Abstract
Multiple datasets observed on 14 June 2002 illustrate the development of the moisture field during the evolution of the CBL. The CBL grows up from the surface several hours after sunrise and penetrates into and dominates the wave motions within the previous evenings' stable layer. The CBL continues its growth into the previous days' residual layer and becomes the dominant surface-based layer by 1815 UTC. Ongoing work includes i) extending these analyses using the other observations noted in Section 2 and ii) comparing and contrasting these observations with two other IHOP boundary layer evolution study days: 21 June and 25 June 2002.
Original language | English (US) |
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Title of host publication | 87th AMS Annual Meeting |
State | Published - 2007 |
Event | 87th AMS Annual Meeting - San Antonio, TX, United States Duration: Jan 14 2007 → Jan 18 2007 |
Other
Other | 87th AMS Annual Meeting |
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Country/Territory | United States |
City | San Antonio, TX |
Period | 1/14/07 → 1/18/07 |
All Science Journal Classification (ASJC) codes
- Environmental Engineering
- Global and Planetary Change
- Management, Monitoring, Policy and Law