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A study on C, H and L type prismatic buildings for Synoptic wind flow.By Hirak Ranjan Das, Kalyan Kumar Das, Ajan Patowary
Abstract: The atmospheric boundary layer can be defined as part of the troposphere at the lowest level which is influenced by the presence of the earth’s surface, and responds to surface forcing within a timescale of about an hour or less. The boundary layer depth might differ from hundreds of meters to a few kilometers. The wind that blows due to Atmospheric Boundary Layer is known as synoptic wind. Moreover, thunderstorms …
Published in International Journal of Construction Engineering and Planning · Vol. 6, Issue 1, 2020 · pp. 6–14 Read article →