Parameterizing Scalar Transfer over Snow and Ice: A Review

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SHEBA flux–profile relationships in the stable atmospheric boundary layer (2007, background): “There is a long history of testing Monin–Obukhov predictions including profile functions (see, for example, the surveys in Monin and Yaglom 1971; Dyer 1974; Yaglom 1977; Dyer and Bradley 1982; Högström 1988; Sorbjan 1989; Garratt 1992; Andreas 2002).”
On the critical Richardson number in stably stratified turbulence (2007, background): “Similarly, Andreas (2002) suggests that “in stable conditions, turbulence is presumed to cease and the flow becomes laminar when the Richardson number exceeds a critical value Ric” and Canuto (2002a) proposes a definition of Ric as a value of Ri “above which there is no longer turbulent mixing”…”
Flux–gradient relationship, self‐correlation and intermittency in the stable boundary layer (2004, background): “When these variables share a common divisor, however, even random data can produce significant non-zero correlation (Kim 1999; Andreas 2002).”