The conceptual model for Southern Sierra CZO involves understanding varaibles along three axes: i) elevation gradient, representing alo gradients in climate, regolith properties, soils, ecosystems, and associated processes, ii) spatial scales, and iii) temporal scales. We use a variety of numerical models, as reflected in pulications and the work plan.
The conceptual model is presented in four panels, illustrated at right, and accompanying text. The panels are: Conceptual model, Processes, Spatial scales and Temporal feedbacks.
The REHSSys panel is linked to a description of one numerical model we are using, the Regional Hydro-Ecologic Simulation System.
Refer to the Conceptual and Numerical models pages for details.
FEATURED
08 Jul 2019 - CZO will end Nov 2020, succeeded by the “CZ Collaborative Network”. Let’s explore how the CZ community can build upon the CZOs via new NSF proposals.
12 Sep 2018 - Two postdoctoral scholar positions and multiple MS or PhD research assistantships are currently available at the University of California, Merced....
07 Sep 2018 - Recent activities and findings, funding opportunities, upcoming events, and other updates
17 Jul 2018 - Recent activities and findings, funding opportunities, upcoming events, and other updates
27 May 2018 - Recent activities and findings, funding opportunities, upcoming events, and other updates
17 Jan 2018 - Recent activities and findings, funding opportunities, upcoming events, and other updates
Conceptual model diagram
Southern Sierra elevation and climate gradient, with spatial scaling and temporal feedbacks
Conceptual model processes and implications
Drivers of critical zone development must be understood together to address science questions and understand implications
Regional Hydro-Ecologic Simulation System
A spatially distributed dynamic model of coupled eco-hydrologic processes.
Conceptual model—spatial scales
Variables important for spatial scaling of vegetation differences, water cycles and material fluxes
Feedbacks across time
Variables important for temporal feedbacks of vegetation differences, water cycles and material fluxes