The Buoys Light Up: The wonderful Directional Spectra

Swellnet Analysis

The Buoys Light Up: The wonderful Directional Spectra

Swellnet Analysis
Stu Nettle

Rather than the traditional X-Y line graph that can only chart one swell at a time, the Directional Spectra is a 360 degree screen that registers every swell in the water by its direction, its energy, and its period. This represents a significant leap forward. Whereas the line graph could only plot the most dominant swell in the water, the Directional Spectra chronicles multiple swells.

Buoys Follow One Direction

Swellnet Analysis

Buoys Follow One Direction

Swellnet Analysis
Craig Brokensha

Victoria's Surf Coast is uniquely positioned with a broad swell window to the southwest, however incoming swells are refracted as they round Cape Otway. This narrows the apparent swell direction at the coast, so when viewed from shore the majority of swells appear to arrive from the south. So how can you tell if there's a westerly swell or a southerly swell running through Bass Strait if they all appear to be arriving from a similar direction at the coast?

Making sense of Evan

Swellnet Analysis

Making sense of Evan

Swellnet Analysis
Stu Nettle

The swell from Evan was a true cyclone swell, one that was generated in the core of a severe, slow moving tropical cyclone, and yet it was nothing like a classic cyclone swell. The reason Evan won't be remembered that way is because it formed in isolation. Despite spending a week in the far reaches of our swell window and wreaking havoc on Samoa and Fiji, Evan lacked the associated weather features required to create classic cyclone swell conditions.