Hypoxia modeling in Corpus Christi Bay using a Hydrologic Information System

By Ernest Sin Chit To, CRWR

 

Contents

1.0         Introduction.

2.0         Background.

3.0         Hypothesis for hypoxia.

4.0         Investigation of gravity currents.

5.0         Selection of study area.

6.0         Research progress to date.

6.1         Data harvesting in Corpus Christi Bay using HydroGET and ArcHydro II

6.2         A three-dimensional geostatistical model for estimating salinity in Corpus Christi Bay.

6.3         Using space-time interpolation to characterize the movement of gravity currents in Corpus Christi Bay 

7.0         References.

1.0      Introduction

The ultimate goal of hydrological information systems (HIS) is to help scientists do better science.  The hypoxia problem in Corpus Christi Bay is being used as a case study to show how HIS can help researchers gain scientific insights into environmental phenomena.  This web site explains the background of this research and the progress of research activities.

2.0      Background

Hypoxia is a common phenomenon found in estuarine systems.  It occurs when dissolved oxygen is depleted below ~2 mg/L    thereby stressing resident aquatic species and benthic organisms. In Corpus Christi Bay in south Texas, hypoxia is often correlated with the occurrence of salinity-induced density stratification of the water column.  Typically this happens in summer when temperature and evaporation are high and precipitation is low (Ritter and Montagna, 1999).  Density stratification is also suspected to be enhanced by existing hypersaline water inflows to Corpus Christi Bay from adjacent waters, such as Laguna Madre and Oso Bay (David and Hodges, 2006).