USGS Home - www.usgs.gov
Coastal and Marine Geology Program
Coastal & Marine Geology Program > Center for Coastal & Regional Marine Studies > Environmental Atlas of Lake Pontchartrain

Environmental Atlas of the Lake Pontchartrain Basin

Lake Pontchartrain Atlas Home
Lake Pontchartrain Atlas:
Preface
Table of Contents
Introduction
Environmental Overview
Environmental Status & Trends
Restoration
Physical Environments You are at the Physical Environments section of the Environmental Atlas of Lake Pontchartrain
Basin Geology
Biological Resources
Environmental Issues
Bibliography
Resources
Contributors
Acronyms
Contact:
Jack Kindinger
Physical Environments: Climate | Hurricane History | Circulation | Wave Climate | Relative Sea Level | Relative Sea Level Rise

Physical Environments - Wave Climate

Contributors: Peters, Beall, Buster

Wave climate is one of the primary factors controlling sediment transport, deposition and erosion in the coastal environment. The wave climate is defined as the average wave condition over a period of years based on wave height, period, direction, and energy. Wind speed and direction and nearshore bathymetry are the primary forcing mechanisms of wave climate in coastal regions. The changing characteristics of barrier islands, inlets, and the nearshore are dependent on and respond to several variables, including the wave climate and the sediment supply of the area. Daily perturbations, short-term fluctuations, and long-term cycles of wind and wave activity (including the effects of frontal passages and hurricanes) will be reflected in the morphology of the coastline. Figure 54 shows the location of two moored buoys in the Gulf of Mexico and Figure 55 is a photograph of Buoy 42007 located in the northern Gulf of Mexico, Figures 56 through 60 show examples of varying types of data used to forecast the wave and wind regime for the northern Gulf of Mexico.

Map showing the location of two moored buoys in the Gulf of Mexico. NDBC's Buoy 42007
Figure 54: Location of two moored data buoys in the Gulf of Mexico. Figure 55: NDBC's Buoy 42007 located in the northern Gulf of Mexico.
Average wave period of all waves during a 20-minute period.
Figure 56: Average wave period of all waves during a 20-minute period.
Image showing sea-level rise rates.
Figure 57: Dominant wave period is the period with the maximum wave energy.
Significant wave height is calculated as the average of the highest one-third of all of the wave heights during the 20-minute sampling.
Figure 58: Significant wave height is calculated as the average of the highest one-third of all of the wave heights during the 20-minute sampling.
Peak wind speed of a 5 to 8 second duration gust is measured during a two- or eight-minute period.
Figure 59: Peak wind speed of a 5 to 8 second duration gust is measured during a two- or eight-minute period.
Wind speed is averaged over an eight-minute period for buoys.
Figure 60: Wind speed is averaged over an eight-minute period for buoys.

Source: National Data Buoy Center web page (http://ndbc.noaa.gov)

« Previous | Next »


Coastal & Marine Geology Program > Center for Coastal & Regional Marine Studies > Environmental Atlas of Lake Pontchartrain

FirstGov.govemail Feedback [an error occurred while processing this directive]