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Wenchang Yang edited beginequation_rho_c_.tex
over 8 years ago
Commit id: 578cebe3b10d1a4d675482761664efb2cb5a22ea
deletions | additions
diff --git a/beginequation_rho_c_.tex b/beginequation_rho_c_.tex
index 4494556..43b08d6 100644
--- a/beginequation_rho_c_.tex
+++ b/beginequation_rho_c_.tex
...
\begin{equation}
\rho c_p h
\frac{\partial{T}'}{\partial \frac{\partial\mathit{T}'}{\partial t} = R'_s + R'_l + LH' + SH' + D'_o \label{eqn:budget}
\end{equation}
where primes denote the historical$-$AMIP differences; $\rho$, $c_p$, $h$ and $T$ are the sea water density, specific heat at constant pressure, mixed layer depth and mixed layer average temperature, respectively; the left hand side is the heat storage tendency and the right hand side terms are the net short wave radiation, net long wave radiation, latent flux, sensible heat flux (defined as positive into the ocean) and the three-dimensional advection and diffusion by ocean dynamics, respectively.