gordon & Breach, New York, London, Paris, Montreux, Tokyo, Melbourne.
Esser, G. (1990) Modelling Global Terrestrial Sources and Sinks of CO2 with Special Reference to Soil Organic Matter. In: Bouwman, A. F. (ed.). Soils and the Greenhouse Effect, Chap. 10. John Wiley & Sons, Chichester, New York, Brisbane, Toronto, Singapore.
Esser, G. (1991) Osnabrück Biosphere Model: structure, construction, results. In: Modern Ecology: basic and applied aspects (G. Esser and D. Overdieck, eds.). Elsevier, Amsterdam and London. pp. 679-709.
Esser, G. (1992) Implications of Climate Change for Production and Decomposition in Grasslands and Coniferous Forests. Ecological Applications 2, 47-54.
Esser, G., J. Hoffstadt, F. Mack, and U. Wittenberg (1994) High Resolution Biosphere Model, Documentation, Model Version 3.00.00. Mitteilungen aus dem Institut für Pflanzenökologie der Justus-Liebig-Universität Gießen, Heft 2:68 S.
Esser, G. and M. Lautenschlager. (1994). Estimating the Change Of Carbon in the Terrestrial Biosphere from 18000-BP to Present Using a Carbon-Cycle Model. Environmental Pollution 83, 45-53.
Summary
-
- The global High Resolution Biosphere Model (HRBM), which consists of a biome model and a carbon cycle model, was used to estimate the changes of carbon storage in the major pools of the terrestrial biosphere from 18 000 BP to the present. Climate change data to drive the biosphere for 18 000 BP were derived from an Atmospheric General Circulation Model (AGCM). The HRBM data base for the present climate was recalculated for 18 000 BP, using the AGCM anomalies interpolated to a 0.5-degree grid. Important processes influencing carbon storage included (1) climate-induced changes in biospheric processes and vegetation distribution, (2) the CO2 fertilization effect, (3) the inundation of lowland areas resulting from the sea level rise of 100 m. Two scenarios were investigated: the first, which ignored the CO2 fertilization effect, led to total carbon losses from the terrestrial biosphere of -460 x 10^9 t. The second scenario, which assumed that the model formulation of the CO2 fertilization effect as used for preindustrial to present could be extrapolated to the glacial 200 ppmv (parts per million volume), gave a carbon fixation in the terrestrial biosphere of +213 x 10^9 t. When compared with CO2 concentration data and isotopic ratios from air in ice cores, the results of Scenario 1 are not in agreement with the data. Scenario 2 gives realistic delta C-13 shifts in the atmosphere but the biospheric carbon storage at the end of the glacial period seems too large. It is suggested that the low atmospheric CO2 concentration may have favored the C-4 plants in ice age vegetation types. As a consequence the influence of the low CO2 concentration was eventually reduced and the glacial carbon storage in vegetation, litter, and soil was increased.
Foley, J.A. (1994) Net primary productivity in the terrestrial biosphere - the application of a global model. Journal of Geophysical Research - Atmospheres 99, 20773-20783.
Summary
- A process-based model of the terrestrial biosphere, DEMETER, was used to simulate global patterns of net primary productivity (NPP). NPP and vegetation biomass for the modern climate were simulated to be 62.1 Gt C per year and 800.6 Gt C, respectively. Simulated NPP was found to be highly correlated to field observations (r=0.9343) and to the results of the empirically based Miami model (r=0.9587).
Lieth, H.F.H. (1972) Modelling the primary productivity of the the world (10 pp., offset). Deciduous Forest Biome Memo Rep. 72-9.
Lieth, H.F.H. (1973) Primary production: terrestrial ecosystems. Human Ecology 1, 303-332.
Lieth, H.F.H. (1975) Modelling the primary productivity of the world. In: Lieth, H. and R.H. Whittaker (eds.), Primary Productivity of the Biosphere. Ecological Studies 14. Springer-Verlag, New York and Berlin. pp. 237-283.
Lieth, H.F.H., and E. Box (1972) Evapotranspiration and primary productivity: C.W. Thornthwaite Memorial Model. Publications in Climatology 25, 37-46. Centerton/Elmer, New Jersey.
Lieth, H.F.H., and G. Esser (1982) Modelling the relation between global net primary productivity and environmental factors [in German]. Unwellttress, Wiss. Beiträge 1982/1983 der Martin Luther Universität Wittenberg, Halle (Saale), pp. 303-321.
Lurin, B., W. Cramer, B. Moore III, and S.I. Rasool (1994) Global terrestrial net primary productivity. Global Change Newsletter, The International Geosphere-Biosphere Programme: A Study of Global Change (IGBP) of the International Council of Scientific Unions, No. 19, September 1994. pp 6-8.
McGuire, A.D., L.A. Joyce, D.W. Kicklighter, J.M. Melillo, G. Esser, and C.J. Vorosmarty (1993) Productivity response of climax temperate forests to elevated temperature and carbon dioxide - a North American comparison between two global models. Climatic Change 24, 287-310.
Summary
- Regression- and process-based approaches are assessed for predicting biogeochemical responses of ecosystems to global change. A regression-based model, the Osnabrück Model (OBM), and a process-based model, the Terrestrial Ecosystem Model (TEM), were applied to the historical range of temperate forests in North America in a factorial experiment with three levels of temperature (+0-deg-C, +2-deg-C, and +5-deg-C) and two levels Of CO2 (350 ppmv and 700 ppmv) at a spatial resolution of 0.5-deg latitude/longitude. For contemporary climate (+0-deg-C, 350 ppmv), OBM and TEM estimate the total net primary productivity (NPP) for temperate forests in North America to be 2.250 and 2.602 x 10^15 g C per year, respectively. Although the continental predictions for contemporary climate are similar, the responses of NPP to altered changes differ qualitatively; at +0-deg-C and 700 ppmv CO2, OBM and TEM predict median increases in NPP of 12.5% and 2.5%, respectively. The response of NPP to elevated temperature agrees most between the models in northern areas of moist temperate forest, but disagrees in southern areas and in regions of dry temperate forest - and the response to CO2 is qualitatively different between the models for all regions. These differences occur, in part, because TEM includes known feedbacks between temperature and ecosystem processes that affect N availability, photosynthesis, respiration, and soil moisture. Also, it may not be appropriate to extrapolate regression-based models for climatic conditions that are not now experienced by ecosystems. These results suggest that the process-based approach is able to progress beyond the limitations of the regression-based approach.
Nevison, C.D., G. Esser, and E.A. Holland (1996) A global model of changing N2O emissions from natural and perturbed soils. Climatic Change 32, 327-378.
Olson, R.J., J.M.O. Scurlock, R.S. Turner, and S.V. Jennings (1995) Ground-based grasslands data to support remote sensing and ecosystem modeling of terrestrial primary production. pp. 345-350. In: Guyot, G. (ed.) Proceedings of the International Colloquium on Photosynthesis and Remote Sensing. European Association of Remote Sensing Laboratories, Paris/ INRA, Avignon.
Olson, R.J., and S.D. Prince (1996) Global Primary Production Data Initiative update. Global Change Newsletter, The International Geosphere-Biosphere Programme: A Study of Global Change (IGBP) of the International Council of Scientific Unions, No. 27, September 1996. p 13.
Olson, R.J., J.M.O. Scurlock, W. Cramer, W.J. Parton, and S.D. Prince (1997) From Sparse Field Observations to a Consistent Global Data Set on Net Primary Production. IGBP-DIS Working Paper No. 16. International Geosphere-Biosphere Programme Data and Information System, Toulouse, France. 23 pp.
Prince, S.D., R.J. Olson, G. Dedieu, G. Esser, and W. Cramer (1995) Global Primary Production Data Initiative Project Description. IGBP-DIS Working Paper No. 12. International Geosphere-Biosphere Programme Data and Information System, Toulouse, France. 38 pp.
Whittaker, R.H., and P.L. Marks (1975) Methods of Assessing Terrestrial Productivity. In: Lieth, H., Whittaker, R.H. (eds.), Primary Productivity of the Biosphere. Ecological Studies 14. Springer-Verlag, New York and Berlin. pp. 55-118.
Wittenberg, U., and G. Esser (1997) Evaluation of the isotopic disequilibrium in the terrestrial biosphere by a global carbon isotope model. Tellus 49B, 263-269.
OTTER NPP Data Set References
Gholz, H.L. (1982) Environmental limits on aboveground net primary production, leaf area, and biomass
in vegetation zones of the Pacific northwest. Ecology 63, 469-481.
Goward, S.N, R.H. Waring, D.G. Dye and J. Yang (1994)
Ecological remote sensing at OTTER: satellite macroscale observations. Ecological Applications 4, 322-343.
Law, B.E. and R.H. Waring (1994) Combining remote-sensing and climatic data to estimate net primary
production across Oregon. Ecological Applications 4, 717-728.
Peterson, D.L. and R.H. Waring (1994) Overview of the Oregon transect ecosystem research project.
Ecological Applications 4, 211-225.
Pierce L.L., S.W. Running, and J. Walker (1994) Regional-scale relationships of leaf-area index
to specific leaf-area and leaf nitrogen-content. Ecological Applications 4, 313-321.
Spanner, M., L. Johnson, J. Miller, R. McCreight, J. Freemantle, J. Runyon and P. Gong (1994)
Remote sensing of seasonal leaf area index across the Oregon transect. Ecological Applications 4, 258-271.
Waring, R.H. and S.W. Running (1998) Forest Ecosystems: analysis at multiple scales.
Second edition, Academic Press, San Diego. 370 pp. with supplemental CD-ROM.
McGuire, A.D., J.M. Melillo, L.A. Joyce, D.W. Kicklighter, A.L. Grace, B. Moore III, and C.J. Vorosmarty (1992)
Interactions between carbon and nitrogen dynamics in estimating net primary productivity for potential vegetation
in North America. Global Biogeochemical Cycles 6, 101-124.
Melillo, J.M., A.D. McGuire, D.W. Kicklighter, B. Moore, C.J. Vorosmarty, and A.L. Schloss (1993)
Global climate-change and terrestrial net primary production. Nature 363, 234-240.
Pan, Y., A.D. McGuire, D.W. Kicklighter, and J.M. Melillo (1996) The importance of climate and soils for estimates
of net primary production: a sensitivity analysis with the terrestrial ecosystem model. Global Change Biology
2, 5-23.
Summary
Summary
Summary
Marshall, J.D., and R.H. Waring (1986) Comparison of methods of
estimating leaf-area index in old-growth Douglas-fir. Ecology 67, 975-979.
Summary
Summary
Summary
Runyon, J., R.H. Waring, S.N. Goward, and J.M. Welles (1994) Environmental limits on net primary production
and light-use efficiency across the Oregon transect. Ecological Applications 4, 226-237.
Summary
Summary
Terrestrial Ecosystem Model (TEM) NPP Data Set References
Summary
Summary
Summary