Hostname: page-component-7bb8b95d7b-495rp Total loading time: 0 Render date: 2024-09-21T21:22:33.207Z Has data issue: false hasContentIssue false

Year-in-advance Forecasting of the Indian Monsoon Rainfall

Published online by Cambridge University Press:  24 August 2009

Reid A. Bryson
Affiliation:
Professor of Meteorology and Director, Institute for Environmental Studies, University of Wisconsin, Madison, Wisconsin 53706, U.S.A.
William H. Campbell
Affiliation:
Center for Climatic Research, Institute for Environmental Studies, University of Wisconsin, Madison, Wisconsin 53706, USA.

Extract

The paper starts out by discussing factors which influence the Indian monsoon rainfall—including Northern Hemispheric temperature changes, long-period soli–lunar tides, and the tidelike phenomena associated with the wobble of the Earth relative to its spin-axis. When the effects of these factors on precipitation are quantified and integrated into a thermodynamical–statistical model, long-range climatic forecasts can be made that are better than chance or than predicting ‘normal’ up to two or more years in advance.

Climatic changes have had profound effects on the peoples of India through the controlling influence of the monsoon on Indian agriculture. We now have a technological tool, never before available, that might lessen the impact of variations of the monsoon by forecasting these variations one to two years in advance. The two-years-in-advance 1982 monsoon rainfall forecast for June and July, using the same station models that produced the excellent 1981 forecast, indicates that there is a two-to-one chance that the 1982 Indian monsoon rainfall will be less, in general, in June and July, than it was in 1981. The question which we wish to ask the reader is: How can this new technology be used? For example, how can this type of information be used for planning and policy-making in order to ensure less uncertainty about food supplies in the future than in the past?

This region cannot depend upon the monsoon to bring plentiful rain every year, and, therefore, it is essential that we should continue to improve our forecasting capability and that others learn to make optimum use of these forecasts.

Type
Main Papers
Copyright
Copyright © Foundation for Environmental Conservation 1982

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

REFERENCES

Adderley, E. E. & Bowen, E. G. (1962). Lunar component in precipitation data. Science, 137, pp. 749–50.CrossRefGoogle ScholarPubMed
Brier, G. W. (1968). Long-range predictions of the zonal westerlies and some problems in data analysis. Rev. Geophys., 6, pp. 525–51.CrossRefGoogle Scholar
Brier, G. W. & Bradley, D. A. (1964). The lunar synodical period and precipitation in the United States. Journal of the Atmospheric Sciences, 21, pp. 386–95.2.0.CO;2>CrossRefGoogle Scholar
Bryson, R. A. (1948). On a lunar bi-fortnightly tide in the atmosphere. Trans. Am. Geophys. Union, 29, pp. 473–5.Google Scholar
Bryson, R. A. (1975). The lessons of climatic history. Environmental Conservation, 2(3), pp. 163–70, 8 figs.CrossRefGoogle Scholar
Bryson, R. A. & Dittberner, G. J. (1976). A non-equilibrium model of hemispheric mean surface temperature. Journal of the Atmospheric Sciences, 33, pp. 2094–106.2.0.CO;2>CrossRefGoogle Scholar
Bryson, R. A. & Goodman, B. M. (1980). Volcanic activity and climatic change. Science, 207, pp. 1041–4.CrossRefGoogle Scholar
Bryson, R. A., Irving, W. M. & Larson, J. A. (1965). Radiocarbon and soils evidence of former forest in the southern Canadian tundra. Science, 147, pp. 46–8.CrossRefGoogle ScholarPubMed
Bryson, R. A. & Starr, T. B. (1977). Chandler tides in the atmosphere. Journal of the Atmospheric Sciences, 34, pp. 1975–86.2.0.CO;2>CrossRefGoogle Scholar
Bryson, R. A. & Swain, A. M. (1981). Holocene variations of monsoon rainfall in Rajasthan. Quaternary Research, 16, pp. 135–45.CrossRefGoogle Scholar
Das, P. K. (1968). The Monsoon. National Book Trust, New Delhi, India: 162 pp., illustr.Google Scholar
Julian, P. R. & Chervin, R. M. (1978). A study of the Southern Oscillation and Walker Circulation phenomenon. Monthly Weather Review, 106, pp. 1433–51.2.0.CO;2>CrossRefGoogle Scholar
Kutzbach, J. E. (1981). Monsoon climate of the early Holocene: Climate experiment with the Earth's orbital parameters for 9000 years ago. Science, 214, pp. 5961.CrossRefGoogle ScholarPubMed
Maksimov, I. V. (1958). Nutational phenomena in the high latitude atmosphere and their role in the formation of climate. Nat. Res. Council of Canada, Ottawa, Problems of the North, No. 1 (1960), pp. 103–23.Google Scholar
Maksimov, I. V., Karklin, V. P., Sarukhanian, E. I. & Smirnov, N. P. (1967). Nutational migration of the Icelandic low. Dokl. Akad. Nauk SSSR, 177, pp. 8891. (English transl. Dokl. Acad. Sci. USSR, Earth Sci. Section.)Google Scholar
Parthasarathy, B. & Mooley, D. A. (1978). Some features of a long homogeneous series of Indian summer rainfall. Monthly Weather Review, 106, pp. 771–81.2.0.CO;2>CrossRefGoogle Scholar
Shukla, J. (1975). Effect of Arabian sea-surface temperature anomaly on Indian summer monsoon: A numerical experiment with the GFDL model. Journal of the Atmospheric Sciences, 32, pp. 503–11.2.0.CO;2>CrossRefGoogle Scholar
Shukla, J. & Misra, B. M. (1977). Relationship between sea surface temperature and wind speed over the central Arabian Sea, and monsoon rainfall over India. Monthly Weather Review, 105, pp. 9981002.2.0.CO;2>CrossRefGoogle Scholar
Sorenson, C. J., Knox, J. C., Larson, J. A. & Bryson, R. A. (1971). Paleosols and the forest border in Keewatin. Quaternary Research, 1, pp. 468–73.CrossRefGoogle Scholar
Visvanathan, T. R. (1966). Heavy rainfall distribution in relation to the phase of the moon. Indian Journal of Meteorology and Geophysics, 17, pp. 369–72.Google Scholar
[Sir]Walker, G. T. (1924). World Weather IX. Mem. Indian Meteor. Dept, 24, pp. 275332.Google Scholar
Weare, B. C. (1979). A statistical study of the relationships between ocean surface temperatures and the Indian monsoon. Journal of the Atmospheric Sciences, 36, 2279–91.2.0.CO;2>CrossRefGoogle Scholar
Webb, T. III & Bryson, R. A. (1972). The late- and postglacial sequence of climatic events in Wisconsin and eastcentral Minnesota: quantitative estimates derived from fossil pollen spectra by multivariate statistical analysis. Quaternary Research, 2, pp. 70115.CrossRefGoogle Scholar