# Changeset 855 for palm

Ignore:
Timestamp:
Mar 19, 2012 2:26:19 PM (10 years ago)
Message:

Correction of typos

Location:
palm/trunk/DOC/misc
Files:
2 edited

### Legend:

Unmodified
 r543 -\frac{\partial \left(\overline u_{j} \overline u_{i}\right)}{\partial x_{j}} -\frac{1}{\rho_{0}}\frac{\partial \overline \pi^{\ast}}{\partial x_{i}} - \varepsilon_{ijk}f_{j}\overline u_{k} - \varepsilon_{i3k}f_{3}u_{\mathrm{g}_{k}} - \varepsilon_{ijk}f_{j}\overline u_{k} + \varepsilon_{i3k}f_{3}u_{\mathrm{g}_{k}} + g\frac{\overline\theta_{v}-\langle\overline\theta_{v}\rangle}{\theta_{0}}\delta_{i3} -\frac{\partial\,\tau_{ij}}{\partial x_{j}} \begin{eqnarray} \overline q_{s}(\overline T_{l}) = 0.622\frac{\overline e_{s}(\overline T_{l})} {p_{0}(z)-0.377\,\overline e_{s}(\overline T_{l})} {p_{0}(z)-0.378\,\overline e_{s}(\overline T_{l})} \label{eq:qs3} \end{eqnarray} The hydrostatic pressure $p_{0}(z)$ is given by \cite{cuijpers93}: \begin{eqnarray} p_{0}(z) = p_{0}(z=0)\frac{T_{\mathrm{ref}}(z)^{c_{p}/R}}{T_{0}} p_{0}(z) = p_{0}(z=0)\left(\frac{T_{\mathrm{ref}}(z)}{T_{0}}\right)^{c_{p}/R} \label{eq:p_0} \end{eqnarray} \overline q_{l} = \begin{cases} \overline q - \overline q_{s}(\overline T_{l}) & \textnormal{if} \quad \overline q > \overline q_{s}(\overline T_{l}) \\ \overline q - \overline q_{s} & \textnormal{if} \quad \overline q > \overline q_{s} \\ 0  & \textnormal{else} \end{cases} against numerical data. \textit{J. Atmos. Sci.}, \textbf{38}, 2414-2428. \bibitem[Cox (1976)]{cox76} \textbf{Cox, S. K., 1976:} Observations of cloud infrared emissivity. \textbf{Cox, S. K., 1976:} Observations of cloud infrared effective emissivity. \textit{J. Atmos. Sci.}, \textbf{33}, 287-289. \bibitem[Cuijpers and Duynkerke (1993)]{cuijpers93}