Breakup of temperature inversions in deep mountain valleys. Part I. Observations
Journal Article
·
· J. Appl. Meteorol.; (United States)
The breakup of temperature inversions in the deep mountain valleys of western Colorado has been studied by means of tethered balloon observations of wind and temperature structure on clear weather days in different seasons. Vertical potential temperature structure profiles evolve following one of three patterns. Two of the patterns are special cases of the third pattern, in which inversions are destroyed by two continuous processes - upward growth of a convective boundary layer (CBL) into the base of the valley inversion, and descent of the inversion top. The three idealized patterns are described and 21 case studies of inversion breakup following the patterns are summarized. Inversion breakup begins at sunrise and is generally completed in 3-1/2 to 5 h, unless the valley is snow covered or the ground is wet. Warming of the inversion layer is consistent with subsidence heating. An hypothesis is offered to explain the observations, stressing the role of the sensible heat flux in causing the CBL to grow and an upslope flow to develop over the sidewalls. As mass is removed from the base of the inversion layer in the upslope flows, the inversion sinks and warms.
- Research Organization:
- Pacific Northwest Lab., Richland, WA
- OSTI ID:
- 6726340
- Journal Information:
- J. Appl. Meteorol.; (United States), Journal Name: J. Appl. Meteorol.; (United States) Vol. 21:3; ISSN JAMOA
- Country of Publication:
- United States
- Language:
- English
Similar Records
Cross-valley structure of the valley atmosphere during the temperature inversion breakup period
Inversion Breakup in Small Rocky Mountain and Alpine Basins
Breakup of a nocturnal temperature inversion in the Dischma Valley during DISKUS
Technical Report
·
Sat Jan 31 23:00:00 EST 1987
·
OSTI ID:7192779
Inversion Breakup in Small Rocky Mountain and Alpine Basins
Journal Article
·
Sun Aug 01 00:00:00 EDT 2004
· Journal of Applied Meteorology, 43(8):1069-1082
·
OSTI ID:15020846
Breakup of a nocturnal temperature inversion in the Dischma Valley during DISKUS
Journal Article
·
Sun Jan 31 23:00:00 EST 1988
· J. Appl. Meteorol.; (United States)
·
OSTI ID:5091980
Related Subjects
500100* -- Environment
Atmospheric-- Basic Studies-- (-1989)
54 ENVIRONMENTAL SCIENCES
AIRSHIPS
AMBIENT TEMPERATURE
BALLOONS
BOUNDARY LAYERS
COLORADO
CONVECTION
DAILY VARIATIONS
DATA
EXPERIMENTAL DATA
FEDERAL REGION VIII
HEAT FLUX
INFORMATION
LAYERS
METEOROLOGY
MONITORING
MOUNTAINS
NORTH AMERICA
NUMERICAL DATA
SEASONAL VARIATIONS
TEMPERATURE DISTRIBUTION
TEMPERATURE INVERSIONS
TEMPERATURE MEASUREMENT
TOPOGRAPHY
USA
VALLEYS
VARIATIONS
Atmospheric-- Basic Studies-- (-1989)
54 ENVIRONMENTAL SCIENCES
AIRSHIPS
AMBIENT TEMPERATURE
BALLOONS
BOUNDARY LAYERS
COLORADO
CONVECTION
DAILY VARIATIONS
DATA
EXPERIMENTAL DATA
FEDERAL REGION VIII
HEAT FLUX
INFORMATION
LAYERS
METEOROLOGY
MONITORING
MOUNTAINS
NORTH AMERICA
NUMERICAL DATA
SEASONAL VARIATIONS
TEMPERATURE DISTRIBUTION
TEMPERATURE INVERSIONS
TEMPERATURE MEASUREMENT
TOPOGRAPHY
USA
VALLEYS
VARIATIONS