5A.7 Mesoscale disturbances on the periphery of closed anticyclones: A link between mesoscale processes and intraseasonal climate variability

Wednesday, 27 June 2007: 9:30 AM
Summit A (The Yarrow Resort Hotel and Conference Center)
Thomas J. Galarneau Jr., NCAR, Boulder, CO; and L. F. Bosart

Closed anticyclones (CAs) in the upper troposphere over continental regions in the warm season provide an important link between weather and climate on intraseasonal time scales. Given that CAs can persist for a good part of a typical 90-day warm season, the positive (negative) surface temperature (rainfall) anomalies associated with them can determine the overall seasonal temperature (rainfall) anomalies for a given region. A less appreciated aspect of CAs is that high-impact severe weather events can occur in conjunction with migratory upper-level disturbances that traverse: 1) the poleward periphery of CAs where strong deep-layer shear in the flanking jet and high convective available potential energy (CAPE) is often present, and 2) the equatorward periphery of CAs where deep tropical moisture, moderate CAPE and moderate shear is often abundant.

The purpose of this presentation is to discuss how CAs provide one avenue for understanding links between weather and climate on intraseasonal time scales. This task will be accomplished through an examination of a global CA climatology, with a particular emphasis on warm season continental CAs and through case studies of continental CAs that were associated with significant heat waves. In particular, the structure and evolution of heat wave-related continental CAs over the US and Australia during July 1995 and February 2004, respectively, will be compared and contrasted. Attention will be paid to the contribution of these cases to the overall summer season temperature and precipitation anomalies for June, July, and August 1995 and December, January, and February 2004. The role of migratory upper-level disturbances on the periphery of these CAs in determining mode and severity of convection will also be discussed.

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