The Role of Vegetation in the Dynamics of West African Monsoons

Xinyu Zheng Ralph M. Parsons Laboratory, Massachusetts Institute of Technology, Cambridge, Massachusetts

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Elfatih A. B. Eltahir Ralph M. Parsons Laboratory, Massachusetts Institute of Technology, Cambridge, Massachusetts

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Abstract

The focus of this paper is the role of meridional distribution of vegetation in the dynamics of monsoons and rainfall over West Africa. A moist zonally symmetric atmospheric model coupled with a simple land surface scheme is developed to investigate these processes. Four primary experiments have been carried out to examine the sensitivity of West African monsoons to perturbations in the meridional distribution of vegetation. In the control experiment, the authors assume a distribution of vegetation that resembles the natural vegetation cover in West Africa. Each perturbation experiment is identical to the control experiment except that a change in vegetation cover is imposed for a latitudinal belt that is 10° in width. The results of the numerical experiments demonstrate that West African monsoons and therefore rainfall distribution depend critically on the location of the vegetation perturbations. Changes in vegetation cover along the border between the Sahara desert and West Africa (desertification) may have a minor impact on the simulated monsoon circulation. However, coastal deforestation may cause the collapse of the monsoon circulation and have a dramatic impact on the regional rainfall. The observed deforestation in West Africa is then likely to be a significant contributor to the observed drought.

Corresponding author address: Dr. Elfatih A. B. Eltahir, Department of Civil and Environmental Engineering, Massachussets Institute of Technology, Cambridge, MA 02139.

Abstract

The focus of this paper is the role of meridional distribution of vegetation in the dynamics of monsoons and rainfall over West Africa. A moist zonally symmetric atmospheric model coupled with a simple land surface scheme is developed to investigate these processes. Four primary experiments have been carried out to examine the sensitivity of West African monsoons to perturbations in the meridional distribution of vegetation. In the control experiment, the authors assume a distribution of vegetation that resembles the natural vegetation cover in West Africa. Each perturbation experiment is identical to the control experiment except that a change in vegetation cover is imposed for a latitudinal belt that is 10° in width. The results of the numerical experiments demonstrate that West African monsoons and therefore rainfall distribution depend critically on the location of the vegetation perturbations. Changes in vegetation cover along the border between the Sahara desert and West Africa (desertification) may have a minor impact on the simulated monsoon circulation. However, coastal deforestation may cause the collapse of the monsoon circulation and have a dramatic impact on the regional rainfall. The observed deforestation in West Africa is then likely to be a significant contributor to the observed drought.

Corresponding author address: Dr. Elfatih A. B. Eltahir, Department of Civil and Environmental Engineering, Massachussets Institute of Technology, Cambridge, MA 02139.

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  • Budyko, M. I., 1974: Climate and Life. International Geophysical Series, Vol. 18, Academic Press, 508 pp.

  • Charney, J. G., 1975: Dynamics of desert and drought in the Sahel. Quart. J. Roy. Meteor. Soc.,101, 193–202.

  • ——, P. H. Stone, and W. J. Quirk, 1975: Drought in the Sahara: A biogeophysical feedback mechanism. Science,187, 434–435.

  • ——, W. J. Quirk, S.-H. Chow, and J. Kornfield, 1977: A comparative study of the effects of albedo change on drought in semi-arid regions. J. Atmos. Sci.,34, 1366–1385.

  • Chou, M. D., 1984: Broadband water vapor transmission functions for atmospheric IR flux computations. J. Atmos. Sci.,41, 1775–1778.

  • ——, and L. Peng, 1983: A parameterization of the absorption in the 15 μm CO2 spectral region with application to climate sensitivity studies. J. Atmos. Sci.,40, 2183–2192.

  • ——, D. P. Kratz, and W. Ridgway, 1991: Infrared radiation parameterizations in numerical climate models. J. Climate,4, 424–437.

  • Cunnington, C., and P. R. Rowntree, 1986: Simulations of the Saharan atmosphere-dependence on moisture and albedo. Quart. J. Roy. Meteor. Soc.,112, 971–999.

  • Dickinson, R. E., and P. Kennedy, 1992: Impacts on regional climate of Amazon deforestation. Geophys. Res. Lett.,19, 1947–1950.

  • Druyan, L. M., 1991: The sensitivity of sub-Saharan precipitation to Atlantic SST. Climate Change,18, 17–36.

  • Eltahir, E. A. B., 1992: Drought frequency analysis of annual rainfall series in central and western Sudan. Hydrol. Sci. J.,37, 185–199.

  • ——, 1996: The role of vegetation in sustaining large scale atmospheric circulations in the tropics. J. Geophys. Res.,101 (D2), 4255–4268.

  • ——, and C. Gong, 1996: Dynamics of wet and dry years in West Africa. J. Climate,9, 1030–1042.

  • Emanuel, K. A., 1991: A scheme for representing cumulus convection in large-scale models. J. Atmos. Sci.,48, 2313–2335.

  • ——, 1994: Atmospheric Convection. Oxford University Press, 580 pp.

  • ——, 1995: On thermally direct circulations in moist atmospheres. J. Atmos. Sci.,52, 1529–1534.

  • ——, J. D. Neelin, and C. S. Bretherton, 1994: On large-scale circulations in convecting atmospheres. Quart. J. Roy. Meteor. Soc.,120, 1111–1143.

  • Farmer, G., and T. M. L. Wigley, 1985: Climate trends for tropical Africa. Research Rep. for the Overseas Development Administration, 136 pp. [Available from Climate Research Unit, School of Environmental Sciences, University of East Anglia, Norwich NR4 7TJ, United Kingdom.].

  • Flohn, H., D. Henning, and H. C. Korff, 1965: Studies on the water-vapour transport over northern Africa. Bonner Meteor. Abh.,6..

  • Folland, C. K., T. N. Palmer, and D. E. Parker, 1986: Sahel rainfall and worldwide sea temperatures, 1901–85. Nature,320, 602–607.

  • Giorgi, F., M. R. Marinucci, and G. T. Bates, 1993a: Development of a Second-Generation Regional Climate Model (RegCM2). Part I: Boundary-layer and radiative transfer processes. Mon. Wea. Rev.,121, 2794–2813.

  • ——, ——, and ——, 1993b: Development of a Second-Generation Regional Climate Model (RegCM2). Part II: Convective processes and assimilation of lateral boundary conditions. Mon. Wea. Rev.,121, 2814–2832.

  • Goldenberg, S. B., and L. J. Shapiro, 1996: Physical mechanisms for the association of El Niño and West African rainfall with Atlantic major activity. J. Climate,9, 1169–1187.

  • Gong, C., and E. A. B. Eltahir, 1996: Sources of moisture for rainfall in West Africa. Water Resour. Res.,32, 3115–3121.

  • Gornitz, V., 1985: A survey of anthropogenic vegetation changes in West Africa during the last century. Climate Change,7, 285–325.

  • Gray, W. M., 1990: Strong association between West African rainfall and US landfall of intense hurricanes. Science,249, 1251–1256.

  • Gutman, G., G. Ohring, and J. H. Joseph, 1984: Interaction between the geobotanic state and climate: A suggested approach and a test with a zonal model. J. Atmos. Sci.,41, 2663–2678.

  • Held, I. M., and A. Y. Hou, 1980: Nonlinear axially symmetric circulations in a nearly inviscid atmosphere. J. Atmos. Sci.,37, 515–533.

  • Horton, E. B., and D. E. Parker, 1997: Global and regional climate in 1996. Weather,52, 174–182.

  • Huffman, G. J., R. F., Adler, B. Rudoff, U. Schneider, and P. R. Keehn, 1995: Global precipitation estimates based on a technique for combining satellite-based estimates, rain gauge analysis, and NWP model precipitation estimates. J. Climate,8, 1284–1295.

  • Hulme, M., 1994: Century-scale series of regional rainfall anomalies in Africa. Trends (93): A Compendium of Data on Global Change, T. A. Boden et al., Eds., Carbon-Dioxide Information Analysis Center, Oak Ridge National Laboratory, 964–973.

  • Janicot, S., 1992: Spatio-temporal variability of West African rainfall. Part I: Regionalizations and typings. J. Climate,5, 489–497.

  • Joseph, J. H., W. J. Wiscombe, and J. A. Weinman, 1976: The delta-Eddington approximation for radiative flux transfer. J. Atmos. Sci.,33, 2452–2459.

  • Kalnay, E., and Coauthors, 1996: The NCEP/NCAR 40-year reanalysis project. Bull. Amer. Meteor. Soc.,77, 437–471.

  • Kidson, J. W., 1977: African rainfall and its relation to the upper air circulation. Quart. J. Roy. Meteor. Soc.,103, 441–456.

  • King, M. D., and Harshvardhan, 1985: Comments on “The parameterization of radiation for numerical weather prediction and climate models.” Mon. Wea. Rev.,113, 1832–1833.

  • Kitoh, A., K. Yamzaki, and T. Takiota, 1988: Influence of soil moisture and surface albedo changes over African tropical rainforest on summer climate investigated with MRI-GCM-I. J. Meteor. Soc. Japan,66, 65–85.

  • Kutzbach, J., G. Bonan, J. Foley, and S. P. Harrison, 1996: Vegetation and soil feedbacks on the response of the African monsoon to orbital forcing in the early to middle Holocene. Nature,384, 623–626.

  • Lacis, A. A., and J. E. Hansen, 1974: A parameterization for the absorption of solar radiation in the earth’s atmosphere. J. Atmos. Sci.,31, 118–133.

  • Lamb, P. J., 1978a: Case studies of tropical Atlantic surface circulation patterns during recent sub-Saharan weather anomalies: 1967 and 1958. Mon. Wea. Rev.,106, 482–491.

  • ——, 1978b: Large-scale tropical Atlantic surface circulation patterns associated with sub-Saharan weather anomalies. Tellus,30, 240–251.

  • ——, 1983: West African water vapor variations between recent contrasting sub-Saharan rainy seasons. Tellus,35A, 198–212.

  • ——, and R. A. Peppler, 1992: Further case studies of tropical Atlantic surface atmospheric and oceanic patterns associated with sub-Saharan drought. J. Climate,5, 476–488.

  • Landsea, C. W., and W. M. Gray, 1992: The strong association between western Sahel monsoon rainfall and intense Atlantic hurricanes. J. Climate,5, 435–453.

  • ——, N. Nicholls, W. M. Gray, and L. A. Avila, 1996: Downward trends in the frequency of intense Atlantic hurricanes during the past five decades. Geophys. Res. Lett.,23, 1697–1700.

  • Lean, J., and P. R. Rowntree, 1993: A GCM simulation of the impact of Amazonian deforestation on climate using improved canopy representation. Quart. J. Roy. Meteor. Soc.,119, 509–530.

  • Lindzen, R. S., and A. Y. Hou, 1988: Hadley circulations for zonally averaged heating centered off the equator. J. Atmos. Sci.,45, 2416–2427.

  • Lough, J. M., 1986: Tropical sea surface temperature and rainfall variation in sub-Saharan Africa. Mon. Wea. Rev.,114, 561–570.

  • McClatchey, R. A., R. W. Fenn, J. E. A. Selby, F. E. Volz, and J. S. Garing, 1972: Optical properties of the atmosphere. Air Force Cambridge Research Laboratories Environmental Research Pap. 411.

  • Myers, N., 1991: Tropical forests: Present status and future outlook. Climate Change,19, 3–32.

  • Newell, R. E., J. W. Kidson, D. G. Vincent, and G. J. Boer, Eds., 1972a: The General Circulation of the Tropical Atmosphere. Vol. 1. The MIT Press, 258 pp.

  • ——, ——, ——, and ——, Eds., 1972b: The General Circulation of the Tropical Atmosphere. Vol. 2. The MIT Press, 371 pp.

  • Nicholson, S. E., 1988: Land surface atmosphere interaction. Prog. Phys. Geogr.,12, 36–65.

  • ——, 1994: Century-scale series of standardized annual departures of African rainfall. Trends (93): A Compendium of Data on Global Change, T. A. Boden et al., Eds., Carbon-Dioxide Information Analysis Center, Oak Ridge National Laboratory, 952–962.

  • ——, M. B. Ba, and J. Y. Kim, 1996: Rainfall in the Sahel during 1994. J. Climate,9, 1673–1676.

  • Nobre, C. A., P. J. Sellers, and J. Shukla, 1991: Amazonian deforestation and regional climatic change. J. Climate,4, 957–988.

  • Owen, J. A., and M. N. Ward, 1989: Forecasting Sahel rainfall. Weather,44, 57–64.

  • Plumb, R. A., and A. Y. Hou, 1992: The response of a zonally symmetric atmosphere to subtropical thermal forcing: Threshold behavior. J. Atmos. Sci.,49, 1790–1799.

  • Ramage, C. S., 1971: Monsoon Meteorology. Academic Press, 296 pp.

  • Rasmusson, E. M., 1972: Seasonal variation of the tropical humidity parameters. The General Circulation of the Tropical Atmosphere, Vol. 1, R. E. Newell et al., Eds., The MIT Press, 193–221.

  • Renno, N. O., 1992: Moist convection parameterization and numerical modelling of moist atmospheres. Ph.D. thesis, Massachusetts Institute of Technology, 297 pp. [Available from Massachusetts Institute of Technology, 77 Massachusetts Ave., Cambridge, MA 02139.].

  • Reynolds, R. W., and T. M. Smith, 1994: Improved global sea surface temperature analyses. J. Climate,7, 929–948.

  • Rodgers, C. D., 1968: Some extension and applications of the new random model for molecular band transmission. Quart. J. Roy. Meteor. Soc.,94, 99–102.

  • Rodriguez-Iturbe, I., D. Entekhabi, and R. L. Bras, 1991: Nonlinear dynamics of soil moisture at climate scales: 1. Stochastic analysis. Water Resour. Res.,27, 1899–1906.

  • Rodwell, M. J., and B. J. Hoskins, 1996: Monsoons and the dynamics of deserts. Quart. J. Roy. Meteor. Soc.,122, 1385–1404.

  • Rowell, D. P., and C. Blondin, 1990: The influence of soil wetness distribution on short range rainfall forecasting in the West African Sahel. Quart. J. Roy. Meteor. Soc.,116, 1471–1485.

  • Shinoda, M., 1990: Long-term variability of the tropical African rainbelt and its relation to rainfall in the Sahel and northern Kalahari. J. Meteor. Soc. Japan,68, 19–35.

  • Sud, Y. C., and M. J. Fennessy, 1984: Influence of evaporation in semi-arid regions on the July circulation: A numerical study. J. Climatol.,4, 383–398.

  • ——, and A. Molod, 1988: A GCM simulation study of the influence of Saharan evapotranspiration and surface albedo anomalies on July circulation and rainfall. Mon. Wea. Rev.,116, 2388–2400.

  • Walker, J., and P. R. Rowntree, 1977: The effect of soil moisture on circulation and rainfall in a tropical model. Quart. J. Roy. Meteor. Soc.,103, 29–46.

  • Webster, P. J., and L. C. Chou, 1980: Seasonal structure of a simple monsoon system. J. Atmos. Sci.,37, 354–367.

  • Xue, Y., and J. Shukla, 1993: The influence of land surface properties on Sahel climate. Part I: Desertification. J. Climate,6, 2232–2245.

  • ——, K. N. Liou, and A. Kasahara, 1990: Investigation of biogeophysical feedback on the African climate using a two-dimensional model. J. Climate,3, 337–352.

  • Yeh, T.-C., R. T. Wetherald, and S. Manabe, 1984: The effect of soil moisture on the short-term climate and hydrology change—A numerical experiment. Mon. Wea. Rev.,112, 474–490.

  • Zheng, X., 1997: Moist zonally-symmetric models and their applications to West African monsoons. Ph.D. thesis, Massachusetts Institute of Technology, 217 pp. [Available from Massachusetts Institute of Technology, 77 Massachusetts Ave., Cambridge, MA 02139.].

  • ——, and E. Eltahir, 1997: The response to deforestation and desertification in a model of West African monsoons. Geophys. Res. Lett.,24, 155–158.

  • ——, and ——, 1998: A soil moisture–rainfall feedback mechanism:2. Numerical experiments. Water Resour. Res.,34, 777–785.

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