| Titre | Ground ice degradation and thermokarst terrain formation in Canada over the past 16 000 years |
| Télécharger | Téléchargements |
| |
| Licence | Veuillez noter que la Licence du gouvernement
ouvert - Canada remplace toutes les licences antérieures. |
| Auteur | Wolfe, S A ;
O'Neill, H B; Duchesne, C; Froese, D; Young, J M; Kokelj, S V |
| Source | Commission géologique du Canada, Présentation scientifique 134, 2022, 1 feuille, https://doi.org/10.4095/329668  Accès ouvert |
| Image |  |
| Année | 2022 |
| Éditeur | Ressources naturelles Canada |
| Réunion | Arctic Change 2021; décembre 2021 |
| Document | publication en série |
| Lang. | anglais |
| DOI | https://doi.org/10.4095/329668 |
| Media | numérique; en ligne |
| Référence reliée | Cette publication est reliée à Ground ice map of
Canada |
| Formats | pdf |
| Province | Canada; Colombie-Britannique; Alberta; Saskatchewan; Manitoba; Ontario; Québec; Nouveau-Brunswick; Nouvelle-Écosse; Île-du-Prince-Édouard; Terre-Neuve-et-Labrador; Territoires du Nord-Ouest; Yukon;
Nunavut |
| SNRC | 1; 2; 3; 10; 11; 12; 13; 14; 15; 16; 20; 21; 22; 23; 24; 25; 26; 27; 28; 29; 30; 31; 32; 33; 34; 35; 36; 37; 38; 39; 40; 41; 42; 43; 44; 45; 46; 47; 48; 49; 52; 53; 54; 55; 56; 57; 58; 59; 62; 63; 64; 65;
66; 67; 68; 69; 72; 73; 74; 75; 76; 77; 78; 79; 82; 83; 84; 85; 86; 87; 88; 89; 92; 93; 94; 95; 96; 97; 98; 99; 102; 103; 104; 105; 106; 107; 114O; 114P; 115; 116; 117; 120; 340; 560 |
| Lat/Long OENS | -141.0000 -50.0000 90.0000 41.7500 |
| Sujets | pergélisol; glace fossile; caractéristiques périglaciaires; thermokarst; fentes de glace; modèles; glissements de terrain; glissements; affaissement; fluage; buttes; topographie; types de terrain;
Changement climatique; dégel du pergélisol; buttes cryogènes; palses; Base de données; géologie des dépôts meubles/géomorphologie; géologie de l'environnement; Nature et environnement; Sciences et technologie; Phanérozoïque; Cénozoïque;
Quaternaire |
| Illustrations | cartes géolscientiques généralisées; tableaux; photographies; images satellitaires |
| Programme | GEM2 : La géocartographie de l'énergie et des minéraux TransGEM |
| Diffusé | 2022 03 15 |
| Résumé | (disponible en anglais seulement)
Thermokarst results from thawing of excess ground ice in permafrost sediments. Thermokarst processes and landforms are controlled by ground ice type, amount and
distribution, as well as the patterns of ground ice loss over time. Recent acceleration of varied thermokarst processes across diverse Canadian permafrost terrains make for a challenging task in predicting landscape-scale thaw trajectories. Using
existing ground ice models, we examined the modelled amounts and spatial extent of ground ice loss relative to ground ice maxima in the last ca. 16 ka BP for relict, segregated and wedge ice. We relate observed thermokarst features to the nature of
ground ice development and loss in different environments (cold continuous permafrost, discontinuous permafrost, and no current permafrost). In cold, continuous permafrost areas where ground ice loss has been limited over the last 16 ka BP,
thermokarst processes include active layer detachments and slumps in segregated and relict ice, gullying and ponding in ice wedge troughs, and the cyclical development of shallow thermokarst ponds in segregated ice. With ground ice loss in
discontinuous permafrost, thermokarst processes are wide-ranging. Slumps, subsidence, and collapse of lithalsas, palsas and peat plateaus occur from thawing of segregated ice, thermokarst ponds from melting wedge and segregated ice, and involuted
terrain from melting and creep of relict or segregated ice. In former permafrost terrain, evidence of thermokarst includes former ice wedge polygons, collapsed lithalsas, and irregular hummocky terrain. The relations between modelled ground ice loss
and observed thermokarst landscapes assist in understanding present-day processes and in predicting future thermokarst landform evolution with a changing climate. |
| Sommaire | (Résumé en langage clair et simple, non publié)
Nous examinons la relation entre la perte de glace au sol modélisée dans le pergélisol et les processus thermokarstiques et les formes de relief
au Canada. |
| GEOSCAN ID | 329668 |
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