WebApr 19, 2015 · Lower-tropospheric tropical synoptic-scale disturbances (TSDs) are associated with severe weather systems in the Asian Monsoon region. Therefore, exact prediction of the development and behavior of TSDs using atmospheric general circulation models is expected to improve weather forecasting for this region. Recent state-of-the art … WebThe low-level circulation over the Atlantic and Pacific oceans is dominated by the easterly flow around the equatorward flank of the subtropical high-pressure belts near 30N and 30S. Superimposed on this planetary-scale easterly flow are weak synoptic-scale disturbances that cause the wind to fluctuate between northeasterly and southeasterly.
1062 JOURNAL OF THE ATMOSPHERIC SCIENCES …
WebJun 1, 1990 · Mean phase speeds at 850 mb are positively correlated with the mean wind on the equator at 500 mb and below, and negatively correlated with the mean wind above … WebThey are characterized by persistent The above studies have focused almost exclusively on large-scale flow patterns that appear repeatedly at fixed seasonal mean rainfall, while very little attention has geographical locations and organize the behavior of been given to the interannual variability of subseasonal synoptic-scale motions during ... describe gregory crewdson work
Tropical Weather Learn Science at Scitable - Nature
WebThis paper focuses on the synoptic-scale activity over the off-equatorial part of the western Pacific storm tracks where disturbances are initiated and begin to grow. In particular, the circulation structure and disper- sion characteristics of eddies east of … WebSYNOPTIC DISTURBANCES NEAR THE EQUATOR Lockwood, J. G. Weather , Volume 20 (9) – Sep 1, 1965 Read Article Download PDF Share Full Text for Free 10 pages Article Details Recommended References Bookmark Add to Folder Cite Social Times Cited: Web of Science Journals / Weather / Volume 20 Issue 9 Subject Areas / Earth and Planetary Sciences / WebThe atmospheric component is characterized as an oscillation propagating eastwards from the Maritime Continent around the equator 7 at about 5 m s -1; this gives the atmospheric MJO a period of roughly 30-60 days. The spatial scale of the atmospheric MJO can be described in terms of a local wavelength of roughly 12,000-20,000 km. describe greek art and literature