Chapter 1 Minimum Flows and Levels - Southwest Florida Water ...
Chapter 1 Minimum Flows and Levels - Southwest Florida Water ...
Chapter 1 Minimum Flows and Levels - Southwest Florida Water ...
You also want an ePaper? Increase the reach of your titles
YUMPU automatically turns print PDFs into web optimized ePapers that Google loves.
<strong>Chapter</strong> 4 Technical Approach for Establishing<br />
<strong>Minimum</strong> <strong>Flows</strong> <strong>and</strong> <strong>Levels</strong> for the Upper Braden River<br />
4.1 Overview<br />
A number of methods were used to determine the minimum flow requirements for<br />
the upper, fresh water segment of the Braden River. The approach outlined for<br />
the river involves identification of a low flow threshold <strong>and</strong> development of<br />
prescribed flow reductions for periods of low, medium <strong>and</strong> high flows (Blocks 1, 2<br />
<strong>and</strong> 3). The low flow threshold is used to identify a minimum flow condition <strong>and</strong><br />
is expected to be applicable to river flows throughout the year. The prescribed<br />
flow reductions are based on limiting potential changes in aquatic <strong>and</strong> wetl<strong>and</strong><br />
habitat availability that may be associated with changes in river flow during<br />
Blocks 1, 2 <strong>and</strong> 3.<br />
4.2 Transect Locations <strong>and</strong> Field Sampling of Instream <strong>and</strong><br />
Floodplain Habitats<br />
The Braden River is the largest tributary to the Manatee River (Trommer et al.<br />
1999) <strong>and</strong> is a source of freshwater supply for the City of Bradenton, <strong>Florida</strong>. The<br />
river flows for approximately 22 miles in south-central Manatee County <strong>and</strong><br />
northern Sarasota County to the Manatee River <strong>and</strong> includes an 83 square mile<br />
watershed.<br />
The river segment delineated for MFLs determination was confined to areas<br />
upstream of the USGS Braden River at Linger Lodge near Bradenton gage site,<br />
which is located approximately 0.5 miles east of Interstate 75. This river<br />
segment includes 8.6 miles of relatively straight, naturally incised channel that<br />
drains 26 square miles of headwaters that are unaffected by backwater effects<br />
from Bill Evers Reservoir (Figure 4-1). Bill Evers Reservoir was created in 1985<br />
through excavation of Ward Lake to increase storage capacity in the basin to 1.4<br />
billion gallons of water. Permanent backwater conditions extend upstream from<br />
the reservoir dam for approximately six miles <strong>and</strong> the lower reaches of its<br />
tributaries are also affected.<br />
Field sampling in support of MFLs development for the upper Braden River<br />
involved characterization of cross-sectional physical, hydrologic <strong>and</strong> habitat<br />
features. Four types of cross-sectional information were collected, including data<br />
used for HEC-RAS modeling, Physical Habitat Simulation (PHABSIM) modeling,<br />
instream habitat assessment, <strong>and</strong> floodplain vegetation/soils assessments.<br />
HEC-RAS cross-sections were established to develop flow <strong>and</strong> inundation<br />
statistics for the other cross-section sites based on existing flow records for the<br />
4-1