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Title: The effects of large-scale winds on the sea-land-breeze circulations in an area of complex coastal heating

Journal Article · · Journal of Applied Meteorology; (United States)
;  [1]
  1. Iowa State Univ., Ames (United States)

A three-dimensional mesoscale numerical model has been used to examine the effects of large-scale background winds on the characteristics of the sea-land-breeze circulations over an irregular coastline and complex surface-heating patterns at Kennedy Space Center. The surface heating was based on measured surface-temperature variation from the Kennedy Space Center Atmospheric Boundary Layer Experiment (KABLE) during the spring when the land-sea temperature gradient reaches its maximum. The results from the simulations compared well with data from KABLE. The results show an onshore large-scale flow produces weaker sea-breeze perturbations compared to those generated by an offshore flow. The coastal rivers and lagoon create intense surface convergence with strong vertical motion on the seaward side of the river by merging of the onshore flow with offshore river breezes. The disturbances caused by the inland water bodies are significant in the sea-breeze phase but are very minor in the land-breeze phase. An onshore synoptic wind causes an earlier onset of the sea-breeze phase but, delays the the onset of the land breeze, and a strong onshore flow of more than 5 m s[sup [minus]1] does not allow the land breeze to develop at all. The maximum offshore wind speed and vertical motion at night are less sensitive to the magnitude of surface cooling than to the large-scale flow and daytime surface heating, which determine the initial flow at the beginning of the land-breeze phase. The results show that the magnitude, the sense of rotation, and the diurnal variation of the dominant forces governing the wind-vector rotation change as the orientation of the synoptic wind direction changes. The rate of rotation in the sea-breeze phase is dominated by the balance between the mesoscale pressure gradient and friction; at night, the Coriolis effect also contributes to the balance of forces in the land-breeze phase. 35 refs., 12 figs., 1 tab.

OSTI ID:
5779449
Journal Information:
Journal of Applied Meteorology; (United States), Vol. 32:7; ISSN 0894-8763
Country of Publication:
United States
Language:
English