Abstract The global climate in 2000 was again influenced by the long–running Pacific cold episode (La Niña) that began in mid–1998. Consistent with past cold episodes, enhanced convection occurred across the climatologically convective regions of Indonesia and the western equatorial Pacific, while convection was suppressed in the central Pacific. The La Niña was also associated with a well–defined African easterly jet located north of its climatological mean position and low vertical wind shear in the tropical Atlantic and Caribbean, both of which contributed to an active North Atlantic hurricane season. Precipitation patterns influenced by typical La Niña conditions included 1) above–average rainfall in southeastern Africa, 2) unusually heavy rainfall in northern and central regions of Australia, 3) enhanced precipitation in the tropical Indian Ocean and western tropical Pacific, 4) little rainfall in the central tropical Pacific, 5) below–normal precipitation over equatorial east Africa, and 6) drier–th...
CITATION STYLE
Lawrimore, J. H., Menne, M. J., Gleason, K. L., Easterling, D. R., Heim, R. R., Halpert, M. S., … Alexander, L. (2001). Climate Assessment for 2000. Bulletin of the American Meteorological Society, 82(6), 1304–1304. https://doi.org/10.1175/1520-0477(2001)082<1304:caf>2.3.co;2
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