Baroclinic wave variations observed in MLS upper tropospheric water vapor

• Published in: Geophysical research letters Vol. 23; no. 21; pp. 2967 - 2970
• Main Authors: Stone, Elizabeth M., Randel, William J., Stanford, John L., Read, William G., Waters, Joe W.
• Format: Journal Article
• Language: English
• Published: Washington, DC Blackwell Publishing Ltd 15.10.1996; American Geophysical Union
• Subjects: Circulation; Decay; Earth, ocean, space; Evolution; Exact sciences and technology; External geophysics; Geophysics; Meteorology; Southern Hemisphere; Traveling waves; Vorticity; Water in the atmosphere (humidity, clouds, evaporation, precipitation); Water vapor; Southern Hemisphere; Water; Vapor; Troposphere; Vorticity; Summer; Satellite observation; Atmospheric wave; Baroclinic waves
• ISSN: 0094-8276; 1944-8007
• DOI: 10.1029/96GL02576

Upper tropospheric water vapor measurements from the UARS Microwave Limb Sounder are used to investigate the structure and evolution of eastward traveling medium‐scale wave features in Southern Hemisphere summertime. The extratropical Southern Hemisphere summer circulation pattern is frequently dominated by medium scale waves which exhibit life cycles of baroclinic growth and barotropic decay. The water vapor field during such life cycles is examined here and found to be well correlated with meteorological fields derived from European Centre for Medium Range Weather Forecasts global analyses. From mid January to mid February 1992 several episodes of growth and decay in the amplitude of eastward traveling waves are found in the water vapor and meteorological data at levels of the upper troposphere, with zonal waves four, five and six being predominant modes. The water vapor data are compared with derived potential vorticity (PV) fields, with strong anticorrelation observed in middle and high latitudes. The results are consistent with model paradigms for the structure and evolution of baroclinic disturbances, coupled with the known characteristics of high PV and low water vapor mixing ratios in lower stratospheric air parcels and the reverse for upper tropospheric air.