SAN LORENZO LAGOON: HOW DOES IT WORK? 2016 State of the San Lorenzo River Symposium Dr. David Revell revellcoastal@gmail. com 5/21/2016
CONCEPTUAL LAGOON FUNCTION LAGOON a stretch of salt water separated from the sea by a low sand bank (or coral reef) Closed Mouth – Lagoon Full Open Mouth – Tidal Conditions Open Mouth – Perched (muted tides) Figure from ESA PWA Closed Mouth
SALINITY Amount of salt in the water • Salt Water is heavier than freshwater • Salt water sinks and freshwater floats • Creates different types of habitat conditions DISSOLVED OXYGEN (DO) Amount of oxygen in the water • Needed by fish and other aquatic organisms • Without oxygen aquatic organisms suffocate
2002 - 2012 Water Quality Data from 2 nd Nature, Wave Data from ESA PWA
HIGH STREAM FLOW
LOW STREAM FLOW
NO STREAM FLOW
IMPACT OF THE HARBOR
IMPACT OF THE HARBOR
IMPACT OF THE HARBOR
SEABRIGHT BEACH FILLING
SEABRIGHT BEACH 1955
1953 SEABRIGHT BEACH
MARCH 2012
08/29/2014
09/08/2014
11/10/2014
11/12/2014
11/18/2014
11/19/2014
11/21/2014
11/22/2014
11/23/2014
11/29/2014
12/03/2014
12/04/2014
12/05/2014
12/06/2014
12/08/2014
12/11/2014
12/12/2014
12/22/2014
Close-up: 2007 Low Waves
Close-up: 2005 High Waves
HOW DOES IT WORK • Waves strongly influence water level and salinity in closed lagoon • Beach sill typically mutes tide below 0 -3’ NGVD • Bottom temperature high until lagoon freshens • Lagoon does freshen some during closure (2 - 4 weeks) • Bottom DO generally low after mouth closure • Wave overwash increases DO at bottom Beach elevation ranges from 6. 5 to 9’ (NGVD) during closure Beach crest is highest in front of the inlet Thalweg depth varies widely from beach to train trestle Everything will change in the future