Seasonal Variability of the 40–50 Day Oscillation in Wind and Rainfall in the Tropics
- 1 October 1988
- journal article
- Published by American Meteorological Society in Journal of the Atmospheric Sciences
- Vol. 45 (19) , 2680-2702
- https://doi.org/10.1175/1520-0469(1988)045<2680:svotdo>2.0.co;2
Abstract
Time spectral analysis is performed on long records of wind and precipitation from stations in the tropical Indian Ocean-Pacific Ocean are. The spectra are done separately for winter and summer half-years. Statistically significant spectral peaks in the 40–50 day period range show strong seasonal variability. The 40–50 day peaks in the 200 mb zonal wind spectra are stronger and more prevalent during the Northern Hemisphere winter half-year. Spectral peaks in the 850 mb wind show a preference for summer in the Northern Hemisphere. Precipitation spectra show significant 40–50 day peaks at selected locations in the Indonesian region and along the South Pacific convergence zone in the central Pacific during Southern Hemisphere summer. These oscillations in precipitation are coherent with nearby zonal wind oscillations. No significant oscillations in precipitation were found for stations significantly north of the equator during either half-year. In particular, no significant peaks in precipitation sp... Abstract Time spectral analysis is performed on long records of wind and precipitation from stations in the tropical Indian Ocean-Pacific Ocean are. The spectra are done separately for winter and summer half-years. Statistically significant spectral peaks in the 40–50 day period range show strong seasonal variability. The 40–50 day peaks in the 200 mb zonal wind spectra are stronger and more prevalent during the Northern Hemisphere winter half-year. Spectral peaks in the 850 mb wind show a preference for summer in the Northern Hemisphere. Precipitation spectra show significant 40–50 day peaks at selected locations in the Indonesian region and along the South Pacific convergence zone in the central Pacific during Southern Hemisphere summer. These oscillations in precipitation are coherent with nearby zonal wind oscillations. No significant oscillations in precipitation were found for stations significantly north of the equator during either half-year. In particular, no significant peaks in precipitation sp...Keywords
This publication has 0 references indexed in Scilit: