HR: 17:20h
AN: A44A-06    [Abstracts]
TI: Mesoscale and Synoptic Summertime Circulations and Their Impact on Visibility in the Arabian Gulf
AU: * Eleuterio, D P
EM: daneleuterio@yahoo.com
AF: Naval Research Laboratory DC, Ocean and Atmospheric Science & Technology Directorate (Code 7005) 4555 Overlook Avenue SW, Washington, DC 20375-5349
AU: Walker, A L
EM: walker@nrlmry.navy.mil
AF: Naval Research Laboratory Monterey, Aerosol and Radiation Section, Code 7543 7 Grace Hopper Ave., Stop 2, Monterey, CA 93943-5502
AB: Although frequently characterized as a region of relatively persistent northwesterly winds, often referred to as the 40-day shamal, several researchers have recognized significant temporal and spatial variability in the summer low level winds in the Arabian Gulf. In addition to the synoptically driven gradient between the subtropical high to the north and the monsoon trough across the Gulf of Oman and Northern Arabian Sea, there are complex interactions between the Saudi Arabian and Pakistani heat lows, land-sea breeze circulations, and coastal terrain influence due to the proximity of the Zagros Mountains. These interactions frequently result in several distinct wind regimes within the Arabian Gulf, to include weak thermally and dynamically forced southerlies in the southern Gulf, a diurnally varying region of convergence/ divergence across the central Gulf, and northwesterly shamal type flow in the northern Gulf. The relative orientation and strength of these wind regimes and the strength of the subsidence inversion at the top of the marine boundary layer greatly impact the aerosol loading over water and resulting visibility due to wind-blown sand, dust, and smoke. Several case studies are examined to explore the interaction between mesoscale and synoptic forcing and the resulting spatial and temporal variability in visibility and aerosol optical depth. Conditions range from two to three day periods of rapid and persistent regional clearing with freshening northwesterly winds, to persistent periods of moderate to poor visibility in marine haze under light winds, to large scale events that create a distinct wind and dust front, severely reducing visibility through much of Iraq, Kuwait, and Saudi Arabia, and extending well into the Arabian Gulf. These strong, widespread events may be correlated with synoptically forced conditions farther north. Alternatively, smaller scale regional plumes of mobilized dust are often created by mesoscale events which, in conjunction with oil smoke and industrial pollution, can rapidly reduce visibility in localized regions for periods of 1-2 days and are relatively difficult to forecast because of their mesoscale nature.
DE: 0305 Aerosols and particles (0345, 4801, 4906)
DE: 3329 Mesoscale meteorology
SC: Atmospheric Sciences [A]
MN: Fall Meeting 2005