Dye tracer tests of water movement at the glacier Austre Okstindbreen, Norway.
Whilst some water passes rapidly through the glacier from points of entry at the surface, considerable delays characterise throughflow from many points. Relatively low ice permeability is indicated by the results of a test in which tracer injected into water entering a crevasse re-emerged in water o...
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ftumanchesterpub:oai:pure.atira.dk:publications/5aeda41b-bc5b-46dc-8fc5-48b2544b0858 2024-06-23T07:53:03+00:00 Dye tracer tests of water movement at the glacier Austre Okstindbreen, Norway. Theakstone, W. H. Knudsen, N. T. 1981 https://research.manchester.ac.uk/en/publications/5aeda41b-bc5b-46dc-8fc5-48b2544b0858 eng eng https://research.manchester.ac.uk/en/publications/5aeda41b-bc5b-46dc-8fc5-48b2544b0858 info:eu-repo/semantics/restrictedAccess Theakstone , W H & Knudsen , N T 1981 , ' Dye tracer tests of water movement at the glacier Austre Okstindbreen, Norway. ' , Norsk Geografisk Tidsskrift , vol. 35 , no. 1 , pp. 21-28 . article 1981 ftumanchesterpub 2024-06-04T00:21:31Z Whilst some water passes rapidly through the glacier from points of entry at the surface, considerable delays characterise throughflow from many points. Relatively low ice permeability is indicated by the results of a test in which tracer injected into water entering a crevasse re-emerged in water overflowing from another crevasse, and in which one water-filled crevasse remained tracer-free although the water in another crevasse only a metre away became strongly coloured by the dye.-from Authors Article in Journal/Newspaper glacier The University of Manchester: Research Explorer Norway austre Okstindbreen ENVELOPE(14.293,14.293,66.014,66.014) Okstindbreen ENVELOPE(14.148,14.148,65.987,65.987) |
institution |
Open Polar |
collection |
The University of Manchester: Research Explorer |
op_collection_id |
ftumanchesterpub |
language |
English |
description |
Whilst some water passes rapidly through the glacier from points of entry at the surface, considerable delays characterise throughflow from many points. Relatively low ice permeability is indicated by the results of a test in which tracer injected into water entering a crevasse re-emerged in water overflowing from another crevasse, and in which one water-filled crevasse remained tracer-free although the water in another crevasse only a metre away became strongly coloured by the dye.-from Authors |
format |
Article in Journal/Newspaper |
author |
Theakstone, W. H. Knudsen, N. T. |
spellingShingle |
Theakstone, W. H. Knudsen, N. T. Dye tracer tests of water movement at the glacier Austre Okstindbreen, Norway. |
author_facet |
Theakstone, W. H. Knudsen, N. T. |
author_sort |
Theakstone, W. H. |
title |
Dye tracer tests of water movement at the glacier Austre Okstindbreen, Norway. |
title_short |
Dye tracer tests of water movement at the glacier Austre Okstindbreen, Norway. |
title_full |
Dye tracer tests of water movement at the glacier Austre Okstindbreen, Norway. |
title_fullStr |
Dye tracer tests of water movement at the glacier Austre Okstindbreen, Norway. |
title_full_unstemmed |
Dye tracer tests of water movement at the glacier Austre Okstindbreen, Norway. |
title_sort |
dye tracer tests of water movement at the glacier austre okstindbreen, norway. |
publishDate |
1981 |
url |
https://research.manchester.ac.uk/en/publications/5aeda41b-bc5b-46dc-8fc5-48b2544b0858 |
long_lat |
ENVELOPE(14.293,14.293,66.014,66.014) ENVELOPE(14.148,14.148,65.987,65.987) |
geographic |
Norway austre Okstindbreen Okstindbreen |
geographic_facet |
Norway austre Okstindbreen Okstindbreen |
genre |
glacier |
genre_facet |
glacier |
op_source |
Theakstone , W H & Knudsen , N T 1981 , ' Dye tracer tests of water movement at the glacier Austre Okstindbreen, Norway. ' , Norsk Geografisk Tidsskrift , vol. 35 , no. 1 , pp. 21-28 . |
op_relation |
https://research.manchester.ac.uk/en/publications/5aeda41b-bc5b-46dc-8fc5-48b2544b0858 |
op_rights |
info:eu-repo/semantics/restrictedAccess |
_version_ |
1802644538613825536 |