Observations of the Mean and Turbulence Structure of the Marine Boundary Layer over the Bay of Bengal during MONEX 79

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  • 1 Department of Marine, Earth and Atmospheric Sciences, North Carolina State University, Raleigh, NC 27695
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Abstract

Radiosondes from Soviet ships along with dropsondes and mean and turbulence data from the National Center for Atmospheric Research (NCAR) Electra gust probe aircraft are analyzed to infer the structure of the monsoon marine boundary layer during MONEX 79. Results of mean wind profiles indicate the existence of a jetlike structure in the upper part of the boundary layer during the more suppressed “monsoon-break” conditions. The thermal structure of the monsoon boundary layer during these break conditions is characterized by near-neutral to slightly unstable conditions. There was an approximate balance of form in the monsoon boundary layer between advective acceleration, friction and geostrophic departure. Advective acceleration was found to be a significant term, especially in the lower levels of the boundary layer. This contrasts with typical trade-wind boundary layers in which acceleration is generally negligible.

Results indicate that turbulence statistics associated with wind speed components and temperature in the monsoon boundary layer during MONEX 79 are generally large. Profiles of momentum and virtual temperature flux change sign at altitudes as low as 30 to 50% of the boundary layer height. The turbulent kinetic energy budget indicates that buoyancy is not a dominant source term above, roughly, one-third the boundary layer height. Viscous energy dissipation and turbulent transport are the important sink terms in the lowest one-half of the boundary layer.

Abstract

Radiosondes from Soviet ships along with dropsondes and mean and turbulence data from the National Center for Atmospheric Research (NCAR) Electra gust probe aircraft are analyzed to infer the structure of the monsoon marine boundary layer during MONEX 79. Results of mean wind profiles indicate the existence of a jetlike structure in the upper part of the boundary layer during the more suppressed “monsoon-break” conditions. The thermal structure of the monsoon boundary layer during these break conditions is characterized by near-neutral to slightly unstable conditions. There was an approximate balance of form in the monsoon boundary layer between advective acceleration, friction and geostrophic departure. Advective acceleration was found to be a significant term, especially in the lower levels of the boundary layer. This contrasts with typical trade-wind boundary layers in which acceleration is generally negligible.

Results indicate that turbulence statistics associated with wind speed components and temperature in the monsoon boundary layer during MONEX 79 are generally large. Profiles of momentum and virtual temperature flux change sign at altitudes as low as 30 to 50% of the boundary layer height. The turbulent kinetic energy budget indicates that buoyancy is not a dominant source term above, roughly, one-third the boundary layer height. Viscous energy dissipation and turbulent transport are the important sink terms in the lowest one-half of the boundary layer.

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