Flight-level thermodynamic instrument wetting errors in hurricanes. Part II: Implications

Monthly Weather Review

Volumn 130, Issue 4, 2002, Pages 842-851

  Eastin, Matthew D ^a   Black, Peter G ^a   Gray, William M ^a  

^a Engineering Research Center and Hydraulics Laboratory   (United States)

Author keywords

[No Author keywords available]

Indexed keywords

BUOYANCY; ERROR ANALYSIS; HEAT FLUX; INSTRUMENT ERRORS; TEMPERATURE MEASUREMENT; WETTING;

RAINBANDS;

HURRICANES;

AIRBORNE SENSOR; ERROR ANALYSIS; HURRICANE; RADIOMETER; WETTING;

EID: 0036538469     PISSN: 00270644     EISSN: None     Source Type: Journal    
DOI: 10.1175/1520-0493(2002)130<0842:FLTIWE>2.0.CO;2     Document Type: Article

References (41)

1. The distribution of liquid water in hurricanes
2. Response of the hurricane boundary layer to changes in sea surface temperature in a numerical model
3. Mesoscale and convective structure of a hurricane rainband
4. Thermodynamic budget diagrams for the hurricane subcloud layer
5. The boundary layer of Tropical Cyclone Kerry (1979)
6. Observations of the distribution of ice in hurricanes
7. Conditional instability and shear for six hurricanes over the Atlantic Ocean
8. The computation of equivalent potential temperature
9. Surface observations within the hurricane environment
10. Flight-level instrument wetting errors in hurricanes. Part I: Observations
11. Is there any hope for tropical cyclone intensity change prediction? - A panel discussion
12. An air-sea interaction theory for tropical cyclones. Part I: Steady-state maintenance
13. The structure and energetics of the tropical cyclone. I. Storm structure
14. A composite analysis of the core of a mature hurricane
15. Calculations of cumulus draft velocities in hurricanes from aircraft data
16. The tropical cyclones maximum potential intensity (MPI)
17. The hurricane's inner core region. II. Thermal stability and dynamic characteristics
18. Hurricane Hilda, 1964, II. Structure and budgets of the hurricane on October 1, 1964
19. The structure of a small, intense hurricane - Inez, 1966
20. Updraft and downdraft cores in TOGA COARE: Why so many buoyant downdraft cores?
21. Marked changes in characteristics of the eye of intense typhoons between the deepening and filling stages
22. Mesoscale and convective-scale characteristics of mature hurricanes. Part I: General observations by air-craft
23. Mesoscale and convective-scale characteristics of mature hurricanes. Part II: Inner core structure of Hurricane Allen (1980)
24. Vertical velocity characteristics of oceanic convection
25. Vertical motions in intense hurricanes
26. Two distinct regimes in the kinematic and thermodynamic structure of the hurricane eye and eyewall
27. Dynamics of convective vortices and eye formation
28. Vertical velocity in oceanic convection off tropical Australia
29. On the structure and maintenance of the mature hurricane eye
30. On the dynamics and energy transformations in steady-state hurricanes
31. Low-layer features of two limited-area hurricane regimes
32. Conceptual evolution of the theory and modeling of the tropical cyclone
33. Boundary layer structure and dynamics in outer hurricane rainbands. Part II: Downdraft modification and mixed layer recovery
34. Vertical exchange of momentum and energy in the subcloud layer of Australian Hurricane (1979) Kerry
35. The hurricane's inner core region. I. Symmetric and asymmetric structure
36. Buoyancy of convective clouds in TOGA COARE
37. Tropical cyclone eye thermodynamics
38. A multiscale numerical study of Hurricane Andrew (1992). Part III: Dynamically induced vertical motion
39. Mesoscale motion fields associated with a slowly moving GATE convective band