Ch.13 World Wave Climate Ch.14 Forecasting the Waves
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Transcript of Ch.13 World Wave Climate Ch.14 Forecasting the Waves
Ch.13 World Wave Climate
Ch.14 Forecasting the Waves Science of Forecasting Waves
GNM 1136Mr. Werner
What do you want to know about your destination before you travel there?◦ Surf Consistency◦ Temperatures (land and water)◦ Wind Patterns◦ Animal Life (sharks, jellies, etc…◦ Type of Break (reef, rocks, sand, etc…)◦ Localism◦ Language Barriers◦ Lodging
Questions to Consider
Satellites – radar altimetry Article Link
Wave Measurements from Space
When is the North Atlantic more active? South Pacific? (fig.13.1, 13.2) How do these maps relate to surfable wave
heights?◦ Why are the two ocean basins so different?
Challenge
Hawaii Europe Mediterranean Africa Indian Ocean East Asia Australia New Zealand
North Pacific North America Caribbean Mexico/Central
America South America S. Pacific Islands
Wave Climate Zones
Biggest Waves on Earth? (Fig. 13.3) World’s Biggest Tsunami Rogue Wave Observations off the US West C
oast New York Times Bermuda Triangle – National Geographic
Video
Wave-Current Interaction
Ch.14 Forecasting the Waves
Derived from multiple mathematical models◦ Wind = atmospheric calculations – layers◦ Waves = grid system
Computer calculates predictions every 20 minutes for approximately 10 days = a model “run”
Each calculation builds off of the previous one. Done twice a day. Smooth color lines are used to differentiate
between wave heights. Wave model is highly dependant on Wind model.
About Wave Models
Significant wave height – Hs or H1/3 = average height of 1/3 of all the waves
Significant Period – Ts – average period of about 10-15 successive prominent waves
Peak Period – period on spectrum that contains the most energy. Similar to Ts.
Wave height and period examples
Wave Height & Period
Current data – not predicted (Table 14.1) Look at trends (36 hours) – Multiple uses Delaware Buoy Will the wave height be the same on the
beach?
Buoy Reports
Surface weather analysis chart Lab Activity
Understanding Weather Maps
How to Read a Wave Model NOAA – Understanding Wavewatch III Wavewatch III Current Model –WW3 http://stormsurf.com/
Wavewatch III Model
Wave Models can be very tricky because of local bathymetric effects.
Do not rely entirely on one model – combine all models together for the best results.
Look at local winds, tides, period and direction
Be Careful
“The wave models provide an easy to read analysis and forecast of sea state conditions two times per day for 3 days (for the NOAA Suite) and one week (for the FNMOC Suite). The precaution about using wave models for swell prediction is doubly important. It's a model that uses a model to make a prediction. That is, the wave model uses an atmospheric model to determine the future state of the atmosphere, then makes a prediction of how the atmosphere will affect the water under it. So there's lot's of room for error.”
Quote from Stormsurf.com