- Timestamp:
- 2019-05-20T20:57:09+02:00 (5 years ago)
- Location:
- NEMO/trunk/doc/latex/SI3/subfiles
- Files:
-
- 1 edited
- 1 moved
Legend:
- Unmodified
- Added
- Removed
-
NEMO/trunk/doc/latex/SI3/subfiles/chap_radiative_transfer.tex
r9995 r11015 1 1 2 \documentclass[../ ../tex_main/NEMO_manual]{subfiles}2 \documentclass[../main/SI3_manual]{subfiles} 3 3 4 4 \begin{document} … … 28 28 \begin{center} 29 29 \vspace{0cm} 30 \includegraphics[height=6cm,angle=-00]{ ../Figures/radiative_transfer.png}30 \includegraphics[height=6cm,angle=-00]{radiative_transfer} 31 31 \caption{Partitionning of solar radiation in the snow-ice system, as represented in SI$^3$.} 32 32 \label{fig_radiative_transfer} … … 54 54 The user has control on 5 reference namelist values, which describe the asymptotic values of albedo of snow and ice for dry and wet conditions, as well as the deep ponded-ice albedo. Observational surveys, in particular during SHEBA in the Arctic \citep{Perovichetal02alb} and further additional experiments \citep{GrenfellPerovich04}, as well as by \cite{Brandtetal05} in the Antarctic, have provided relatively strong constraints on the surface albedo. In this context, the albedo can hardly be used as the main model tuning parameter, at least outside of these observation-based bounds (see namalb for reference values). 55 55 56 \ forfile{../namelists/namalb}56 \nlst{namalb} 57 57 58 58 %-------------------------------------------------------------------------------------------------------------------- … … 63 63 \begin{center} 64 64 \vspace{0cm} 65 \includegraphics[height=10cm,angle=-00]{ ../Figures/albedo_cloud_correction.png}65 \includegraphics[height=10cm,angle=-00]{albedo_cloud_correction} 66 66 \caption{Albedo correction $\Delta \alpha$ as a function of overcast sky (diffuse light) albedo $\alpha_os$, from field observations \cite[][their Table 3]{GrenfellPerovich04} (squares) and 2nd-order fit (Eq. \ref{eq_albedo_cloud_correction}). Red squares represent the irrelevant data points excluded from the fit. For indication, the amplitude of the correction used in the ocean component is also depicted (blue circle).} 67 67 % ocean uses 0.06 for overcast sky (Payne 74) and Briegleb and Ramanathan parameterization … … 94 94 \begin{center} 95 95 \vspace{0cm} 96 \includegraphics[height=4cm,angle=-00]{ ../Figures/albedo_dependencies.png}96 \includegraphics[height=4cm,angle=-00]{albedo_dependencies} 97 97 \caption{Example albedo dependencies on ice thickness, snow depth and pond depth, as parameterized in SI$^3$.} 98 98 \label{fig_albedo_dependencies} … … 183 183 \begin{center} 184 184 \vspace{0cm} 185 \includegraphics[height=8cm,angle=-00]{ ../Figures/radiation_atm_ice_oce.png}185 \includegraphics[height=8cm,angle=-00]{radiation_atm_ice_oce} 186 186 \caption{Framing solar radiation transfer through sea ice into the atmosphere-ice-ocean context.} 187 187 % ocean uses 0.06 for overcast sky (Payne 74) and Briegleb and Ramanathan parameterization
Note: See TracChangeset
for help on using the changeset viewer.