Heat storage. Conservation of energy requires that incoming energy balances outgoing energy plus a change in storage. To relate changes in heat content with temperature, we use: Δ Q S / Δ z = C s Δ T / Δ t.
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(0.0012 × 106 J m-3 K-1) ×ΔT/0.003 m
m2 s-1)(0.0012 J m-3 K-1)} = 0.3/0.0246 K = 12.2 K
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s-1 near the laminar boundary layer to as large as 102 m2 s-1 higher up in the PBL (that equates to 7 orders of magnitude!).
Oke (1987) Back Lunch
θ = T + Γ z
Oke (1987) have if it were moved adiabatically to 1000 hPa.