multiple states in coastal lagoons and estuaries next steps toward understanding the lagoons of the...
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Multiple States in Coastal Lagoons and Estuaries
Next Steps Toward Understanding the Lagoons of the Yaqui ValleyNext Steps Toward Understanding the Lagoons of the Yaqui Valley
Arnoldo Valle-LevinsonArnoldo Valle-Levinson S. MonismithS. Monismith Juan DelgadoJuan Delgado Esther CruzEsther Cruz Bob ChantBob ChantCtr. for Coastal Physical Oceanogr. Stanford University ITMAR Guaymas CECARENA RutgersOcean, Earth and Atmos. Sci. Dept. Guaymas UniversityOld Dominion University New BrunswickNorfolk, Virginia N.J.
Inverse Estuary
Classical EstuaryLooking into the lagoon
Red = outflow
Blue = inflow
Guaymas Bay
OUT
OUTOUT
IN
IN
Mean Flow at Transect 4
red is inflow; blue is outflow (looking seaward)
NeapTides
Interface slope, spring tides ~ 2.5e-03 (25 m in 10 km)
Interface slope, neap tides ~ 2.0e-03 (18 m in 9 km)
Distance from Transect Origin (km)
WetSeason:Classical
DrySeason:Inverse
Importance:
Water and Soil(?) Quality
Climate Variability
OUT
OUT
IN
IN
Conservation of Salt and Heat
Relative influence of salinity and temperature on density gradients
Q
Freshwater
Precipitation
Outflow
Inflow
Se, Te
So, To
Heating
CLASSICAL
Q
Freshwater
Evaporation
Outflow
Inflow
Se, Te
So, To
Cooling
INVERSE
Relative influence of salinity and temperature on density gradients
Salinity influence
Temperature influence
Net influence
Q
In reality: kQ
Salinity influence
Temperature influence
Net influence
Q
T mode
S mode
Multiple states --- Stommel Transitions
Salinity influence
Temperature influence
Net influence
Q
Critical response for multiple states
qQ 10
WDgQ 23
41
LWDg
Q
12
4
Guess for Tobari and Lobos
Do Yaqui Valley lagoons/estuaries show ‘Stommel Transitions’?
Implications for water and soil quality…
Does causeway prevent INVERSE conditions?
What is the time scale of the Transitions?
Natural laboratory to examine climate variations
Are the systems in the Yaqui Valley more VULNERABLE to drought?