Dear Jennifer,
My paper ‘Lunar Tides and the Long-Term Variation of the Peak Latitude Anomaly of the Summer Sub-Tropical High Pressure Ridge over Eastern Australia’ has been published at:
http://www.benthamscience.com/open/toascj/articles/V006/49TOASCJ.pdf
It can be down loaded for free!
The main take-home conclusions from this paper are that:
1. The most important influence upon the climate of Northern NSW and Southern Queensland after the La Nina/El Nino phenomenon is the Peak Latitude Anomaly for the Summer Sub-Tropical High Pressure Ridge over Eastern Australia (L(SA)).
2. The interannual variability of L(SA) is major mechanism influencing inter-annual rainfall variability in Eastern Australia. It has also been shown to be connected to the inter-annular variability of the annual mean maximum temperatures, zonal westerly winds, meridional winds and mean air temperature.
3. The long-term (i.e for periods of 2 to 20 years) variations of L(SA) are dominated by (significant) periodic signals at 9.4 (+0.4/-0.3) and 3.78 (+/- 0.06) years.
4. L(SA) systematically moves away from the Equator as the angle between the Earth-Sun axis and the line-of-nodes of the Lunar orbit (at the time of perihelion) decreases. The magnitude of the movement of the mean summer peak latitude anomaly can amount to 1 degree of latitude over the 9.3 year semi-draconic spring tidal cycle.
5. L(SA) systematically moves towards the Equator as the number of days (to the nearest full day) that New/Full is from Perihelion decreases. The magnitude of the movement of the mean summer peak latitude anomaly can amount to 0.7 degree of latitude over the 3.8 year peak spring tidal cycle.
6. The 9.4 year signal in L(SA) is in-phase with the draconic spring tidal cycle, while the phase of the 3.8 year signal in L(SA) is retarded by one year compared to the 3.8 year peak spring tidal cycle.
7. This paper supports the conclusion that long-term changes in the lunar tides, in combination with the more dominant solar-driven seasonal cycles, play an important role in determining the observed inter-annual to decadal variations of L(SA).
8. The IPCC does not take into account the important effects upon climate of long-term
lunar atmospheric tides.
Cheers,
Ian Wison
Toowoomba, Queensland, Australia
Jennifer Marohasy BSc PhD has worked in industry and government. She is currently researching a novel technique for long-range weather forecasting funded by the B. Macfie Family Foundation.