![]() ![]() ![]() Near the top of the PBL, these pollutants were horizontally advected to a region with lower PBL heights, resulting in pollution transport out of the boundary layer and into the free troposphere. The strength and duration of the bay breeze allowed pollutants to converge, resulting in high concentrations locally near the bay-breeze front within the Baltimore metropolitan area, where they were then lofted to the top of the planetary boundary layer (PBL). A strong and prolonged bay breeze developed during the late morning and early afternoon along the western coastline of the bay. Results show that southerly winds during the overnight and early-morning hours prevented the advection of air pollutants from the Washington, D.C., and Baltimore, Maryland, metropolitan areas over the surface waters of the bay. A case study was conducted to understand why a particular day was the only one during an 11-day ship-based field campaign on which surface ozone was not elevated in concentration over the Chesapeake Bay relative to the closest upwind site and why high ozone concentrations were observed aloft by in situ aircraft observations. Meteorological and air-quality model simulations are analyzed alongside observations to investigate the role of the Chesapeake Bay breeze on surface air quality, pollutant transport, and boundary layer venting. The bay breeze was identified by noting the change in surface wind direction associated with the large virtual potential temperature gradient, surface convergence, and vertical motion at the bay-breeze front, as shown in Fig. The blue lines in the middle-right and bottom-right panels show the location of the bay-breeze front. The letters W and B in the top-left panel show the locations of Washington and Baltimore, respectively, and the letter P in the middle-left panel denotes the location of Padonia. The bay-breeze convergence zone pushed farther inland by 1400 EDT (see bottom row). The bay-breeze circulation along the northern half of the western coastline of the bay began to form at 1100 EDT when winds over the water changed from calm or southwesterly to south-southeasterly while winds over land remained southerly or south-southwesterly (see middle row). One of every 14 grid cells has a wind vector plotted. The WRF results are from the 1.33-km-horizontal-resolution domain. ![]() I will not return to Bay Breeze, and will inform everyone I know of this occurrence, including the complete disrespect I received.(left) Observed 2-m temperature and 10-m wind velocity, (center) WRF-diagnosed 2-m temperature and 10-m wind velocity, and (right) WRF-simulated virtual potential temperature in the first model layer (about 11 m AGL) and 10-m wind velocity on at (top) 0700, (middle) 1100, and (bottom) 1400 EDT. However, this experience has completely changed my mind. We have enjoyed this restaurant for many years, and have had no problem ever. I did not feel comfortable “forcing” someone to to their job, as I feared our food would be tainted in some way. My wife told me that she would go find someone and tell them our situation, because she was hungry. After no service for a seated 25 minutes, we left. He walked past us a handful of times, not once talking to us at all. Another 5 minutes went by, and he told us “I’ll be right with you”, and left 3 straws. She asked if he wanted her to go ahead and get our drink order, and he said “no, I got it”. waiter “Brian” to our table and he wouldn’t come to the table. To which the reply was “no ma’am, not yet”. Chinese Restaurants for Lunch in HamptonĪfter waiting the customary 40 minutes to be seated, we were not seen about until another waitress passed by the third time and asked if we had been taken care of.American Restaurants for Lunch in Hampton.Restaurants near Bay Breeze Seafood Restaurant.Melia Punta Cana Beach Wellness Inclusive - Adults only.Hotels near (ATL) Hartsfield-Jackson Atlanta Intl Airport. ![]()
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