330 likes | 491 Views
Freshwater flows to bays and estuaries. Paul Montagna George Ward University of Texas at Austin. PROBLEMS. SCIENTIFIC:. WHAT IS THE RELATION BETWEEN INFLOW AND THE ESTUARY ECOSYSTEM?. POLICY:. WHAT ARE THE SOCIETAL TRADE-OFFS BETWEEN POPULATION GROWTH AND ECOSYSTEM MAINTENANCE?.
E N D
Freshwater flows tobays and estuaries Paul MontagnaGeorge Ward University of Texas at Austin
PROBLEMS SCIENTIFIC: WHAT IS THE RELATION BETWEEN INFLOW AND THE ESTUARY ECOSYSTEM? POLICY: WHAT ARE THE SOCIETAL TRADE-OFFS BETWEEN POPULATION GROWTH AND ECOSYSTEM MAINTENANCE? REGULATORY: HOW DO WE IMPLEMENT THE AGREED POLICY AND ENSURE THAT IT WORKS?
SCIENCE E = f(Q) monitor Q (s,t) POLICY REGULATORY
HYDRODYNAMIC TRANSPORT WATERBORNECONSTITUENTS BIOLOGICALCOMMUNITIES (currents, mixing, water depths) (distribution & abundance of organisms) (water quality) CAUSE EFFECT
HYDRODYNAMIC TRANSPORT WATERBORNECONSTITUENTS BIOLOGICALCOMMUNITIES (currents, mixing, water depths) (distribution & abundance of organisms) (water quality) WARD MONTAGNA
RIVER ESTUARY OCEAN BOUNDARY ZONE
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
Sabine Lake Galveston Bay Matagorda Bay San Antonio Bay Aransas-Copano Bays Corpus Christi Bay Upper Laguna Madre-Baffin Bay Lower Laguna Madre
HYDRODYNAMIC TRANSPORT WATERBORNECONSTITUENTS BIOLOGICALCOMMUNITIES SOLIDS CURRENTS HYDRODYNAMIC TRANSPORT WATERBORNECONSTITUENTS BIOLOGICALCOMMUNITIES FLORA NUTRIENTS DENSITY HERBIVORES SALINITY MIXING CARNIVORES OTHERS
EXTERNAL (FORCING) VARIABLES EXTERNAL VARIABLES HYDRODYNAMIC TRANSPORT WATERBORNECONSTITUENTS BIOLOGICALCOMMUNITIES INTERNAL VARIABLES SOLIDS CURRENTS HYDRODYNAMIC TRANSPORT WATERBORNECONSTITUENTS BIOLOGICALCOMMUNITIES FLORA NUTRIENTS DENSITY HERBIVORES SALINITY MIXING CARNIVORES OTHERS
METEOROLOGY INFLOW LOADS INSOLATION MIGRATION OCEANSALINITY TIDES HYDRODYNAMIC TRANSPORT WATERBORNECONSTITUENTS BIOLOGICALCOMMUNITIES SOLIDS CURRENTS HYDRODYNAMIC TRANSPORT WATERBORNECONSTITUENTS BIOLOGICALCOMMUNITIES FLORA NUTRIENTS DENSITY HERBIVORES SALINITY MIXING CARNIVORES OTHERS
SCIENTIFIC STRATEGIES 1 - Model cause-and-effect linkages
SCIENTIFIC STRATEGIES 1 - Model cause-and-effect linkages 2 - Relate variables statistically
SCIENTIFIC STRATEGIES 1 - Model cause-and-effect linkages 2 - Relate variables statistically
METEOROLOGY INFLOW LOADS INSOLATION MIGRATION OCEANSALINITY TIDES HYDRODYNAMIC TRANSPORT WATERBORNECONSTITUENTS BIOLOGICALCOMMUNITIES SOLIDS CURRENTS HYDRODYNAMIC TRANSPORT WATERBORNECONSTITUENTS BIOLOGICALCOMMUNITIES FLORA NUTRIENTS DENSITY HERBIVORES SALINITY MIXING CARNIVORES OTHERS
METEOROLOGY INFLOW LOADS INSOLATION MIGRATION OCEANSALINITY TIDES HYDRODYNAMIC TRANSPORT WATERBORNECONSTITUENTS BIOLOGICALCOMMUNITIES SOLIDS CURRENTS HYDRODYNAMIC TRANSPORT WATERBORNECONSTITUENTS BIOLOGICALCOMMUNITIES FLORA NUTRIENTS DENSITY HERBIVORES SALINITY MIXING CARNIVORES OTHERS
METEOROLOGY INFLOW LOADS INSOLATION MIGRATION OCEANSALINITY TIDES HYDRODYNAMIC TRANSPORT WATERBORNECONSTITUENTS BIOLOGICALCOMMUNITIES SOLIDS CURRENTS HYDRODYNAMIC TRANSPORT WATERBORNECONSTITUENTS BIOLOGICALCOMMUNITIES FLORA NUTRIENTS DENSITY HERBIVORES SALINITY MIXING CARNIVORES OTHERS 1 - Model cause-and-effect linkages
METEOROLOGY INFLOW LOADS INSOLATION MIGRATION OCEANSALINITY TIDES HYDRODYNAMIC TRANSPORT WATERBORNECONSTITUENTS BIOLOGICALCOMMUNITIES SOLIDS CURRENTS HYDRODYNAMIC TRANSPORT WATERBORNECONSTITUENTS BIOLOGICALCOMMUNITIES FLORA NUTRIENTS DENSITY HERBIVORES SALINITY MIXING CARNIVORES OTHERS 2 - Relate variables statistically
TWO PRECEPTS Any assumed functional variation of a model represents a source of error. Any external variable not explicitly modeled represents a source of variance.
TWO (2) FACTS ABOUT TEXAS RAINFALL PRODUCED ALMOST ENTIRELY FROM DEEP CONVECTION DECLINES PRECIPITOUSLY FROM EAST TO WEST
TWO (2) FACTS ABOUT TEXAS RUNOFF SMALL AS A PROPORTION OF RAINFALL DECLINES EVEN MORE PRECIPITOUSLY FROM EAST TO WEST
TWO (2) FACTS ABOUT TEXAS STREAM FLOW FLASHY SUBSTANTIAL YEAR-TO-YEAR (& LONG-TERM) VARIABILITY
Guadalupe River at Victoria daily flow 30-day sliding mean
2.7 3.9 8.9 14.3 years
Freshwater flows tobays and estuaries Paul MontagnaGeorge Ward University of Texas at Austin