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The “Effects of Lake Breezes on Weather in Manitoba” project was conducted during 6–24 July 2013 to better understand local lake-breeze characteristics. Data were collected using a variety of platforms including Doppler wind lidar, rawinsondes, Doppler radar, surface meteorological stations, and a mobile weather station. The spatial and temporal variability of thermodynamic and kinematic characteristics of lake-breeze fronts are presented for three cases. Lake-breeze frontal passages were characterized by an average increase in dew point of 2.5 $$^{\circ }$$ ∘ C and decrease in temperature of 0.5 $$^{\circ }$$ ∘ C. The lake-breeze front width varied significantly over multiple measurements and cases, ranging between 50 and 800 m. The depth of the lake-breeze circulation varied between 100 and 700 m. Vertical velocities were measured at the lake-breeze front using lidar, with upward velocities of 2–3 m s $$^{-1}$$ - 1 and small downward velocities of magnitude 0.5 m s $$^{-1}$$ - 1 behind the front. These observations of lake-breeze fronts in southern Manitoba contribute both to the local and broader understanding of the variability (temporally and spatially) of inland shallow lake breezes.
Boundary-Layer Meteorology – Springer Journals
Published: Nov 9, 2016
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