Process linkages between geology, topography, and life: Vegetation distribution in the Eel River watershed appears to be controlled principally by lithologic variation across accreted terrains. For example, coniferous forests are often absent from the central mélange belt, but the mechanisms inhibiting these forests are poorly understood. A complementary area of interest is to better understand how tectonic forcing, biota, and geomorphic processes produce unique landscape forms across different rock types. For example, hillslopes are steep and convexo-planar in the greywackes and argillites of the ER CZO, relative to the gently undulating nearby mélange, but the processes responsible for hillslope sediment transport (and ultimately landscape form) in both rock types are not well understood. One way to explore a process inferred from field observation is to cast it in the form of a geomorphic transport law, which can be coupled with continuity in a model landscape.
CZO Research Groups
Quantification of the seasonal hillslope water storage that does not drive streamflow. Dralle, D.N., Hahm, W.J., Rempe, D.M., Karst, N.J., Thompson, S.E., Dietrich, W.E. (2018): Hydrological Processes
Controls on the distribution and resilience of Quercus garryana: ecophysiological evidence of oak's water‐limitation tolerance. Hahm, W.J., Dietrich, W.E., and Dawson, T.E. (2018): Ecosphere 9 (5)
Testing for supply limited and kinetic limited chemical erosion in field measurements of regolith production and chemical depletion. Ferrier, K. L., Riebe, C. S. and Hahm, W. J. (2016): Geochemistry, Geophysics, Geosystems. 17 (6), 2270-2285.
Landscape response to tipping points in granite weathering: The case of stepped topography in the Southern Sierra Critical Zone Observatory. Jessup, BS; Hahm, WJ; Miller, SN; Kirchner, JW; Riebe, CS. (2011): Applied Geochemistry
Papers and books that explicitly acknowledge a CZO grant are highlighted in PALE ORANGE.
Comprehensive seismic surveys suggest that subsurface water-holding capacity is secondary to bedrock nutrient content as a regulator of vegetation productivity in the Sierra Nevada Batholith, California. Taylor, N.J.; Riebe, C.S.; Dueker, K.G.; Goulden, M.; Flinchum, B.A.; Pasquet, S.; Callahan, R.P.; Hahm, W.J.; Keifer, I.S.; Holbrook, W.S. (2016): Fall Meeting, American Geophysical Union, December 2016. Abstract EP43C-0964.
Testing for supply-limited chemical erosion in field measurements of soil production and chemical depletion. Ferrier, K.; C. Riebe; W.J. Hahm; J. Kirchner (2014): American Geophysical Union, Fall Meeting 2014, abstract #EP13E-04
Strong Lithologic Control on Mountain Ecosystem Productivity and Landscape Evolution. Hahm, W.J., C.S. Riebe, C.E. Lukens, and S. Araki. (2013): The Geological Society of America annual meeting
Bedrock composition limits mountain ecosystem productivity and landscape evolution. Riebe, C.S. W.J. Hahm; and C. Lukens (2013): American Geophysical Union, Fall Meeting 2013, abstract #B13L-02