AnnularCane wrote:cycloneye wrote:AnnularCane wrote:What exactly is "wave breaking" anyway?
Is very long this document about Rossby wave breaking.
An excerpt:
RWB events are identified in the upper troposphere but affect the flow at all tropospheric levels and play an important role in the meridional transport of both tropical and subtropical air masses [Homeyer and Bowman, 2013]. At the surface, AWB drives a positive sea level pressure (SLP) anomaly to the South of the breaking and a negative anomaly to the North, while the converse holds for CWB [Strong and Magnusdottir, 2008a]. A midlatitude AWB (CWB) is therefore associated with an enhanced (reduced) SLP dipole over the Atlantic and a more northerly (southerly) jet than usual [Riviere and Orlanski, 2007]. Strong and Magnusdottir [2008a] found the relationship between RWB and the NAO to be strongly dependent on the meridional location of RWB, with AWB (CWB) centered around 50°N associated with the positive (negative) phase of the NAO, in agreement with previous studies [e.g., Benedict et al., 2004]. RWB events shifted 20° to the north or south were found to drive the opposite NAO polarity.
https://agupubs.onlinelibrary.wiley.com ... 15JD023854
Thanks...but I probably should have told you to explain it like I'm five years old.
The shortest words. Dry air that pushes down from the Azores / Europe area to cool the waters.
