Physical Process Variables

The relative sea-level change variable is derived from the increase or decrease in annual mean water elevation over time as measured at tide gauge stations along the coast. The rate of sea-level rise for Padre Island, TX is 3.44 +/- 0.56 mm/yr based on 37 years of data (Zervas, 2001). This variable inherently includes both eustatic sea-level rise as well as regional sea-level rise due to isostatic and tectonic adjustments of the land surface. Relative sea-level change data are a historical record, and thus only portray the recent sea-level trend (<150 years). Relative sea-level rise for Padre Island falls within very high vulnerability based on water elevation data at South Padre Island and Port Isabel.

Mean significant wave height is used here as a proxy for wave energy which drives the coastal sediment budget. Wave energy is directly related to the square of wave height:

E = 1/8 ρgH²

where E is energy density, H is wave height, ρ is water density and g is acceleration due to gravity. Thus, the ability to mobilize and transport coastal sediments is a function of wave height squared. In this report, we use hindcast nearshore mean significant wave height data for the period 1976-95 obtained from the U.S. Army Corps of Engineers Wave Information Study (WIS) (see references in Hubertz and others, 1996). The model wave heights were compared to historical measured wave height data obtained from the NOAA National Data Buoy Center to ensure that model values were representative of the study area. For Padre Island, mean significant wave heights are between 0.8 and 1.0 m, which represents low and moderate vulnerability, respectively.

Tidal range is linked to both permanent and episodic inundation hazards. Tide range data were obtained from NOAA/NOS for a Gulf tide gauge at Corpus Christi and Brazos Santiago Pass. All of Padre Island is classified as very high vulnerability (< 1m) with respect to tidal range.