Patrick99 wrote:What is "wavebreaking?" Is it just a buzzword for dry air suppressing tropical waves?
You can think of it much like an ocean wave. Cyclonic wave breaking (CWB) occurs when the amplitude of a mid-upper level short wave trough becomes too large compared to its wavelength. Anticyclonic wave breaking (AWB) occurs when the amplitude of a mid-upper level short wave ridge becomes too large compared to its wavelength. The processes of both CWB and AWB are accompanied by and increase in deformation and wind shear, which creates unvfavorable/less favorable conditions when and where it occurs. In this case, I believe the wave breaking being referred to is AWB.
In the context of the (sub)tropics, let's look at the semi-permanent mid-oceanic TUTT. Its strongest reflection occurs at about 200MB, In the summer, when amplification of the NHEM flow occurs (i.e. development of short wave troughs and ridges), wave breaking will eventually occur when they reach the Atlantic basin and are of significant amplitude (they drill far enough south into the subtropics), and invariably interact with the TUTT to some degree. During the wave break process, the resulant amplification of the TUTT causes the upper level westerlies to strengthen and drop southward from the subtropics into the central-western Atlantic MDR. After an AWB occurs, development (and westward retrogression) of a cutoff low results, although these cutoffs vary greatly in terms of size, strength, persistence, movement, etc. Generally a piece of the TUTT fractures off an retrogrades westward underneath the rebuilding mid-upper ridge. This stronger winds/shear will then move away from the area as retrogression occurs. This is cyclical, and more frequent wave breaking is a sign of more frequent interaction between between northern stream Atlantic troughs and the TUTT. In my experience, this more frequent interaction occurs when there is anamalously strong mid-upper ridging over NOAM/CONUS (think heat waves), which causes lower heights downstream over the Atlantic. However, this doesn't seem to be the case as 500-200MB heights have been above normal across virtually the entire Atlantic since 1 JUL.
Explaining atmospheric waves, breaks and the TUTT isn't the easiest thing in the world to do while keeping it simple, but hopefully this helps you grasp the concept a little.
[soapbox]
As I've stated in previous posts, I don't count all mid to upper level troughs/lows in the subtropics as TUTTs, only ones which have significant interaction with the TUTT . The others I'll often refer to as "TUTT-type" lows. Operationally here in Florida, I've found that there's an important difference in that a true TUTT (troughs or cutoff low) will almost always have a weaker reflection at 500MB than a non TUTT counterpart. (TUTT has been overused/incorrectly applied to non-TUTT features, but that's a rant for another day). [/soapbox]