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deep within an urban street canyon. While all field experiments represent case studies that are difficult to generalize, an attempt has been made here to extract and describe more generic features associated with real urban canyon flows subjected to a limited range of varying upstream stabilities. Three broad stability classification regimes were chosen for nominally southerly winds: stable ( z / L > 0.2), neutral (−0.2 < z / L < 0.2), and unstable ( z / L < −0.2). In general, most of the
deep within an urban street canyon. While all field experiments represent case studies that are difficult to generalize, an attempt has been made here to extract and describe more generic features associated with real urban canyon flows subjected to a limited range of varying upstream stabilities. Three broad stability classification regimes were chosen for nominally southerly winds: stable ( z / L > 0.2), neutral (−0.2 < z / L < 0.2), and unstable ( z / L < −0.2). In general, most of the
