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Freshwater flows to bays and estuaries Paul Montagna George Ward University of Texas at Austin
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PROBLEMS SCIENTIFIC: POLICY: REGULATORY: WHAT IS THE RELATION BETWEEN INFLOW AND THE ESTUARY ECOSYSTEM? WHAT ARE THE SOCIETAL TRADE-OFFS BETWEEN POPULATION GROWTH AND ECOSYSTEM MAINTENANCE? HOW DO WE IMPLEMENT THE AGREED POLICY AND ENSURE THAT IT WORKS?
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SCIENCE POLICY REGULATORY E = f(Q) Q(s,t) monitor
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HYDRODYNAMIC TRANSPORT (currents, mixing, water depths) WATERBORNE CONSTITUENTS BIOLOGICAL COMMUNITIES (water quality) (distribution & abundance of organisms) CAUSEEFFECT
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HYDRODYNAMIC TRANSPORT (currents, mixing, water depths) WATERBORNE CONSTITUENTS BIOLOGICAL COMMUNITIES (water quality) (distribution & abundance of organisms) WARDMONTAGNA
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OCEAN RIVER ESTUARY BOUNDARY ZONE
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ESTUARIES transitional systems, between freshwater and marine hydrography and chemistry governed by both terrestrial and marine controls terrestrial controls: freshwater influxes, flooding & inundation, runoff and inflow loads (sediment, nutrients, pollutants), and atmospheric deposition marine controls: tides, waves, non-astronomical sea-level variations, marine storms, salinity, and littoral sediment influx predominance of these factors depends upon position in estuary: pronounced environmental gradients extreme time variability in estuary
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Sabine Lake Galveston Bay Matagorda Bay San Antonio Bay Aransas-Copano Bays Corpus Christi Bay Upper Laguna Madre- Baffin Bay Lower Laguna Madre
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HYDRODYNAMIC TRANSPORT WATERBORNE CONSTITUENTS BIOLOGICAL COMMUNITIES WATERBORNE CONSTITUENTS HYDRODYNAMIC TRANSPORT CURRENTS DENSITY MIXING SOLIDS NUTRIENTS SALINITY OTHERS FLORA HERBIVORES CARNIVORES
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HYDRODYNAMIC TRANSPORT WATERBORNE CONSTITUENTS BIOLOGICAL COMMUNITIES WATERBORNE CONSTITUENTS HYDRODYNAMIC TRANSPORT CURRENTS DENSITY MIXING SOLIDS NUTRIENTS SALINITY OTHERS FLORA HERBIVORES CARNIVORES INTERNAL VARIABLES EXTERNAL VARIABLESEXTERNAL (FORCING) VARIABLES
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HYDRODYNAMIC TRANSPORT WATERBORNE CONSTITUENTS BIOLOGICAL COMMUNITIES WATERBORNE CONSTITUENTS HYDRODYNAMIC TRANSPORT CURRENTS DENSITY MIXING SOLIDS NUTRIENTS SALINITY OTHERS FLORA HERBIVORES CARNIVORES OCEAN SALINITY INFLOW TIDES METEOROLOGY LOADS INSOLATION MIGRATION
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1 - Model cause-and-effect linkages SCIENTIFIC STRATEGIES
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1 - Model cause-and-effect linkages 2 - Relate variables statistically
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SCIENTIFIC STRATEGIES 1 - Model cause-and-effect linkages 2 - Relate variables statistically
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HYDRODYNAMIC TRANSPORT WATERBORNE CONSTITUENTS BIOLOGICAL COMMUNITIES WATERBORNE CONSTITUENTS HYDRODYNAMIC TRANSPORT CURRENTS DENSITY MIXING SOLIDS NUTRIENTS SALINITY OTHERS FLORA HERBIVORES CARNIVORES OCEAN SALINITY INFLOW TIDES METEOROLOGY LOADS INSOLATION MIGRATION
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HYDRODYNAMIC TRANSPORT WATERBORNE CONSTITUENTS BIOLOGICAL COMMUNITIES WATERBORNE CONSTITUENTS HYDRODYNAMIC TRANSPORT CURRENTS DENSITY MIXING SOLIDS NUTRIENTS SALINITY OTHERS FLORA HERBIVORES CARNIVORES OCEAN SALINITY INFLOW TIDES METEOROLOGY LOADS INSOLATION MIGRATION
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HYDRODYNAMIC TRANSPORT WATERBORNE CONSTITUENTS BIOLOGICAL COMMUNITIES WATERBORNE CONSTITUENTS HYDRODYNAMIC TRANSPORT CURRENTS DENSITY MIXING SOLIDS NUTRIENTS SALINITY OTHERS FLORA HERBIVORES CARNIVORES OCEAN SALINITY INFLOW TIDES METEOROLOGY LOADS INSOLATION MIGRATION 1 - Model cause-and-effect linkages
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HYDRODYNAMIC TRANSPORT WATERBORNE CONSTITUENTS BIOLOGICAL COMMUNITIES WATERBORNE CONSTITUENTS HYDRODYNAMIC TRANSPORT CURRENTS DENSITY MIXING SOLIDS NUTRIENTS SALINITY OTHERS FLORA HERBIVORES CARNIVORES OCEAN SALINITY INFLOW TIDES METEOROLOGY LOADS INSOLATION MIGRATION 2 - Relate variables statistically
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Any assumed functional variation of a model represents a source of error. Any external variable not explicitly modeled represents a source of variance. TWO PRECEPTS
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Hydrology of Texas estuaries
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TWO (2) FACTS ABOUT TEXAS RAINFALL PRODUCED ALMOST ENTIRELY FROM DEEP CONVECTION DECLINES PRECIPITOUSLY FROM EAST TO WEST
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Isohyets in inches/year
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TWO (2) FACTS ABOUT TEXAS RUNOFF SMALL AS A PROPORTION OF RAINFALL DECLINES EVEN MORE PRECIPITOUSLY FROM EAST TO WEST
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RUNOFF / RAINFALL
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TWO (2) FACTS ABOUT TEXAS STREAM FLOW FLASHY SUBSTANTIAL YEAR-TO-YEAR (& LONG-TERM) VARIABILITY
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Guadalupe River at Victoria daily flow 30-day sliding mean
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2.73.98.914.3 years
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Mid-Galveston Bay salinity versus Trinity River flow
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Freshwater flows to bays and estuaries Paul Montagna George Ward University of Texas at Austin
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