SEIFERT, Shannon L.1, SCHWARZ, Terence C.1, and WALTER, M. Todd2, (1) Environmental Science, Univ of Alaska Southeast, 11120 Glacier Highway, Juneau, AK 99801,, (2) Biological and Environmental Engineering, Cornell Univ, Ithaca, NY 14853-5701

An interconnected system of small supraglacial lakes on Lemon Glacier near Juneau, AK was studied throughout summer 2001 to better understand downstream implications of glacial lake outburst flood (GLOF) on Lemon Creek water quality. Through processes of supraglacial lake expansion, increasing volumes of glacially stored water are discharged over time. Determining the effects of current GLOF discharge on Lemon Creek water quality will aid in anticipating impacts of larger volume GLOF discharges in the coming decades. Mechanisms governing supraglacial lake filling and drainage specific to Lemon Glacier are only hypothesized at this time as englacial or subglacial blockage disturbed by a moderate to extreme storm event triggering release in late summer. Glacially stored water is eventually discharged from beneath the glacier terminus into Lemon Creek, a proglacial stream supporting several resident and anadromous fish species that is currently listed by the EPA as impaired for sediment and turbidity. Daily sediment samples collected throughout summer 2001 at a USGS discharge gauging station 4 miles downstream from the glacier terminus were analyzed for suspended sediment concentration (SSC). No discernible discharge peak is associated with glacier lake outburst flooding on Lemon Creek, as glacial drainage events are triggered by, and tend to "piggyback" moderate to extreme storm events. However, the SSC increase generated by storm events was relatively minor when compared to the increase in SSC generated by outburst flood events, suggesting a “flushing” of subglacial sediment and debris unique to subglacial drainage.

Cordilleran Section - 98th Annual Meeting (May 13–15, 2002)
Session No. 26--Booth# 3
Quaternary Geology and Paleoclimate (Posters)
LaSells Stewart Center: Agriculture
1:30 PM-5:30 PM, Tuesday, May 14, 2002

© Copyright 2002 The Geological Society of America (GSA), all rights reserved. Permission is hereby granted to the author(s) of this abstract to reproduce and distribute it freely, for noncommercial purposes. Permission is hereby granted to any individual scientist to download a single copy of this electronic file and reproduce up to 20 paper copies for noncommercial purposes advancing science and education, including classroom use, providing all reproductions include the complete content shown here, including the author information. All other forms of reproduction and/or transmittal are prohibited without written permission from GSA Copyright Permissions.