Further Investigations of a Mesospheric Inversion Layer Observed in the ALOHA-93 Campaign
Abstract
Temperature and wind data obtained from a Na wind/temperature lidar operated by the University of Illinois group during the Airborne Lidar and Observations of the Hawaiian Airglow (ALOHA-93) Campaign, previously analyzed by Huang et al. [1998] using an isothermal Brunt-Vaisala frequency, have been reexamined to include temperature gradients in the calculation of the Richardson number. In the previous analysis using the isothermal Brunt-Vaisala frequency the existence of convective instability could not be assessed. New analysis shows that the nonisothermal Richardson number preserves some features found previously, with some striking differences noticeable at times between 0900 and 1030 UT. The nonisothermal Richardson number becomes negative as early as 0930 UT, indicating conditions conducive to the development of convective instability and turbulence. The possibility that turbulence could exist at times earlier than previously thought explains more satisfactorily the large temperature increase observed before 1000 UT.
Document Details
- Document Type
- Technical Report
- Publication Date
- Oct 15, 2002
- Accession Number
- ADA437972
Entities
People
- E. M. Dewan
- M. P. Hickey
- R. H. Picard
- Tai-fu Tuan
- Tai-yin Huang
Organizations
- Air Force Research Laboratory