Articles | Volume 11, issue 5
https://doi.org/10.5194/esurf-11-849-2023
https://doi.org/10.5194/esurf-11-849-2023
Research article
 | 
08 Sep 2023
Research article |  | 08 Sep 2023

Spatially coherent variability in modern orographic precipitation produces asymmetric paleo-glacier extents in flowline models: Olympic Mountains, USA

Andrew A. Margason, Alison M. Anders, Robert J. C. Conrick, and Gerard H. Roe

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Cited articles

Adams, B. A. and Ehlers, T. A.: Tectonic controls of Holocene erosion in a glaciated orogen, Earth Surf. Dynam., 6, 595–610, https://doi.org/10.5194/esurf-6-595-2018, 2018. 
Anders, A. M., Roe, G. H., Durran, D. R., and Minder, J. R.: Small-Scale Spatial Gradients in Climatological Precipitation on the Olympic Peninsula, J. Hydrometeorol., 8, 1068–1081, https://doi.org/10.1175/JHM610.1, 2007. 
Anders, A. M., Mitchell, S. G., and Tomkin, J. H.: Cirques, peaks, and precipitation patterns in the Swiss Alps: Connections among climate, glacial erosion, and topography, Geology, 38, 239–242, https://doi.org/10.1130/G30691.1, 2010. 
Barnston, A. G. and Livezey, R. E.: Classification, Seasonality and Persistence of Low-Frequency Atmospheric Circulation Patterns, Mon. Weather Rev., 115, 1083–1126, https://doi.org/10.1175/1520-0493(1987)115<1083:CSAPOL>2.0.CO;2, 1987. 
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Short summary
We examine differences in glacier extent in the Olympic Mountains, USA, where modern precipitation in east-facing valleys is only 50 % of that in west-facing valleys. During the Last Glacial Period, there were very small glaciers in the east and very large glaciers in the west. We use climate data and glacier models to show that the modern spatial pattern of precipitation is likely to have been similar during the past glaciation and may be sufficient to explain the asymmetry of glacier extent.
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