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 contributing 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 affects of frontal passages and hurricanes) will be reflected in the morphology of the coastline. Figure 61 shows the location of two moored buoys in the Gulf of Mexico and Figure 62 is a photograph of Buoy 42003 located in the central Gulf of Mexico. Figures 63 through 67 show examples of varying types of data used to forecast the wave and wind regime for the central Gulf of Mexico.

Map showing the location of two moored buoys in the Gulf of Mexico. NDBC's Buoy 42003
Figure 61: Location of two moored data buoys in the Gulf of Mexico. Figure 62: NDBC's Buoy 42003 located in the central Gulf of Mexico.
Average wave period 7/77-12/93.
Figure 63: Average wave period of all waves during a 20-minute period.

Dominant wave period 10/7-12/93.
Figure 64: Dominant wave period is the period with the maximum wave energy.

Significant wave height 7/77-12/93.
Figure 65: 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 gust 1/80-12/93.
Figure 66: Peak wind speed of a 5 to 8 second duration gust is measured during a two- or eight-minute period.

Average wind speed 11/76-12/93.
Figure 67: Wind speed is averaged over an eight-minute period for buoys.

Source: National Data Buoy Center web page (http://seaboard.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]