Modelling the glacial-interglacial changes in the continental biosphere

[en] A new estimate of the glacial-interglacial variations of the terrestrial carbon storage was obtained with the CARAIB biosphere model. The climatic data for the Last Glacial Maximum (LGM) necessary to drive the biosphere model are derived from results of the ECHAM2 General Circulation Model (GCM). Six model simulations (four under typical interglacial and two under typical glacial climatic conditions) were performed to analyse the roles of different environmental changes influencing the biospheric net primary productivity (NPP) and carbon stocks. The main differences between these simulations come from the adopted CO, levels in the atmosphere, the presence or absence of crops and from changing continental boundaries. The variation of the terrestrial carbon stocks since the LGM are estimated by comparing the pre-agricultural (280 ppm of CO2, no crops, modern climate) and the full glacial simulations (200 ppm of CO2, LGM climate reconstruction). Our model predicts a global NPP increase from 38 Gt C year(-1) to 53 Gt C year(-1) during the deglaciation, a substantial part of that change being due to CO, fertilization. At the same time, the terrestrial biosphere would have fixed between 134 (neglecting CO2 fertilization effects) and 606 Gt C. The treatment of both the C-3 and C-4 photosynthetic pathways in the CARAIB model enabled us further to reconstruct the partitioning between C, and C, plants. Following our experiments, 29.7% of the total biospheric carbon stock at the LGM was C-4 material, compared to an interglacial fraction of only 19.8%. The average biospheric fractionation factor was similar to 1.5 parts per thousand less negative at LGM than it is today. Considering an atmospheric delta(13)C 0.5 +/- 0.2 parts per thousand lower at LGM than at pre-industrial times, the 606 Gt C transfer would lead to a global ocean delta(13)C shift of roughly -0.41 parts per thousand, fully consistent with currently available data. For the smaller change of 134 Gt C obtained without the CO2 fertilization effect, this shift would only be on the order of -0.10 parts per thousand. (C) 1998 Elsevier Science B,V. All rights reserved.

Disciplines :

Earth sciences & physical geography
Physical, chemical, mathematical & earth Sciences: Multidisciplinary, general & others

Author, co-author :

François, Louis ; Université de Liège - ULiège > Département d'astrophys., géophysique et océanographie (AGO) > Modélisation du climat et des cycles biogéochimiques

Delire, Christine; Université de Liège - ULiège > LPAP

Warnant, Pierre ; Université de Liège - ULiège > Département d'astrophys., géophysique et océanographie (AGO) > Modélisation du climat et des cycles biogéochimiques

Munhoven, Guy ; Université de Liège - ULiège > Département d'astrophys., géophysique et océanographie (AGO) > Labo de physique atmosphérique et planétaire (LPAP) - Pétrologie et géochimie endogènes

Language :

English

Title :

Modelling the glacial-interglacial changes in the continental biosphere

Publication date :

1998

Journal title :

Global and Planetary Change

ISSN :

0921-8181

Publisher :

Elsevier Science, Amsterdam, Netherlands

Volume :

Pages :

37-52

Peer reviewed :

Peer Reviewed verified by ORBi

Available on ORBi :

since 13 May 2010

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Bibliography

Adams J.M., Faure H., Faure-Denard L., McGlade J.M., Woodward F.I. Increases in the terrestrial carbon storage from the Last Glacial Maximum to the present. Nature. 348:1990;711-714.
Amthor J.S. Terrestrial higher-plant response to increasing atmospheric [CO2] in relation to the global carbon cycle. Global Change Biol. 1:1995;243-274.
Ball, J.T., Woodrow, I.E., Berry, J.A., 1987. A model predicting stomatal conductance and its contribution to the control of photosynthesis under different environmental conditions. In: Biggins, J. (Ed.), Progress in Photosynthesis Research, Vol. 4, Nijhoff, Dordrecht, pp. 221-224.
Barnola J.-M., Raynaud D., Korotkevich Y.S., Lorius C. Vostok ice core provides 160 000-year record of atmospheric CO2. Nature. 329:1987;408-414.
Bird M.I., Lloyd J., Farquhar G.D. Terrestrial carbon storage at the LGM. Nature. 371:1994;566.
CLIMAP Project Members The surface of the ice-age earth. Science. 191:1976;1131-1137.
CLIMAP Project Members Seasonal reconstruction of the earth's surface at the Last Glacial Maximum. Geol. Soc. Am. Map Chart Ser. MC 36:1981.
Cogley, J.G., GGHYDRO - Global Hydrographic Data, Release 2.1. Trent Climate Note 91-1, Trent University, Department of Geography, Peterborough, Ontario, 1994.
Collatz G.J., Ribas-Carbo M., Berry J.A. Coupled photosynthesis - stomatal conductance model for leaves of C4 plants. Aust. J. Plant Physiol. 19:1992;519-538.
Crowley T.J. Ice age carbon. Nature. 352:1991;575-576.
Crowley T.J. Ice age terrestrial carbon changes revisited. Global Biogeochem. Cycles. 9(3):1995;377-389.
Delmas R.J., Ascencio J.-M., Legrand M. Polar ice evidence that atmospheric CO2 20 000 year BP was 50% of present. Nature. 284:1980;155-157.
Duplessy J.-C., Shackleton N.J., Fairbanks R.G., Labeyrie L., Oppo D., Kallel N. Deepwater source variations during the last climatic cycle and their impact on the global deepwater circulation. Paleoceanography. 3(3):1988;343-360.
Esser, G., 1991. Osnabrück Biosphere Model: structure, construction, results. In: Esser, G., Overdieck, D. (Eds.), Modern Ecology. Basic and Applied Aspects, Chap. 31, Elsevier, Amsterdam, pp. 679-709.
Esser G., Lautenschlager M. Estimating the change of carbon in the terrestrial biosphere from 18 000 bp to present using a carbon cycle model. Environ. Pollut. 83:1994;45-53.
FAO, (Food and Agricultural Organization of the United Nations) 1993. FAO Yearbook. Production 1992, FAO Statistics Series 112, Vol. 46, FAO, Rome, Italy.
Farquhar G.D., O'Leary M.H., Berry J.A. On the relationship between carbon isotope discrimination and the intercellular carbon dioxide concentration in leaves. Aust. J. Plant Physiol. 9:1982;121-137.
Farquhar G.D., von Caemmerer S., Berry J.A. A biogeochemical model of photosynthetic CO2 assimilation in leaves of C3 species. Planta. 149:1980;78-90.
Friedlingstein P., Delire C., Müller J.-F., Gérard J.-C. The climate-induced variation of the continental biosphere: a model simulation of the Last Glacial Maximum. Geophys. Res. Lett. 19(9):1992;897-900.
Gates, W.L., Nelson, A.B., 1975. A new (revised) tabulation of the Scripps topography on a 1 degree global grid. The Rand. R-1276-1-ARPA.
Guilderson T.P., Fairbanks R.G., Rubenstone J.L. Tropical temperature variations since 20 000 years ago: modulating interhemispheric climate change. Science. 263:1994;663-665.
Hubert, B., François, L.M., Warnant, P., Strivay, D., 1998. Stochastic generation of meteorological variables and effects on global models of water and carbon cycles in vegetation and soils. J. Hydrol., in press.
Hunt E.R. Jr., Piper S.C., Nemani R., Keeling C.D., Otto R.D., Running S.W. Global net carbon exchange and intra-annual atmospheric CO2 concentrations predicted by an ecosystem process model and three-dimensional atmospheric transport model. Global Biogeochem. Cycles. 10:1996;431-456.
Keeling, C.D., Bacastow, R.B., Carter, A.F., Piper, S.C., Whorf, T.P., Heimann, M., Mook, W.G., Roeloffzen, H., 1989. A three-dimensional model of atmospheric CO2 transport based on observed winds: 1. Analysis of observational data. In: Peterson, D.H. (Ed.), Aspects of Climate Variability in the Pacific and the Western Americas, Geophys. Monogr. Ser., Vol. 55, AGU, Washington, DC, pp. 165-236.
Korzoun, V.I., Sokolov, A.A., Budyko, M.I., Voskresensky, K.P., Kalinin, G.P., Konoplyantsev, A.A., Korotkevich, E.S., Lvovich, M.I. Atlas of World Water Balance. The UNESCO Press, Paris, 1977.
Lautenschlager M., Herterich K. Atmospheric response to ice age conditions: climatology near the Earth's surface. J. Geophys. Res. 95(D13):1990;22547-22557.
Leemans, R., Cramer, W.P., 1991. The IIASA database for mean monthly values of temperature, precipitation and cloudiness on a global terrestrial grid. IIASA-Report RR-91-18, International Institute for Applied Systems Analysis, Laxenburg, Austria.
Leuenberger M., Siegenthaler U., Langway C.C. Carbon isotope composition of atmospheric CO2 during the last ice age from an Antarctic ice core. Nature. 357:1992;488-490.
Munhoven, G., François, L.M., 1994. Glacial-interglacial changes in continental weathering: Possible implications for atmospheric CO2. In: Zahn, R., Pedersen, T.F., Kaminski, M.A., Labeyrie, L. (Eds.), Carbon Cycling in the Glacial Ocean: Constraints on the Ocean's Role in Global Change, NATO ASI Series I: Global Environmental Change, Vol. 17, Berlin, Springer-Verlag, pp. 39-58.
Munhoven G., François L.M. Glacial-interglacial variability of atmospheric CO2 due to changing continental silicate rock weathering: a model study. J. Geophys. Res. 101(D16):1996;21423-21437.
Neftel A., Oeschger H., Schwander J., Stauffer B., Zumbrunn R. Ice core samplements give atmospheric CO2 content during the past 40 000 year. Nature. 295:1982;220-223.
Nemry B., François L.M., Warnant P., Robinet F., Gérard J.-C. The seasonality of the CO2 exchange between the atmosphere and the land biosphere: a study with a global mechanistic model. J. Geophys. Res. 101:1996;7111-7125.
O'Leary, M.H., 1993. Biochemical basis of carbon isotope fractionation. In: Ehleringer, J.R., et al. (Eds.), Stable Isotopes and Plant Carbon-Water Relations. Academic Press, San Diego, CA, pp. 19-28.
Olson, J.S., Watts, J.A., Allison, L.J., 1985. Major world ecosystem complexes ranked by carbon in live vegetation: a database. CDIC Numeric Data Collection NDP-017, Oak Ridge National Laboratory, Oak Ridge, TN.
Prentice I.C., Sykes M.T., Lautenschlager M., Harrison S.P., Dennissenko O., Bartlein P.J. Modelling the global vegetation patterns and terrestrial carbon storage at the last glacial maximum. Global Ecol. Biogeorg. Lett. 3:1993;67-76.
Prentice K.C., Fung I.Y. The sensitivity of terrestrial carbon storage to climate change. Nature. 346:1990;48-51.
Raich J.W., Schlesinger W.H. The global carbon dioxide flux in soil respiration and its relationship to vegetation and climate. Tellus. 44B:1992;81-99.
Schimel, D., Enting, I.G., Heimann, M., Wigley, T.M.L., Raynaud, D., Alves, D., Siegenthaler, U., 1992. CO2 and the carbon cycle. In: Houghton, J.T., Meira Filho, L.G., Bruce, J., Lee, H., Chandler, B.A., Haites, E., Harris, N., Maskell, K. (Eds.), Climate Change 1994. Radiative Forcing of Climate Change and an Evaluation of the IPCC IS92 Emission Scenarios, Chap. 1. Cambridge Univ. Press, Cambridge, pp. 35-71.
Shackleton, N.J., 1977. Carbon-13 in Uvigerina: Tropical rainforest history and the Equatorial Pacific carbonate dissolution cycles. In: Andersen, N.R., Malahoff, A. (Eds.), The Fate of Fossil Fuel CO2 in the Oceans. Plenum Press, New York, NY, pp. 401-427.
Teeri J.A., Stowe L.G. Climatic patterns and the distribution of C4 grasses in North America. Oecologia. 23:1976;1-12.
Van Campo E., Guiot J., Peng C. A data-based re-appraisal of the terrestrial carbon budget at the Last Glacial Maximum. Global Planet Change. 8:1993;189-201.
Warnant P., François L.M., Strivay D., Gérard J.-C. CARAIB: a global model of terrestrial biological productivity. Global Biogeochem. Cycles. 8:1994;255-270.
Watson, R.T., Rohde, H., Oeschger, H., Siegenthaler, U., 1990. Greenhouse gases and aerosols. In: Houghton, J.T., Jenkins, G.J., Ephraums, J.J. (Eds.), Climate Change. The IPCC Scientific Assessment, Chap. 1. Cambridge Univ. Press, Cambridge, pp. 1-40.