{"id":511,"date":"2022-12-18T15:04:09","date_gmt":"2022-12-18T22:04:09","guid":{"rendered":"http:\/\/shaksnas2.local\/cripe-wp-dev\/?page_id=511"},"modified":"2026-01-10T16:19:12","modified_gmt":"2026-01-10T23:19:12","slug":"recherche","status":"publish","type":"page","link":"https:\/\/cripe.ca\/fr\/publications\/procedure\/recherche\/","title":{"rendered":"Consulter les actes"},"content":{"rendered":"
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\n \"Ic\u00f4ne\"\n <\/div>\n
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Mesure \u00e0 distance de la \u00e9paisseur de la glace\n <\/h3>\n
J. S. Ford, S. Beltaos, W. J. Moody et N. Madsen<\/div>\n
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\n <\/i> 2,06 Mo\n <\/div>\n <\/div>\n
\n Consulter le document<\/a>\n <\/div>\n <\/div>\n<\/div>\n<\/div>
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\n \"Ic\u00f4ne\"\n <\/div>\n
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Effets de la glace de Frazil sur les poissons\n <\/h3>\n
R. S. Brown, S. S. Stanislawski et W. C. Mackay<\/div>\n
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\n <\/i> 762,33 Ko\n <\/div>\n <\/div>\n
\n Consulter le document<\/a>\n <\/div>\n <\/div>\n<\/div>\n<\/div>
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\n \"Ic\u00f4ne\"\n <\/div>\n
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Simulation de la coul\u00e9e de glace dans les rivi\u00e8res avec des \u00eeles\n <\/h3>\n
M. Jasek<\/div>\n
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\n <\/i> 764,50 Ko\n <\/div>\n <\/div>\n
\n Consulter le document<\/a>\n <\/div>\n <\/div>\n<\/div>\n<\/div>
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\n \"Ic\u00f4ne\"\n <\/div>\n
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Une comparaison des mod\u00e8les de profil ICEJAM et RIVJAM Ice Jam\n <\/h3>\n
D. Healy, F. Hicks et S. Beltaos<\/div>\n
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\n <\/i> 708,99 Ko\n <\/div>\n <\/div>\n
\n Consulter le document<\/a>\n <\/div>\n <\/div>\n<\/div>\n<\/div>
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\n \"Ic\u00f4ne\"\n <\/div>\n
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Mod\u00e9lisation \u00e9l\u00e9mentaire des glaciers et des structures de navigation fluviales\n <\/h3>\n
M. Hopkins et S. Daly<\/div>\n
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\n <\/i> 7,33 Mo\n <\/div>\n <\/div>\n
\n Consulter le document<\/a>\n <\/div>\n <\/div>\n<\/div>\n<\/div>
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\n \"Ic\u00f4ne\"\n <\/div>\n
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Simulation dynamique des conditions de glace dans les zones adjacentes aux \u00e9cluses et aux barrages\n <\/h3>\n
L. Liu, A. M. Tuthill et H. T. Shen<\/div>\n
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\n <\/i> 668,15 Ko\n <\/div>\n <\/div>\n
\n Consulter le document<\/a>\n <\/div>\n <\/div>\n<\/div>\n<\/div>
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\n \"Ic\u00f4ne\"\n <\/div>\n
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Observations du mouvement de glace dynamique sur la rivi\u00e8re Athabasca \u00e0 Fort McMurray, en Alberta\n <\/h3>\n
T. Kowalczyk et F. Hicks<\/div>\n
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\n <\/i> 2,04 Mo\n <\/div>\n <\/div>\n
\n Consulter le document<\/a>\n <\/div>\n <\/div>\n<\/div>\n<\/div>
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\n \"Ic\u00f4ne\"\n <\/div>\n
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Un instrument pour d\u00e9tecter les processus de glace de gel, de mi-hiver et de rupture dans les rivi\u00e8res\n <\/h3>\n
M. Jasek, M. Marko, D. Fissel, M. Clarke, M. Buermans et K. Paslawski<\/div>\n
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\n <\/i> 2,82 Mo\n <\/div>\n <\/div>\n
\n Consulter le document<\/a>\n <\/div>\n <\/div>\n<\/div>\n<\/div>
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\n \"Ic\u00f4ne\"\n <\/div>\n
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Mod\u00e9lisation de la consolidation de la couverture de glace lors de la phase de gel de la rivi\u00e8re Peace, en Alberta\n <\/h3>\n
F. Hicks, R. Andrishak et Y. She<\/div>\n
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\n <\/i> 2,75 Mo\n <\/div>\n <\/div>\n
\n Consulter le document<\/a>\n <\/div>\n <\/div>\n<\/div>\n<\/div>
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\n \"Ic\u00f4ne\"\n <\/div>\n
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Comparaison des concentrations de glace mod\u00e9lis\u00e9es par CRISSP et mesur\u00e9es par SWIPS sur la rivi\u00e8re Peace\n <\/h3>\n
Martin Jasek, Tadros Ghobrial, Mark Loewen et Faye Hicks<\/div>\n
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\n <\/i> 2,49 Mo\n <\/div>\n <\/div>\n
\n Consulter le document<\/a>\n <\/div>\n <\/div>\n<\/div>\n<\/div><\/div>
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