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Wenchang Yang edited beginequation_rho_c_.tex
over 8 years ago
Commit id: 67a5a002e906141f474128ce5ec4194e3113d1f1
deletions | additions
diff --git a/beginequation_rho_c_.tex b/beginequation_rho_c_.tex
index 6f7bf05..3a3e739 100644
--- a/beginequation_rho_c_.tex
+++ b/beginequation_rho_c_.tex
...
\begin{equation}
\rho c_p h
\frac{\partial T'}{\partial t} \partial T'/\partial t = R'_s + R'_l + LH' + SH' + D'_o
\end{equation}\label{eqn:budget}
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.