Measured and derived wave parameters from data collected by a wave monitoring buoy anchored at Bilinga. For more information, please refer to www.qld.gov.au/waves. Field names are; Hs - Significant wave height, an average of the highest third of the waves in a record (26.6 minute recording period). Hmax - The maximum wave height in the record. Tz - The zero upcrossing wave period. Tp - The peak energy wave period. Peak Direction - Direction (related to true north) from which the peak period waves are coming from. SST - Sea Surface Temperature as measured by a sensor embedded in the hull of the buoy.

Measured and derived wave parameters from data collected by a wave monitoring buoy anchored at Emu Park. For more information please refer to www.qld.gov.au/waves. Field names are; Hs - Significant wave height, an average of the highest third of the waves in a record (26.6 minute recording period). Hmax - The maximum wave height in the record. Tz - The zero upcrossing wave period. Tp - The peak energy wave period. Peak Direction - Direction (related to true north) from which the peak period waves are coming from. SST -Sea Surface Temperature as measured by a sensor embedded in the bottom of the hull of the buoy.

Measured and derived wave parameters from data collected by a wave monitoring buoy anchored at Bundaberg. For more information please refer to www.qld.gov.au/waves. Field names; Hs- Significant wave height, an average of the highest third of the waves in a record (26.6 minute recording period). Hmax - The maximum wave height in the record. Tz - The zero up-crossing wave period. Tp- The peak energy wave period. Direction not captured.

Predicted water level heights at Skardon River Offshore at regular time intervals.

In July 1985 the Division of Oceanography embarked on a wave observation program with the deployment of two "Waverider" buoys in the Southern Ocean near Cape Sorell on the west coast of Tasmania. Data were collected from moored Waverider Buoys deployed for various periods in Tasmanian coastal waters off Cape Grim, Cape Sorell (100m), Cape Sorell (50m) and Storm Bay. These observations are used to assess both typical and extreme sea states at these sites and for estimating spatial, seasonal and interannual variations in wave conditions in the Tasmanian region. The program concluded in December 1993 when the Storm Bay buoy ceased operation. There are two distinct datasets: a) Derived statistical data is available on-line for the seven locations mentioned in "Wave Climate Measurements in the Southern Ocean." b) Sample burst data for each of (possibly) nine locations. NOTES: All instruments used, and a copy of the data obtained during this program were sent to the Bureau of Meteorology. The Marine Observation Unit at the Bureau (marine_obs@bom.gov.au) may be able to provide additional information. The data files in this collection are not in a Datacente supported format and no assurances are given as to the accuracy of data, or of the locations implied by the data file names. The CSIRO Waverider program has not been continued.

Predicted high and low water level heights at Skardon River Offshore.

Measured and derived wave parameters from data collected by a wave monitoring buoy anchored at Gladstone. This site is jointly operated by the Department of Environment and Science and the Gladstone Ports Corporation. For more information please refer to www.qld.gov.au/waves. Field names; Hs - Significant wave height, an average of the highest third of the waves in a record (26.6 minute recording period). Hmax - The maximum wave height in the record. Tz - The zero upcrossing wave period. Tp - The peak energy wave period. Peak Direction - Direction (related to true north) from which the peak period waves are coming from. SST - Sea surface temperature as measured by a sensor embedded in the bottom of the hull of the buoy.

Coastal marshes are highly dynamic and ecologically important ecosystems that are subject to pervasive and often harmful disturbances, including shoreline erosion. Shoreline erosion can result in an overall loss of coastal marsh, particularly in estuaries with moderate- or high-wave energy. Not only can waves be important physical drivers of shoreline change, they can also influence shore-proximal vertical accretion through sediment delivery. For these reason, estimates of wave energy can provide a quantitative measure of wave effects on marsh shorelines. Since wave energy is difficult to measure at all locations, scientists and managers often rely on hydrodynamic models to estimate wave properties at different locations. The Wave Exposure Model (WEMo) is a simple tool that uses linear wave theory to estimate wave energy characteristics for enclosed and semi-enclosed estuaries(Malhotra and Fonseca, 2007). The interpretation of hydrodynamic models is improved if model results can be validated against measured data. The data presented in this publication are input and validation data for modeled and observed mean wave height for two temporary oceanographic stations established by the U.S. Geological Survey (USGS) in the Grand Bay National Estuarine Research Reserve, Mississippi.