ILL £ Observations of Multiple Sea Breeze Boundaries during an Unseasonably Warm Day in Metropolitan New York City BY DAVID R. NOVAK AND BRIAN A . COLLE f ea-breeze de- \ velopment is commonl y ob- serve d in the New Yor k City (NYC) metropolita n (met- ro) area during the spring an d summer, du e to the city's proximit y to the Atlanti c Ocea n and Long Island Sound (Fig. 1). The forma- tio n and evolution of sea breezes is of particula r inter- FIG. I. (a) Topographi c map of th e region surrounding NY C with geographi c features es t to the energy, labeled , and elevation shaded (m) . Th e NY C metro are a is outline d by a box. (b) Map aviation , and air- of th e NY C metro-area observationa l network (as of Januar y 2005) with META R (red, qualit y communi- labeled) , buoy (white), mesonet (gray), and ACAR S (box) stations plotted. tie s (amon g oth- ers) , since the sea evolution when downslope westerly flow off elevated breez e alters the low-level win d and temperature fields. As shown
Bulletin of the American Meteorological Society – American Meteorological Society
Published: Feb 1, 2006
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