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Poodle, T. (1987) Factors affecting the future of the Scottish hydrometric network. Transactions of the Royal Society of Edinburgh: Earth Sciences, 78 (4) 269-274 doi:10.1017/s0263593300011202

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Reference TypeJournal (article/letter/editorial)
TitleFactors affecting the future of the Scottish hydrometric network
JournalTransactions of the Royal Society of Edinburgh: Earth Sciences
AuthorsPoodle, T.Author
Year1987Volume78
Issue4
PublisherCambridge University Press (CUP)
DOIdoi:10.1017/s0263593300011202Search in ResearchGate
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Mindat Ref. ID494103Long-form Identifiermindat:1:5:494103:7
GUID0
Full ReferencePoodle, T. (1987) Factors affecting the future of the Scottish hydrometric network. Transactions of the Royal Society of Edinburgh: Earth Sciences, 78 (4) 269-274 doi:10.1017/s0263593300011202
Plain TextPoodle, T. (1987) Factors affecting the future of the Scottish hydrometric network. Transactions of the Royal Society of Edinburgh: Earth Sciences, 78 (4) 269-274 doi:10.1017/s0263593300011202
In(1987) Transactions of the Royal Society of Edinburgh: Earth Sciences Vol. 78 (4) Cambridge University Press (CUP)
Abstract/NotesABSTRACTThe Scottish Hydrometric Network consists of a number of river gauging stations which have been located at sites considered suitable to provide long term flow records. Economic recession has placed some stress on the gauging programme, and has given rise to extensive closures of gauging stations in England and, to a minor extent so far, in Scotland. The way in which the network became established provides a mixture of strengths and weaknesses which could have unpredictable consequences in an adverse economic climate. Changing technology provides some opportunity to reduce the cost of data acquisition and improve the deployment of manpower, while maintaining data standards. In these changing circumstances, particularly with extensive use of computer systems, it is important that standards are established for data returned to the Water Archive and that the network is not allowed to degenerate by default.


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