Evolving High Arctic Landscapes: A Fluvial Geomorphic Perspective
Recent climate warming and changing precipitation patterns have both thermally and physically disturbed permafrost watersheds across much of the Arctic, increasing the mobility of dissolved and particulate material from terrestrial to aquatic environments. The overarching objective of this research was to determine the spatial and temporal scale of the impact permafrost disturbances, both thermal and physical, have on all of the major components of fluvial material fluxes. This research significantly expanded on long-term field observations (2003- 2017) at the Cape Bounty Arctic Watershed Observatory (CBAWO) in the Canadian High Arctic (~75 ºN). Thermal disturbance (deep active layer thaw) significantly alters the export of dissolved ions at all spatial scales observed and fluxes remain elevated after a decade of observation, post-disturbance. Localized physical disturbances (active layer detachments: ALDs) were shown to change fluvial systems from dissolved to particulate dominated export in small, headwater-slope streams. Particulate fluxes respond immediately to and recover rapidly from localized ALDs, but remain elevated ten-years post physical-disturbance. Despite increased particulate erosion from small, headwater-slope streams, localized ALDs have not increased the downstream, watershed-scale flux of particulate material beyond an immediate, short-lived pulse at the outlet of both watersheds. This indicates that the impact of localized ALDs on particulate material fluxes does not spatially scale-up to the larger watersheds at the CBAWO, which is largely explained by: (1) the propensity toward net in-channel and extra-channel sediment storage along the main drainage network, (2) changing hydrometeorological conditions, and (3) limited contemporary fluvial energy to mobilize additional sediment in this setting. This research has substantially advanced our understanding of how different types of permafrost disturbance alter the composition and magnitudes of fluvial fluxes in discernible ways that improve our understanding of changes to circum-Arctic environments. This thesis provides essential constraints on the temporal persistence of the impact of differing permafrost disturbances on fluvial systems. Results from this thesis will help inform coupled climate-terrestrial models and will help to spatially-scale the impact of permafrost changes on fluvial systems across the circum-Arctic.
URI for this recordhttp://hdl.handle.net/1974/26548
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