Climate, Tectonics, in addition to Topographic Evolution of the Washington Cascades: Insigh
Besse, Barry, Operations Manager has reference to this Academic Journal, PHwiki organized this Journal Climate, Tectonics, in addition to Topographic Evolution of the Washington Cascades: Insights from Coupled Process Models in addition to Thermochronometry Todd Ehlers – University of Michigan Peter Reiners, Gerard Roe, Sara Mitchell, David Montgomery [ George Collot, 1796 ] Washington Cascades, U.S.A. Hypothesis Tested: Long term erosion rates across the Cascades are best explained by young, transient, topography in addition to a strong orographic effect. Observations in addition to conceptual models tested Methods: Coupled atmospheric-surface processes model Comparison of model predictions in addition to data
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Observations: Erosion Rates Across Topography Distance East (km) Elevation (m) Apparent Erosion Rate (mm/yr) Max Elevation Mean Elevation Min Elevation Conceptual Models Tested Conceptual Models Tested
Conceptual Models Tested Methods Coupled Numerical Models Atmospheric Model: Similar to approach of Alpert  in addition to Roe et al. 
Atmospheric Model Per as long as mance Central Washington Cascades Surface Process Model: Based on the CASCADE algorithm of Braun in addition to Sambridge (1997) Uni as long as m Precipitation
Physically Based Atmospheric Model Topographic Evolution in addition to Precipitation Rate Animation: Topographic Evolution in addition to Precipitation Rate
Topographic Evolution in addition to Erosion Rate Animation: Topographic Evolution in addition to Erosion Rate Erosion Rate in addition to Topography: u = 0.4 mm/yr
Washington Cascades, U.S.A. Conclusions: Influence of climate on topographic evolution in orogens: Strong orographic effect results in asymmetric topography. Pulse of high erosion rates propagates across the range. Young AHe ages predicted on windward side of range. Comparison with Data Model A.5! AHe ages are generally consistent with uni as long as m uplift in addition to transient topography over last 10 Ma. Model discrepancies with data are due to neglection of isostasy which would introduce a component of non-uni as long as m uplift.
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