LAKE MOVEMENTS WITH PARTIAL ICE COVER
A recording current meter was operated under a winter ice sheet at Nanticoke, Lake Erie, in 11 m of water at a depth of 3 m from the bottom. Current magnitude and direc-tion and water temperature were measured every 10 min. Current magnitudes up to 1 month after the ice sheet formed were similar to...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.558.3713 2023-05-15T16:40:14+02:00 LAKE MOVEMENTS WITH PARTIAL ICE COVER M. D. Palmer J. Bryan Ixatt The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.558.3713 http://www.aslo.org/lo/toc/vol_17/issue_3/0403.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.558.3713 http://www.aslo.org/lo/toc/vol_17/issue_3/0403.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.aslo.org/lo/toc/vol_17/issue_3/0403.pdf text ftciteseerx 2016-01-08T11:53:05Z A recording current meter was operated under a winter ice sheet at Nanticoke, Lake Erie, in 11 m of water at a depth of 3 m from the bottom. Current magnitude and direc-tion and water temperature were measured every 10 min. Current magnitudes up to 1 month after the ice sheet formed were similar to measurements made without ice; auto-variance density spectra for this period showed energy concentrations at frequencies cor-responding to the fret oscillation modes of Lake Erie. Several months after the ice had been in place the measured currents were half as fast (3-9 cm/set) and spectra during this period showed no energy concentrations at Lake Erie oscillation frequencies. Text Ice Sheet Unknown |
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ftciteseerx |
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English |
description |
A recording current meter was operated under a winter ice sheet at Nanticoke, Lake Erie, in 11 m of water at a depth of 3 m from the bottom. Current magnitude and direc-tion and water temperature were measured every 10 min. Current magnitudes up to 1 month after the ice sheet formed were similar to measurements made without ice; auto-variance density spectra for this period showed energy concentrations at frequencies cor-responding to the fret oscillation modes of Lake Erie. Several months after the ice had been in place the measured currents were half as fast (3-9 cm/set) and spectra during this period showed no energy concentrations at Lake Erie oscillation frequencies. |
author2 |
The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
M. D. Palmer J. Bryan Ixatt |
spellingShingle |
M. D. Palmer J. Bryan Ixatt LAKE MOVEMENTS WITH PARTIAL ICE COVER |
author_facet |
M. D. Palmer J. Bryan Ixatt |
author_sort |
M. D. Palmer |
title |
LAKE MOVEMENTS WITH PARTIAL ICE COVER |
title_short |
LAKE MOVEMENTS WITH PARTIAL ICE COVER |
title_full |
LAKE MOVEMENTS WITH PARTIAL ICE COVER |
title_fullStr |
LAKE MOVEMENTS WITH PARTIAL ICE COVER |
title_full_unstemmed |
LAKE MOVEMENTS WITH PARTIAL ICE COVER |
title_sort |
lake movements with partial ice cover |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.558.3713 http://www.aslo.org/lo/toc/vol_17/issue_3/0403.pdf |
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Ice Sheet |
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Ice Sheet |
op_source |
http://www.aslo.org/lo/toc/vol_17/issue_3/0403.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.558.3713 http://www.aslo.org/lo/toc/vol_17/issue_3/0403.pdf |
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Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
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1766030618792034304 |