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Riverflow reconstructions for 15 catchments over England and Wales and an assessment of hydrologic drought since 1865
Author(s) -
Jones P. D.,
Lister D. H.
Publication year - 1998
Publication title -
international journal of climatology
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.58
H-Index - 166
eISSN - 1097-0088
pISSN - 0899-8418
DOI - 10.1002/(sici)1097-0088(199807)18:9<999::aid-joc300>3.0.co;2-8
Subject(s) - context (archaeology) , surface runoff , drainage basin , streamflow , environmental science , period (music) , hydrology (agriculture) , climatology , hydrological modelling , water year , physical geography , geography , geology , cartography , archaeology , ecology , physics , geotechnical engineering , acoustics , biology
Recent years have seen increased risks of water supply problems because of reduced rainfall in some seasons. Over England and Wales most riverflow records begin during the 1950s and 1960s. The short record length, therefore, makes assessment of the rarity of some low flow sequences difficult. A means of extending riverflow records is to reconstruct them using a simple catchment model and the plentiful monthly rainfall totals available for England and Wales. Riverflow data on a monthly basis have been reconstructed for 15 catchments for the period since the 1860s. The reconstructions are produced with a regression‐based catchment model that relates lagged values of rainfall to runoff. The statistical nature of the model requires that any reconstructions be assessed over an independent data period. All perform almost as well as during the calibration periods. Using the reconstructions, recent hydrologic droughts are put in to a longer term context. On none of the catchments is the most extreme 6 months (April–September) average riverflow found to occur during the 1986–1995 period. On a number of catchments, the extreme year is 1976 or 1984. Flows were low during 1989–1992 and 1995, with the former four year period being unusual, because the years occurred in succession. On all 15 catchments, however, an earlier sequence occurring between 1865 and 1980 is more severe. © 1998 Royal Meteorological Society