Abstract
A global atmospheric model is used to calculate the monthly river flow for nine of the world's major high latitude rivers for the present climate and for a doubled CO2 climate. The model has a horizontal resolution of 4° × 5°, but the model's runoff from each grid box is quartered and added to the appropriate river drainage basin on a 2° × 2.5° resolution. A routing scheme is used to move runoff from a grid box to its neighboring downstream grid box and ultimately to the mouth of the river. In a model simulation in which atmospheric carbon dioxide is doubled, mean annual precipitation and river flow increase for all of these rivers, increased outflow at the river mouths begins earlier in the spring, and the maximum outflow occurs approximately one month sooner due to an earlier snow melt season. In the doubled CO2 climate, snow mass decreases for the Yukon and Mackenzie rivers in North America and for rivers in northwestern Asia, but snow mass increases for rivers in northeastern Asia.
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Ayers, M. A., Tasker, G. D., Wolak, D. M., McCabe, G. J., and Hay, L. E.: 1990, ‘Simulated Effects of Climatic Change on Runoff and Drought in the Delaware River Basin’,Annu. Civ. Eng. Conv. Expo., Published by ASCE, New York, NY, pp. 31–38.
Baumgartner, A. and Reichel, E.: 1975,The World Water Balance, Elsevier, Amsterdam.
Critchfield, H. J.: 1974,General Climatology, Prentice-Hall, Englewood Cliffs, New Jersey, 446 pp.
Flaschko, I., Stockton, C. W., and Boggess, W. R.: 1987, ‘Climate Variation and Surface Water Resources in the Great Basin Region’,Water Resourc. Bull. 23, 47–57.
Gates, W. L. and Nelson, A. B.: 1975,A New (Revised) Tabulation of the Scripps Topography on a 1° Global Grid. Part I, Terrain Heights, Rep. R-1276-1, Adv. Res. Proj. Agency, Rand Corporation, Santa Monica, California, 132 pp.
Gleick, P. H.: 1987, ‘Regional Hydrological Consequences of Increases in Atmospheric CO2 and Other Trace Gases’,Clim. Change 10, 137–160.
Hansen, J., Russell, G., Rind, D., Stone, P., Lacis, A., Lebedeff, S., Ruedy, R., and Travis, L.: 1983, ‘Efficient Three-Dimensional Global Models for Climate Studies: Models I and II’,Mon. Wea. Rev. 111, 609–662.
Hansen, J., Lacis, A., Rind, D., Russell, G., Stone, P., Fung, I., Ruedy, R., and Lerner, J.: 1984, ‘Climate Sensitivity: Analysis of Feedback Mechanisms’, in Hansen, J. E. and Takahashi, T. (eds.),Climate Processes and Climate Sensitivity, Geophys. Monogr. 29, pp. 130–163.
Korzoun, V. I., Sokolov, A. A., Budyko, M. I., Voskresensky, K. P., Kalinin, G. P., Konoplyantsev, A. A., Korotkevich, E. S., and Lovich, M. I. (eds.): 1977,Atlas of World Water Balance, U.S.S.R. National Committee for the International Hydrological Decade, UNESCO Press, Paris.
Kuhl, S. C. and Miller, J. R.: 1992, ‘Seasonal River Runoff Calculated from a Global Atmospheric Model’,Water Resourc. Res. 28, 2029–2039.
Legates, D. and Willmott, C.: 1990, ‘Mean Seasonal and Spatial Variability in Gauge-Corrected, Global Precipitation’,Int. J. Climatol. 10, 111–127.
Lettenmaier, D. P. and Gan, T. Y.: 1990, ‘Hydrologic Sensitivities of the Sacramento-San Joaquin River Basin, California, to Global Warming’,Water Resourc. 26, 69–86.
Manabe, S. and Stouffer, R. J.: 1980, ‘Sensitivity of a Global Climatic Model to an Increase of CO2 Concentration on the Atmosphere’,J. Geophys. Res. 85, 5529–5554.
Matthews, E.: 1983, ‘Global Vegetation and Land Use: New High-Resolution Data Bases for Climate Studies’,J. Clim. Appl. Meteorol. 22, 474–487.
Miller, J. R. and Russell, G. L.: 1992, ‘The Impact of Global Warming on River Runoff’,J. Geophys. Res. 97, 2757–2764.
Miller, J. R., Russell, G. L., and Caliri, G.: 1994, ‘Continental Scale River Flow in Climate Models’,J. Clim. 7, 914–928.
Milliman, J. D. and Meade, R. H.: 1983, ‘World-Wide Delivery of River Sediment to the Oceans’,J. Geol. 91, 1–21.
Mitchell, J. F. B.: 1989, ‘The “Greenhouse” Effect and Climate Change’,Rev. Geophys. 27, 115–139.
Nash, J. E. and Sutcliffe, J. V.: 1970, ‘River Flow Forecasting through Conceptual Models. Part I -A Discussion of Principles’,J. Hydrol. 10, 282–290.
Rind, D.: 1988, ‘The Doubled CO2 Climate and the Sensitivity of the Modeled Hydrologic Cycle’,J. Geophys. Res. 93, 5385–5412.
Roos, M.: 1989, ‘Possible Climate Change and Its Impact on Water Supply in California’,Oceans I, 247–249.
Russell, G. L. and Miller, J. R.: 1990, ‘Global River Runoff Calculated from a Global Atmospheric General Circulation Model’,J. Hydrol. 117, 241–254.
Stouffer, R. J., Manabe, S., and Bryan, K.: 1989, ‘Interhemispheric Asymmetry in Climate Response to a Gradual Increase of Atmospheric CO2’,Nature 342, 660–662.
Times Atlas of the World: 1967, Comprehensive Edition, 2nd ed., John Bartholomew and Son, Houghton Mifflin, Boston, Mass.
UNESCO: 1969, ‘Discharge of Selected Rivers of the World: Volume 1. General and Regime Characteristics of Stations Selected’, UNESCO, 7 Place de Fontenoy, Paris.
UNESCO: 1974, ‘Discharge of Selected Rivers of the World: Volume 3, Part 2. Mean Monthly and Extreme Discharges (1969–1972)’, UNESCO, 7 Place de Fontenoy, Paris.
UNESCO: 1985, ‘Discharge of Selected Rivers of the World: Volume 3, Part 4. Mean Monthly and Extreme Discharges (1976–1979)’, UNESCO, 7 Place de Fontenoy, Paris.
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Van Blarcum, S.C., Miller, J.R. & Russell, G.L. High latitude river runoff in a doubled CO2 climate. Climatic Change 30, 7–26 (1995). https://doi.org/10.1007/BF01093223
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DOI: https://doi.org/10.1007/BF01093223