Climate, Tectonics, in addition to Topographic Evolution of the Washington Cascades: Insigh

Climate, Tectonics, in addition to Topographic Evolution of the Washington Cascades: Insigh www.phwiki.com

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 [1986] in addition to Roe et al. [2002]

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.

Besse, Barry KKNT-AM Operations Manager www.phwiki.com

Besse, Barry Operations Manager

Besse, Barry is from United States and they belong to KKNT-AM and they are from  Phoenix, United States got related to this Particular Journal. and Besse, Barry deal with the subjects like Entertainment

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