Tucker, Donna F.2014-11-262014-11-261999-04-01Tucker, Donna F. (1999). "The Summer Plateau Low Pressure System of Mexico." J. Climate, 12(4):1002-1015. http://dx.doi.org/10.1175/1520-0442(1999)012<1002:TSPLPS>2.0.CO;2.0894-8755https://hdl.handle.net/1808/15916This is the publisher's version, also available electronically from http://journals.ametsoc.org/doi/abs/10.1175/1520-0442%281999%29012%3C1002%3ATSPLPS%3E2.0.CO%3B2.Average July heights and winds over a 10-yr period are computed at 850 mb over Mexico using both surface and radiosonde data. During the day central Mexico at this level is dominated by low pressure, with some smaller areas of high pressure. The pressure systems were less pronounced in 1990 and the smaller high pressure areas were notably weaker during 1993, showing that there is important interannual variability in these patterns. At night, the low pressure weakens and there are generally expanded areas of high pressure. This area of low pressure is caused by the high plateau, which acts as an elevated heat source for the atmosphere during the day. Thus, the circulation is an extension of a similar one previously observed in the United States and is of about the same magnitude. Although computation of 850-mb heights from surface data helps improve horizontal resolution at this level, additional data would be needed to assess the vertical structure of the plateau circulation system as well as to provide more details on the diurnal variations.Article10.1175/1520-0442(1999)012<1002:TSPLPS>2.0.CO;2openAccess