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Commit dc8d3a70 authored by Lionel GUEZ's avatar Lionel GUEZ
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Polish

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......@@ -79,7 +79,7 @@ that date index, or by a unique integer identifier $n$, which we can call a
The date index $d$ is an integer value. It is a number of time steps
since some arbitrary reference date. For flexibility, we do not assume
that the reference date is the first date of the dataset. So $d$ may
not be 0 for the first date of the dataset.
not be 0 for the first date of the dataset. $d$ can be negative.
For Aviso data, the time step is one day and the reference date would
be conveniently January \nth{1}, 1950, since it is the reference date
......@@ -104,10 +104,10 @@ is:
\begin{equation*}
n = d E + e
\end{equation*}
So $n \ge 1$ and usually jumps at each change of date. The
anticyclones at the first date have a node index between 1 and $E$, at
the second date between $E + 1$ and $2 E$, and so on. Same for
cyclones. Cf. table (\ref{tab:eddy_id_Matlab}).
So $n$ usually jumps at each change of date. The eddies at date 0 (if
date 0 is in the range of dates) would have a node index between 1 and
$E$, at date 1 between $E + 1$ and $2 E$, and so on. Cf. table
(\ref{tab:eddy_id_Matlab}).
\begin{table}[htbp]
\centering
\begin{tabular}{lll}
......@@ -115,12 +115,12 @@ cyclones. Cf. table (\ref{tab:eddy_id_Matlab}).
& anticyclones & $n = 1, \dots, e_\mathrm{max,anti}(0)$ \\
& cyclones & $n = 1, \dots, e_\mathrm{max,cyclo}(0)$ \\
date index d & & \\
& anticyclones & $n = d E + 1, \dots, d
E + e_\mathrm{max,anti}(d)$ \\
& cyclones & $n = d E + 1, \dots, d E
& anticyclones & $n = d E_\mathrm{anti} + 1, \dots, d
E_\mathrm{anti} + e_\mathrm{max,anti}(d)$ \\
& cyclones & $n = d E_\mathrm{cyclo} + 1, \dots, d E_\mathrm{cyclo}
+ e_\mathrm{max,cyclo}(d)$
\end{tabular}
\caption{Node indices. $d$ is the date index.}
\caption{Node indices}
\label{tab:eddy_id_Matlab}
\end{table}
Conversely, from the definition of $E$, knowing $n$ and $E$, we can
......
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