The symposium was an in-person, free and open to the public event hosted on Saturday, December 7, 2024 9.30 am, 112 Bauer Wurster Hall, UC Berkeley.

PROGRAM:

9:30: Welcome by Zan Rubin (Balance Hydrologics and UC Berkeley)
Keynote Presentation by Erin Bray (San Francisco State University)
River mechanics for river restoration: How rivers warm and river rocks round (see bio
and abstract below)
 
10:30-12:00 Student Presentations
 
The Hydrologic and Geomorphic Response to Beaver Arrival on Rush Creek
 
Contrasting Goals and Outcomes: Comparing Restoration on Codornices and Wildcat
Creeks
 
A Decade Later: The Impacts of the Eden Landing Ecologic Reserve
 
Lost in Time: Evaluating step pool habitat two decades after restoration on Codornices
Creek
 
Assessing the Role of Marsh Restoration on Sedimentation, Flood Management, and Sea-
Level Rise: A Case Study of Walnut Creek
 
Cows and Water: How Grazing Alters our Waterways
 
12:00- 12:30 Concluding Panel: Reflections from Erin Bray (San Francisco State) and
Tami Church (US Army Corps of Engineers)

Keynote Talk Abstract:
River mechanics for river restoration: How rivers warm and river rocks round
Along many rivers dams trap sediment and water released from the dam is cool and clear.
Downstream of the dam, temperature variability is controlled by climate that warms or
cools the water, the flow magnitude, and spectral properties of the water and the river’s
bed sediment. Separately, the grain size and shape of sediment on the bed is controlled by
the sediment supplied from hillslopes and fluvial sources, and the flow-driven abrasion
that contributes to particles getting smaller and rounder as they are transported along
stream. We developed a numerical river energy balance model to understand the controls
to river temperature. The Fluvial Energy Balance Model (FLUVIAL-EB) couples a full-
spectrum radiation balance model with turbulent heat fluxes, bed conduction, advection,
diffusion, and a 1D channel flow model over the length of the river, and is applied to
investigate temperatures along the San Joaquin River. We show that variations in the river temperature are sensitive to changes in the albedo of the sediment on the riverbed,
especially at smaller discharges and along abrupt gravel-to-sand transitions from dark
gravel to bright sand. A separate laboratory study uses a rock tumbler and angular rocks
sourced from nearby hillslope environments to investigate how river rocks round as they
tumble along river distances, to understand whether grain size reductions as opposed to
rounding is the dominant factor leading to sediment mass lost during abrasion. These two
studies highlight the importance of geomorphic processes on river sediment and
temperature, both of which support salmon spawning habitat.
 
Keynote Speaker:
Erin Bray is an Assistant Professor in the School of the Environment at San Francisco
State University (formerly the Department of Earth and Climate Sciences) where she leads
the Rivers Lab. Her research focuses on hydrology and fluvial geomorphology, with
emphasis on river processes and river restoration. Previously, she was an Assistant
Professor at California State University Northridge where she served as the Co-Lead for
the Water Science Program. Dr. Bray was a Postdoctoral Fellow at the University of
California, Berkeley, and the University of California, Santa Barbara, supported under a
fellowship from the Delta Stewardship Council. She received her Ph.D. from the
University of California, Santa Barbara, her M.A. from Brown University, and her B.S.
from Cornell University. Dr. Bray’s research focuses on hydrology and fluvial
geomorphology, with an emphasis on river processes, river restoration, and water
resources management. She has developed a model that, together with field measurements
and climate data, can be used to study impacts of flow releases from dams and climate on
the energy balance and water temperature of rivers. She also conducts in-situ field
measurements of saturated hydraulic conductivity to better understand the impacts of
sediment transport, sediment permeability, and flow on patterns of hyporheic exchange,
and how those patterns generate and sustain physical processes that support salmon
spawning habitat.