Hostname: page-component-cd9895bd7-fscjk Total loading time: 0 Render date: 2024-12-18T18:08:52.355Z Has data issue: false hasContentIssue false

The use of long-term rainfall records for augmenting historic flood series: a case study on the upper Dee, Aberdeenshire, Scotland

Published online by Cambridge University Press:  03 November 2011

L. J. McEwen
Affiliation:
The Department of Geography, The University, St Andrews, Fife KY16 9AL, Scotland, U.K.

Abstract

Establishing the magnitude and frequency of floods within upland catchments on the basis of short-term gauged runoff records is crucially dependent upon the extent to which the record is truly representative. In the case of the River Dee, upstream of Crathie in Aberdeenshire, gauged discharge records are limited in length. Although the middle Dee has been gauged since 1929, the gauge within the upper catchment has only ten years of record. Thus, reliable estimates of the return intervals of extreme floods for this part of the Dee can only be obtained by using a variety of historical sources to extend the flood series.

Long-term rainfall records, where available, provide a valuable independent check on the reconstructed flood series. Such rainfall records, when analysed in terms of the magnitude, frequency and duration of major events, should, in general terms, correspond with the flood series. In this paper, the recurrence interval of extreme rainfalls of varying magnitude and duration in upper Deeside is estimated by extreme value analysis of the annual maximum series. The frequency of rainfall events above varying thresholds is also assessed. The existence of climatic fluctuations giving highly variable recurrence intervals for rainfall events of the same magnitude is demonstrated. Finally, the seasonality of frequent flood-producing storms is analysed. Patterns observed within the rainfall record are compared with those previously established within the historic flood series to substantiate and augment the flood record.

Type
Hydrometeorology
Copyright
Copyright © Royal Society of Edinburgh 1987

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

Acreman, M. C. 1986. Estimating flood statistics from basin characteristics in Scotland. Unpublished Ph.D. Thesis, University of St. Andrews.Google Scholar
Ballantyne, C. K. 1983. Precipitation gradients in Wester Ross, North-west Scotland. WEATHER 38, 379–87.CrossRefGoogle Scholar
Bleasdale, A. 19611965. The presentation of monthly rainfall. BR RAINFALL SUPPL 5, 227–59. Meteorological Office.Google Scholar
Box, G. E. P. & Jenkins, G. M. 1976. Time series analysis: forecasting and control. San Francisco: Holden-Day.Google Scholar
Bremner, A. 1922. The Dee floods of October, 1920. THE DEESIDE FIELD 1, 3032.Google Scholar
British Rainfall 18601966. London: Her Majesty's Stationery Office.Google Scholar
Finch, C. R. 1972. Some heavy rainfalls in Great Britain, 1956–1971. WEATHER 27, 364–77.CrossRefGoogle Scholar
Fuller, W. A. 1976. Introduction to statistical time series. New York: Wiley.Google Scholar
Gloyne, R. W. 1968. Some climatic influences affecting hill land productivity. BR GRASSLAND SOC 4, Hill-land productivity, 915.Google Scholar
Jenkinson, A. F. 1955. The frequency distribution of the annual maximum (or minimum) values of meteorological elements. Q J METEOROL SOC 81, 158–71.CrossRefGoogle Scholar
Jones, P. D. 1980. A homogeneous rainfall record for the Cirencester area, 1844–1977. METEOROL MAG 109, 249–58.Google Scholar
Jones, P. D. 1981. A survey of rainfall recording in two regions of the northern Pennines. METEOROL MAG 110, 239–52.Google Scholar
Lamb, H. H. 1972. Climate: Present, past and future, Vol. 1. London: Methuen.Google Scholar
Lamb, H. H. 1977. Climate: Present, past and future, Vol. 2. London: Methuen.Google Scholar
Lamb, H. H. 1982. Climatic changes in our own times and future threats. GEOGRAPHY 67, 203–20.Google Scholar
Lauder, T. D. 1830. An account of the great floods of August, 1829 in the province of Moray and adjoining districts. Elgin: McGillivray and son.Google Scholar
McEwen, L. J. 1986. River channel planform changes in upland Scotland, with specific reference to climatic fluctuation and Landuse Changes over the last 250 years. Unpublished Ph.D. Thesis, University of St. Andrews.Google Scholar
Natural Environment Research Council 1975. Flood studies report. London: Her Majesty's Stationery Office.Google Scholar
Perry, A. H. & Howells, K. A. 1982. Are large falls of rain in Wales becoming more frequent? WEATHER 37, 240–43.CrossRefGoogle Scholar
Salter, M. de. C. S. 1921. The rainfall of the British Isles. London: University of London Press.Google Scholar
Steven, H. M. & Carlisle, A. 1959. The native pinewoods of Scotland. Edinburgh: Oliver and Boyd.Google Scholar
Symons, G. J. 1867. Remarkably wet and cold summers. METEOROL MAG 2, 42.Google Scholar
Tabony, R. C. 1979. A spectral and filter analysis of long-period rainfall records in England and Wales. METEOROL MAG 108, 97118.Google Scholar
Werritty, A. & Acreman, M. C. 1984. The flood hazard in Scotland. In Harrison, S. J. (ed.) Climatic hazards in Scotland, 2540. Norwich: Geo-books.Google Scholar