Changeset 701 for palm/trunk
- Timestamp:
- Mar 23, 2011 8:37:42 AM (14 years ago)
- Location:
- palm/trunk/DOC/tec/methods/cloud_physics
- Files:
-
- 2 edited
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palm/trunk/DOC/tec/methods/cloud_physics/cloud_physics.tex
r481 r701 237 237 gives 238 238 \begin{eqnarray} 239 \overline q_{s} = \overline q_{s}(\overline T_{l})\frac{\left(1.0+\beta\,\overline q\right)}239 \overline q_{s}(T) = \overline q_{s}(\overline T_{l})\frac{\left(1.0+\beta\,\overline q\right)} 240 240 {1.0 + \beta\, \overline q_{s}(\overline{T_{l}})}. 241 241 \label{eq:qs2} … … 244 244 \begin{eqnarray} 245 245 \overline q_{s}(\overline T_{l}) = 0.622\frac{\overline e_{s}(\overline T_{l})} 246 {p_{0}(z)-0.37 7\,\overline e_{s}(\overline T_{l})}246 {p_{0}(z)-0.378\,\overline e_{s}(\overline T_{l})} 247 247 \label{eq:qs3} 248 248 \end{eqnarray} … … 266 266 The hydrostatic pressure $p_{0}(z)$ is given by \cite{cuijpers93}: 267 267 \begin{eqnarray} 268 p_{0}(z) = p_{0}(z=0)\ frac{T_{\mathrm{ref}}(z)^{c_{p}/R}}{T_{0}}268 p_{0}(z) = p_{0}(z=0)\left(\frac{T_{\mathrm{ref}}(z)}{T_{0}}\right)^{c_{p}/R} 269 269 \label{eq:p_0} 270 270 \end{eqnarray} … … 285 285 \overline q_{l} = 286 286 \begin{cases} 287 \overline q - \overline q_{s}(\overline T _{l}) &288 \textnormal{if} \quad \overline q > \overline q_{s}(\overline T _{l}) \\287 \overline q - \overline q_{s}(\overline T) & 288 \textnormal{if} \quad \overline q > \overline q_{s}(\overline T) \\ 289 289 0 & \textnormal{else} 290 290 \end{cases} … … 427 427 against numerical data. \textit{J. Atmos. Sci.}, \textbf{38}, 2414-2428. 428 428 \bibitem[Cox (1976)]{cox76} 429 \textbf{Cox, S. K., 1976:} Observations of cloud infrared e missivity.429 \textbf{Cox, S. K., 1976:} Observations of cloud infrared effective emissivity. 430 430 \textit{J. Atmos. Sci.}, \textbf{33}, 287-289. 431 431 \bibitem[Cuijpers and Duynkerke (1993)]{cuijpers93}
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