The influence of local topography on the surface wind was found to be especially strong where the sea narrows to form a channel. Surface wind through a channel seems to be confined within the channel; the wind direction is adjusted to run parallel to the channel orientation. -from Author
CITATION STYLE
Ito, H. (1982). Wind through a channel - surface wind measurements in Smith Sound and Jones Sound in northern Baffin Bay. Journal of Applied Meteorology, 21(8), 1053–1062. https://doi.org/10.1175/1520-0450(1982)021<1053:WTACWM>2.0.CO;2
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