Steve,
Theres nothing in public domain to my knowledge but the NOAA Wave Watch III model that virtually all automatad buoy data draws from is only the unclassified version of what the US Navy uses. I spent a lot of time operating on submarines out of Hawaii based in Pearl and the models we had access to for planning purposes were insane. As you know, as surfers we are really only concerned with what is happening in the top 10 metres of the water column and WW3 addresses that on a global scale. For my site we needed buoy data to cover all of our 4000 surf spots so we came up with our own algorithm that draws directly from WW3 GRIB data. It's difficult to turn what is essentially an open water forecasting tool into something that is accurate nearshore but if you want one algorithm to cover the entire world then you have to accept some limitations.
The truth is that the final size and period of a breaking wave is the product of what is happening in up to 1000m of water column. Iv'e been at 200M in large storms and still felt the sub corkscrewing through the water. Off Hawaii where open ocean swells are ramping up from the 1000m to the 100m contour extremely quickly the effect is enormous. Once at 100M we lost 30M in depth in a fraction of a second. I can only describe it as a feeling of underwater turbulence, similar to when a plane drops without warning. What it was was an 'internal wave' within the water column. So if your in 150M of water at 100M and suddenly you loose 30M in depth while you are doing 15 knots and the bottom is lava or basalt...the holes in the swiss cheese start to line up pretty quickly. Anyway so thats why the USN put a lot of work into region specific models that account for every effect down to 1000M in depth, its like crunching an entire global model just for the Hawaiian Islands. When we came in after the internal wave incident I went up to forecasting and the guy there said - "how'd that internal wave treat ya off Hilo?" I asked him how he knew and he lent out and patted an enormous grey box that was basically a stripped down CRAY supercomputer with an Atari sticker on it as a joke and he said "she told me" He had actually forecast it with the model.
Side benefit was that this model was the most accurate surf forecasting tool for Hawaii you could ever imagine. I took great pleasure in using US tax payers funds by printing out forecasts before I decided where to go for surf and it was accurate to the inch. An interesting feature was that you could reverse model the size of the surf you were after to see what weather pattern would create it. Like all good US military planning tools it would have a 'bodycount' on the bottom of the screen to show you how severe the storm damage would be to create the surf you were after. I modelled 30, 50, 100 and even 1000 year storm events on the North Shore. The 1000 year storm event created 60 foot waves at Pipeline and forecasted 120 feet waves cresting at Waimea before 'breaking down' due to surface tension. Unfortunately in that model, most of the population of Haleiwa didnt make it. :?
Anyway, there are a lot of good forecasters on this site, you included but my point is that from experience, with larges storm events in the Tasman, often the total bathymetry can put a very substantial wobble into the final size of nearshore waves in NSW, particularly in swells with a strong southerly vector. These swells have to navigate around and between a very complex connection of sub surface features that stretch all the way from the Lord Howe Rise to Eastern Victoria and to my knowledge there is no known model that takes due account of all of this for the Australian station
, you just have to apply it's effect as a fudge factor based on experience.