Dynamics of a Massive Freshwater Influx in the Clyde Estuary

The Clyde Estuary catchment area received an immense amount of rainfall over a short period (9–11 December 1994) with an estimated return period of over 500 years. The average flow into the Estuary is 156m3s−1, and the total peak flow gauged during this event was about 2000m3s−1. The influx of this...

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Veröffentlicht in:Estuarine, coastal and shelf science coastal and shelf science, 1997-04, Vol.44 (4), p.385-393
Hauptverfasser: Thomason, J.C., Hills, J.M., Bennett, A.M.
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container_title Estuarine, coastal and shelf science
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creator Thomason, J.C.
Hills, J.M.
Bennett, A.M.
description The Clyde Estuary catchment area received an immense amount of rainfall over a short period (9–11 December 1994) with an estimated return period of over 500 years. The average flow into the Estuary is 156m3s−1, and the total peak flow gauged during this event was about 2000m3s−1. The influx of this water was monitored daily over the following week for a single transect across the Largs Channel. A cruise was made around the Estuary at the peak of the influx on 16 December. Profiles of salinity, temperature and photosynthetically active radiation were taken at 38 stations, covering over 34km. The daily and cruise data are presented against background data collected since September 1994 for a single station in the Largs Channel.
doi_str_mv 10.1006/ecss.1996.0141
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source Elsevier ScienceDirect Journals
subjects Brackish
Earth sciences
Earth, ocean, space
estuaries
Exact sciences and technology
Firth of Clyde
freshwater
Marine and continental quaternary
rainfall
salinity
Scotland
Surficial geology
temperature
title Dynamics of a Massive Freshwater Influx in the Clyde Estuary
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