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- W2049230220 abstract "The current retreat of the glacier fronts induces changes of both discharge and sediment availability. Consequently, the fluvial hydrosystem adjusts its fluvial pattern to these new conditions. However, the relationships between rate of glacial retreat and fluvial pattern adjustment are not direct. Some landscape units linked to glacial activity, like moraines and proglacial lakes, alter locally the sediment balance and disturb the alluvial outwash plain response." @default.
- W2049230220 created "2016-06-24" @default.
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- W2049230220 date "2008-01-01" @default.
- W2049230220 modified "2023-09-23" @default.
- W2049230220 title "Modification du style fluvial proglaciaire en contexte paraglaciaire : l'exemple du Morsárjökull, (Change of proglacial fluvial pattern under paraglacial setting : the Morsárjökull case)" @default.
- W2049230220 doi "https://doi.org/10.3406/bagf.2008.2611" @default.
- W2049230220 hasPublicationYear "2008" @default.
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