Southern Sierra Critical Zone Observatory infrastructure consists of several instrumented field sites, datasets, and other resources for carrrying out field research, data analysis, and modeling.

For questions about our field infrastructure or visiting field sites for research purposes, contact our Field Manager, Erin Stacy, or Outreach Manager, Michelle Gilmore. Data can be browsed and accessed through our dataset listings; please direct data questions to our Data Manager, Xiande Meng.

Water-cycling instrumentation around Critical Zone Tree 1

CZO infrastructure creates an extensive and informed research platform

Tightly-linked, multidisciplinary research carried out by our investigators, collaborators, and other researchers have resulted in intensively studied field areas with multi-year measurement records, many of which are available online in our Data Listings. Learn more about our five research areas in the Field Areas section of our website. Our CZO also offers sample collection resources and logistical support for researchers who want to conduct studies at our sites. 

A selection of ongoing instrument-based and manual measurement initiatives are described below. Additional information about field areas, sensors, and other infrastructure and resources are available in the subpages of this Infrastructure section.

Interactive Map of Research at SSCZO Field Sites

Click here to view a larger version of this map (recommended).

The map above was developed in 2018 by undergraduate assistant Madeline Castro under supervision of Michelle Gilmore and Erin Stacy in collaboration with the UC Merced Spatial Analysis & Research Center. In 2019, we plan to expand map layers to include our work in Sequoia National Park and more locations of previous sample collection efforts. If you have feedback about the map or suggestions for improvements, please contact Michelle Gilmore.



Evapotranspiration Studies

There are currently four eddy covariance gas flux towers in operation at along a west-to-east transect of the southern Sierra Nevada, including San Joaquin Experimental Range (405 m), Soaproot Saddle (1160 m), Providence Creek Catchment P301 (2015 m), and Shorthair Creek (2700 m). The change in climate along the flux tower transect allows for investigations on interactions between climate, soil development, species distribution, biotic production, and hydrological balance.

Flux towers provide individual measurements of water, energy and carbon exchange with the atmosphere. This data is then extended outward using the meteorological, snow/soil, remotely sensed and other spatial data to understand broader interactions at different scales. Tower instruments also provide an measure of evapotranspiration and net ecosystem productivity by measuring 3-dimensional windspeeds, gaseous carbon dioxide, and water vapor. Additional instrumentation has been added over several years, such as multi-wavelength panning cameras.

Two Cosmic-ray Soil Moisture Observing Systems (COSMOS) were co-located with the P301 and Shorthair towers in June 2011. COSMOS is an advanced technology used to measure soil water content over large areas; this is a collaboration with the University of Arizona. Additionally, the Providence Creek flux tower is used as the main data transmission hub for the site's embedded wireless sensor network.

See other webpages for more information about the towers' instruments and locations. For additional information, contact: Michael Goulden.

Critical Zone Tree Experiments

In August 2008 we instrumented a mature white fir (Abies concolor) and the surrounding soil to better define the water balance in a single tree; we call this tree CZT-1. In July 2010, we instrumented a second tree, a Ponderosa pine (Pinus ponderosa) in shallower soils on a drier, exposed slope. Sap-flow measurements in the trunk and stem-water-potential measurements in the canopy capture the seasonal cycles of soil wetting and drying. See time lapse photos of snow around the tree in 2008-09. Between 2010 and the present, six other Critical Zone Trees were established for shorter term monitoring projects. Today CZT-1 is still actively instrumented.

The objectives of this study are to 1) monitor surface and subsurface water budgets in remote landscapes, with specific attention to moisture and temperature variability in near surface soils and 2) study the interactions between soil hydrology and tree functioning in a forested catchment, as part of a wider effort to analyze changing ecosystem response to changing environmental inputs.

In September 2010 a root excavation was conducted on a white fir adjacent to the first Critical Zone tree. Excavation was performed to map the root structure and location in response to new questions regarding moisture deficit in the soil profile. Excavation allows us to confirm the lateral and vertical extent of the root system and provide a better estimate of the area of influence of moisture removal for the tree.

See other webpages for more information about Critical Zone Tree instruments and site location. For additional information, contact Peter Hartsough.


Some of the biogeochemical studies conducted at the Southern Sierra Critical Zone Observatory include:

  • Using snow melt plots to determine which soil biogeochemical processes are most likely to be impacted by climate change across the rain-snow transition zone.
  • Researching carbon cycling and organic matter stabilization as affected by erosion.
  • Estimating the response of gaseous fluxes to climate change using an N isotope mass-balance model in order to determine how the rain-snow transition zone affects N cycling in the plant-soil system.
  • Investigatiing nutrient hotspots and O horizon runoff in soils.

For additional information, contact Asmeret Asefaw Berhe or Stephen Hart.

Surface-Groundwater Interactions

The objective of this experiment is to determine variations in diel temperature change, inflow and outflow of groundwater into the stream, quantify interactions between vegetation and water, and understand the water balance and hydrologic processes. Experiments are being conducted in both the P301 meadow complex and at Long Meadow in Sequoia National Park.

Groundwater exchange in P301 meadow includes the installation of 24 wells and piezometers, 2 stilling wells, and 3 three sap rock piezometers to a depth of 205 to 500 cm. Evapotranspiration chamber measurements commenced in June 2010, continuing in Fall 2011 in order to understand ET throughout the growing season. Salt dilutions have commenced at the installed stilling wells to measure flow and establish a rating curve.

Activities in Long meadow, Sequoia NP began in 2007. Long Meadow is within the Wolverton area of the park. Research has focused on exploiting temperature as a hydrologic tracer using a distributed temperature sensor (DTS) and Tidbit temperature sensors, plus data from piezometers and observation wells. The DTS system includes a computer, two 1-km long fiber optic cables and a power source. The DTS deployment led to the observations of polymictic pool behavior in the meadow pools. This daily thermal stratification and nightly was further assessed in 2008 and 2009 using Hobo Tidbit temperature loggers, for vertical temperature profiles, and Radon-222 analysis.

In addition to temperature and geochemical tracer activities, evapotranspiration, ground water level, and pressure head measurements have been collected since 2008.

For additional information, contact Martha Conklin.

Geochemical and Geophysical Weathering Investigations

Spearheaded by colleagues at the University of Wyoming, researchers have been participating in a number of weathering studies using geochemical and geophysical approaches. Projects investigate long-term versus short-term rates of erosion (sediment basins and solute fluxes versus cosmogenic nuclides and regolith geochemistry), landscape evolution, “stepped topography” and the role of bare rock in shaping landscapes, the role of dust in pedogenesis and nutrient supply to the forests in and around the CZO (from isotopic tracers), and the origins of coarse sediment in streams (also from isotopic tracers).

Geophysical imaging of weathered layers at SSCZO has been studied over the past two summers to provide 2D and 3D knowledge of the subsurface. Methods of geophysical investigation include seismic refraction and resistivity. Tests on hypotheses include what controls the thickness of the subsurface (weathering and erosion), and how much water is stored in the subsurface (porosity versus depth).

Future studies focus on cosmogenic nuclide method development (10Be in magnetite), drilling and coring in partnership with DOSECC (Drilling, Observation and Sampling of the Earths Continental Crust).

For additional information, contact Clifford Riebe.

Wireless Sensor Networks

In the Fall of 2007 a 28-node network of sensors was deployed around the upper and lower met stations in Providence Creek Catchment P300 to capture spatial and temporal variations of snow depth, soil temperature and soil volumetric water content. On N-S aspects sensors were placed and under canopy, at the canopy drip edge, and in the open. In the Fall of 2008 a 50-node wireless embedded sensor network was deployed across varying aspects, elevations, and canopy covers in the P301 headwaters of Providence Creek. Over 300 sensors are now included in this deployment. For more information on the wireless sensor networks, see our Instruments section.

For additional information, contact Erin Stacy.

© Southern Sierra Critical Zone Observatory

© Southern Sierra Critical Zone Observatory

© Southern Sierra Critical Zone Observatory

© Southern Sierra Critical Zone Observatory

© Southern Sierra Critical Zone Observatory


SSCZO - Critical Zone Trees

The primary Critical Zone Tree in the Southern Sierra CZO is a White Fir (Abies concolor) that has been intensely instrumented with soil moisture, temperature, and matric potential sensors, snow depth, solar radiation, and sap flow sensors, resin nutrient collectors, tension lysimeters and time lapse photography.  The Southern Sierra CZO currently has three instrumented trees.

A photo gallery of the Critical Zone Trees can be found here.

SSCZO - Flux Towers

An eddy covariance flux tower is located near the top of the P301 watershed. Instruments collect data on temperature, relative humidity, and fluxes of carbon dioxide and water vapor to determine the physiological responses of the site (for example, how photosynthesis increases with light) and summed over a year to determine the carbon balance of a site (how much carbon it is gaining or losing). Three other flux towers have been instrumented at different elevations with the Sierras including the San Joaquin River, Soaproot, and Short Hair Creek.

This west-east transect spans elevation gradient from 400 m to 2700 m. The change in elevation is accompanied by a slight increase in precipitation, but the main change is a shift from rain-dominated precipitation to snow-dominated precipitation. The climatic shift plays out in other ways as well. At lower elevations, high temperatures and low water availability limit evapotranspiration by vegetation. Meanwhile, forest activity (evapotranspiration) at higher elevations is limited by cold winter temperatures. There is a sweet spot at middle elevations of yera-round evapotranspiration and forest activity.

Photo galleries of each flux tower are available: San Joaquin Experimental Range;  Soaproot SaddleProvidence subcatchment P301; and Short Hair Creek.

SSCZO - Instruments

Hundreds of instruments and sensors have been deployed in the primary SSCZO research site of the Providence Creek watershed as well as in Wolverton basin.  Additional SSCZO flux towers and instruments have also been installed at the San Joaquin Experimental Range, Soaproot Saddle, and Short Hair Creek.

Explore more photos of the intstuments and sensors used by SSCZO.

SSCZO - Water Balance Transect

Within the headwaters of the P301 catchment is a series of montane meadows. The P301 water balance transect is comprised of monitoring wells, piezometers, soil sensors, and meteorological sensors.

A photo gallery of the P301 water balance transect can be found here.