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Southern Sierra Critical Zone ObservatoryIntegrating measurements for advances in hydrology & geochemistry
A research platform for studying Earth surface processes in the “critical zone”, extending from the top of vegetation down through groundwater
Roger Bales, UC MercedBeth Boyer, UC BerkeleyMartha Conklin, UC MercedMike Goulden, UC IrvineJan Hopmans, UC DavisDale Johnson, U NevadaJim Kirchner, UC BerkeleyChristina Tague, UC Santa BarbaraCarolyn Hunsaker, USFS-PSW9 graduate studentsField hydrologist/geochemistData managerEducation/communications scientist
CZO team
The rain-snow transition zone is particularly vulnerable to large & rapid changes in climate & landcover. While this zone undergoes rapid seasonal changes, going from snowcoverto wet soil to dry soil over a 1-2 month period, climate warming will shift this transition period earlier or eliminate it entirely. The result will be major changes in seasonal-to-interannualcritical zone processes involving water, nutrients and ecosystem response of the largely mixed conifer forest found in the rain-snow transition zone. Forest density & the threat of catastrophic fire in the zone are very high, leading to the further likelihood of changes in longer-term critical zone processes. Steep gradients in precipitation patterns, along both elevation and aspect, plus rapid seasonal changes, make this zone an excellent natural laboratory for studying how critical zone processes respond to perturbations, & particularlyhow the water cycle drives critical zone processes. Also, the characteristic spatial differences along gradients offer the opportunity to substitute space for time.
Background
Research support: National Science Foundation
Research partner: Pacific Southwest Research Station, U.S. Forest Service
CZO
– meteorology & snowpack– soil moisture & temperature– groundwater levels & temperature– erosion & sedimentation– snowmelt, rain, stream, groundwater &
soil chemistry
CZO measurements
– water cycle & response to perturbations– coupled hydrologic & (bio)geochemical processes/cycles– extreme hydrologic events in hydrologic & (bio)geochemical
cycles– vegetation control over fluxes of water & nutrients– pathways for transport of water, heat & mass– role of seasonal snowpack in determining critical zone processes
Planned investigations
CZO is located in the N. Fork of the Kings R., in the Southern Sierra Nevada. The CZO catchments cross the rain-snow transition, in the mixed conifer forest.
PSW measurements
– meteorology– stream stage & discharge– stream condition & physical habitat– erosion & sedimentation– geology, soils & litter– snowmelt, rain, stream & soil chemistry– riparian & upland vegetation– stream invertebrates, algae & periphyton
Stream major ionsCumulative discharge for 3 catchments, WY 2004
Installing Echo probes for soil moisture & temperature
sediment basin
stream discharge
groundwater
snow depth
satellite snowcover
More information
Sierra Nevada Research Institute http://snri.ucmerced.edu
CZO home: http://snri.ucmerced.edu/CZO
Data: http://eng.ucmerced.edu/snsjho stream instrumentation
met station