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Surface fluxes and boundary layer recovery in TOGA COARE: sensitivity to convective organization

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dc.contributor.authorSaxen, Thomas R., author
dc.date.accessioned2022-02-24T18:45:41Z
dc.date.available2022-02-24T18:45:41Z
dc.date.issued1996-12
dc.descriptionDecember 1996.
dc.descriptionAlso issued as author's thesis (M.S.) -- Colorado State University, 1997.
dc.description.abstractShipboard radar data collected during the Tropical Ocean Global Atmospheres Coupled Ocean-Atmosphere Response Experiment (TOGA COARE) were used in conjunction with surface meteorological data from the Woods Hole Oceanographic Institute's Improved Meteorology (IMET) buoy to describe in detail how four different classifications of convective systems affect the atmospheric boundary layer and alter the surface fluxes of heat, moisture, and momentum. Atmospheric convective systems observed by radar were separated into four classifications based on spatial scale (sub­MCS vs. MCS scale) and horizontal morphology (non-linear vs. linear organization). Composite analyses of the surface fluxes along with the pertinent bulk variables have been constructed for each of the four classes of convective organization. During the compositing process, the convectively active and recovery periods were separated, allowing both of these distinctly different phases to be accurately represented in the final composite analyses. All four types of convective organization affected the boundary layer and altered the surface fluxes in a similar manner. However, the duration and magnitude of the response was highly dependent on the type of convective organization. The sub-MCS scale events tended to develop in environmental conditions which inhibited their upscale growth and accordingly produced the weakest and shortest response at the surface. The MCS scale events, on the other hand, tended to develop in environmental conditions which allowed the systems to intensify and organize, including strong convective scale downdrafts, which promoted a greater response at the surface. The MCS scale events also had a significant amount of stratiform precipitation associated with them which slowed the rate at which the boundary layer recovered to the pre-convective state. This, combined with the fact that the MCS scale events perturbed the boundary layer to a greater extent, accounted for the recovery phase of the MCS scale events being more than twice as long as the sub-MCS scale events.
dc.description.sponsorshipSponsored by the National Oceanic and Atmospheric Administration under grant NA37RJ0202.
dc.format.mediumreports
dc.identifier.urihttps://hdl.handle.net/10217/234410
dc.languageEnglish
dc.language.isoeng
dc.publisherColorado State University. Libraries
dc.relationCatalog record number (MMS ID): 991001558029703361
dc.relationQC852 .C6 no. 629
dc.relation.ispartofAtmospheric Science Papers (Blue Books)
dc.relation.ispartofAtmospheric science paper, no. 629
dc.rightsCopyright and other restrictions may apply. User is responsible for compliance with all applicable laws. For information about copyright law, please see https://libguides.colostate.edu/copyright.
dc.subject.lcshOcean-atmosphere interaction
dc.subject.lcshBoundary layer (Meteorology)
dc.subject.lcshConvection (Meteorology)
dc.titleSurface fluxes and boundary layer recovery in TOGA COARE: sensitivity to convective organization
dc.typeText
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