Item talk:Q240302
From geokb
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"name": "Glacial conditioning of stream position and flooding in the braid plain of the Exit Glacier foreland, Alaska",
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"abstract": "Flow spilling out of an active braid plain often signals the onset of channel migration or\u00a0avulsion\u00a0to previously occupied areas. In a recently deglaciated environment, distinguishing between shifts in active braid plain location, considered reversible by\u00a0fluvial processes\u00a0at short timescales, and more permanent glacier-conditioned changes in stream position can be critical to understanding flood hazards. Between 2009 and 2014, increased spilling from the Exit Creek braid plain in Kenai\u00a0Fjords\u00a0National Park, Alaska, repeatedly overtopped the only\u00a0access road\u00a0to the popular Exit Glacier visitor facilities and trails. To understand the likely cause of road flooding, we consider recent processes and the interplay between glacier and fluvial system dynamics since the maximum advance of the\u00a0Little Ice Age, around 1815. Patterns of temperature and precipitation, the variables that drive high\u00a0streamflow\u00a0via\u00a0snowmelt, glacier\u00a0meltwater\u00a0runoff, and rainfall, could not fully explain the timing of road floods. Comparison of high-resolution topographic data between 2008 and 2012 showed a strong pattern of braid plain\u00a0aggradation\u00a0along 3\u00a0km of glacier foreland, not unexpected at the base of mountainous glaciers and likely an impetus for channel migration. Historically, a dynamic zone follows the retreating glacier in which channel positions shift rapidly in response to changes in the glacier margin and fresh morainal deposits. This period of paraglacial adjustment lasts one to several decades at Exit Glacier. Subsequently, as\u00a0moraine\u00a0breaches consolidate and lock the channel into position, and as the stream regains the lower-elevation valley center, upper-elevation surfaces are abandoned as terraces inaccessible by fluvial processes for timescales of decades to centuries. Where not constrained by these terraces and\u00a0moraines, the channel is free to migrate, which in this aggradational setting generates an\u00a0alluvial fan\u00a0at the breach of the final prominent moraine. The position of this fan is glacially conditioned but the process of migration of the braided channels across it is not. This broad perspective on channel controls identifies incipient avulsion into the roadside forest as part of a long-term fan-building process independent from changes in streamflow or sediment load.",
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