Brisk westerly winds and a complex low pressure gyre in the Tasman Sea, with multiple cold fronts and a deep S’ly fetch of gales extending down to 55S have ushered in the first day of Winter.
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Another dynamic week ahead but a bit more straightforwards in the sense that all the incoming swell will be from the S - once the current E swell pulse peters out through tomorrow.
Right on cue, as head into the first week of winter, a nice cold outbreak and blast of W’ly winds with accompanying S’ly swells is headed our way.
Synoptic pattern still has a ground-hog day feel to it, with a large, slow moving high inching it’s way across the Tasman and a coastal trough lying parallel to almost the entire East Coast. Change is on the way though.
Flukey swells from the S and light winds this week, with more energy from the E/NE later in the week
Sub-tropical troughs and the remnants of TC Gina near New Caledonia are maintaining a deep E’ly flow through the Coral Sea while the last in a series of powerful cold fronts are now sweeping up past the South Island of New Zealand with small S to SSE swell pulses to come over the next couple of days from this source.
The frontal progression responsible for the S swell pulses over the last couple of days is now on the New Zealand side of the Tasman, with a large high approaching Tasmania setting up a firm ridge along the coast.
A series of cold fronts with embedded troughs are now steaming into the Tasman Sea, anchored by a deep polar low which provided large swells for Victoria and New Zealand’s West Coast.
Stronger fronts push up into the Tasman from later Wed, bringing a SW flow and bigger S swell as we head to the end of the week.
No great change to the weekend f/cast. The fetch of deep E to E/NE winds in the Coral and Northern Tasman Sea is contracting northwards around a surface low off the CQ/Fraser coast, and expected to fizzle out over the weekend.
No great changes to the front end of this weather/surf event, which is starting to kick into gear now. The latter stages have been wound back a few notches, reducing the expected wave heights over the peak of the swell, so let’s take a look at it.