Diurnal, semidiurnal, and fortnightly tidal components in orthotidal proglacial rivers
Author:
Funder
CNCS – UEFISCDI
Publisher
Springer Science and Business Media LLC
Subject
Management, Monitoring, Policy and Law,Pollution,General Environmental Science,General Medicine
Link
http://link.springer.com/article/10.1007/s10661-018-6513-x/fulltext.html
Reference46 articles.
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2. Aðalgeirsdóttir, G., Smith, A. M., Murray, T., King, M. A., Makinson, K., Nicholls, K. W., & Behar, A. E. (2008). Tidal influence on Rutford ice stream, West Antarctica: Observations of surface flow and basal processes from closely spaced GPS and passive seismic stations. Journal of Glaciology, 54(187), 715–724. https://doi.org/10.3189/002214308786570872 .
3. Anandakrishnan, S., Voigt, D. E., & Alley, R. B. (2003). Ice stream D flow speed is strongly modulated by the tide beneath the Ross ice shelf. Geophysical Research Letters, 30(7), 1361.
4. Bartholomaus, T. C., Anderson, R. S., & Suzanne, P. A. (2008). Response of glacier basal motion to transient water storage. Nature Geoscience, 1(1), 33–37. https://doi.org/10.1038/ngeo.2007.52 .
5. Bower, D. R. (1983). Bedrock fracture parameters from the interpretation of well tides. Journal of Geophysical Research, 88(B6), 5025–5035. https://doi.org/10.1029/JB088iB06p05025 .
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