diff --git a/latex/AlborexData.bib b/latex/AlborexData.bib
index ad0b5f11a67a5cf7a36e8554034fdc63d65b5b0b..b0b4d6b45918730762412eb3e95ff2f8b093c358 100644
--- a/latex/AlborexData.bib
+++ b/latex/AlborexData.bib
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@@ -1314,38 +714,6 @@ and Larnicol, G.},
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@@ -1505,67 +856,6 @@ and Larnicol, G.},
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Title = {{Report on operation and data analysis from multiplatform synoptic intensive experiment (AlborEx)}},
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diff --git a/latex/AlborexData_ESSD.tex b/latex/AlborexData_ESSD.tex
index 18413bd8e0a14c58e3ef300a5044a8711cf0dd23..006249b949e455566580f6a1ae2b1acf874b3407 100644
--- a/latex/AlborexData_ESSD.tex
+++ b/latex/AlborexData_ESSD.tex
@@ -2,11 +2,9 @@
%% ---------------------------------
%% This template should be used for copernicus.cls
%% The class file and some style files are bundled in the Copernicus Latex Package, which can be downloaded from the different journal webpages.
-\documentclass[final,essd,manuscript]{copernicus}
+\documentclass[final,essd]{copernicus}
\begin{document}
-\graphicspath{{../figures/}}
-
\title{The AlborEX dataset: sampling of submesoscale features in the Alboran Sea}
\Author[1]{Charles}{Troupin}
@@ -28,16 +26,6 @@
\Author[8]{Amala}{Mahadevan}
\Author[6,2]{Joaqu\'{i}n}{Tintor\'{e}}
-% OrcID's
-%Ananda: https://orcid.org/0000-0001-9476-9272
-%Simón: https://orcid.org/0000-0002-9395-9370
-%JoaquÃn: https://orcid.org/0000-0002-6311-0093
-%Pierre-Marie: https://orcid.org/0000-0003-1342-8463
-%John: https://orcid.org/0000-0001-7357-6623
-%Giulio https://orcid.org/0000-0002-8532-2097
-%Félix https://orcid.org/0000-0002-1205-3834
-%Antonio Olita: https://orcid.org/0000-0003-1302-8961
-%Antonio Tovar: https://orcid.org/0000-0003-4375-1982
\affil[1]{GeoHydrodynamics and Environment Research (GHER), Freshwater and OCeanic science Unit of reSearch (FOCUS), University of Li\`{e}ge, Li\`{e}ge, Belgium}
\affil[2]{Instituto Mediterr\'{a}neo de Estudios Avanzados (IMEDEA, CSIC-UIB), Esporles, Spain}
@@ -95,10 +83,10 @@ Section~\ref{sec:mission} strives to summarize the motivations behind the sampli
The mission took place from May 25 to May 31, 2014 in the Alboran Sea frontal system \citep[][see Fig.~\ref{fig1:general}]{CHENEY78,TINTORE91}, scene of the confluence of Atlantic and Mediterranean waters. The mission itself is extensively presented in \citet{RUIZ2015} and the features and processes captured by the observations are discussed in \citet{PASCUAL2017}. \citet{OLITA17} examined the deep chlorophyll maximum variation combining the bio-physical data from the gliders and the profiling floats. The present papers focuses solely on the description of the original dataset, graphically summarised in Fig.~\ref{fig1:general}).
-\begin{figure}[t]
+\begin{figure*}[t]
\includegraphics[width=.95\textwidth]{fig01.png}
\caption{Area of study, positions and trajectories of the main platforms. The close-up view on displays the glider and the CTD measurements.\label{fig1:general}}
-\end{figure}
+\end{figure*}
\subsection{General oceanographic context}
@@ -106,10 +94,10 @@ The definitive sampling area was not firmly decided until a few days before the
The pair of images indicates that the front position slightly changed between May 25 and 30. An anticyclonic eddy centered around 36$^{\circ}$30'N, 0$^{\circ}$30'W, according to altimetry data (not shown), slowly followed an eastward trajectory in the following days. Other SST images during the period of interest (not shown here) displayed different temperature values near the front, yet the front position remains stable.
-\begin{figure}[t]
+\begin{figure*}[t]
\includegraphics[width=.95\textwidth]{fig02.png}
\caption{Sea surface temperature in the western Mediterranean Sea from MODIS sensor onboard Aqua satellite corresponding to May 25 and 30, 2014. The dashed black line indicates the approximative position of the front based on the temperature gradient for the period 25--30 May. Level-2, 11 $\mu m$, night-time images were selected. Only pixels with a quality flag equal to 1 (good data) were conserved and represented on the map. The same front position is used in the subsequent figures.\label{fig2:SST}}
-\end{figure}
+\end{figure*}
\subsection{Design of the experiment}
@@ -396,10 +384,10 @@ The vessel's velocity is one or two order or magnitudes greater than the current
The application of all these tests lead to Fig~\ref{fig9b:adcpQC}, which illustrates the QF during the whole mission. The 3 main periods during which the ADCP was turned off are shown as grey areas. In addition, no measurements are available in the first meters of the water column, due to the position of the ADCP on the ship, at a depth of approximately 2~m.
-\begin{figure}[ht]
+\begin{figure*}[ht]
\includegraphics[width=.95\textwidth]{fig12.png}
\caption{Quality flags for the velocity measurements. The areas marked with a $\times$ are those during which the VM-ADCP was no acquiring measurements.\label{fig9b:adcpQC}}
-\end{figure}
+\end{figure*}
Overall the quality of the data tends to deteriorate when the depth increases, as reflected by the bad and missing values. In the first 200~m, about 95\% of the measurements are considered as good. Below 200~m, the ratio drops to 57\% with more than 21\% of missing values. Note that the flags 5 (, 7 and 8 were not used in this case but kept in the plot.
@@ -418,7 +406,7 @@ The original data files (i.e. obtained directly from the sensors and with a form
\subsection{File naming}
In order to keep the file names consistent with the original database, it is decided to keep the same file names as those assigned by SOCIB Data Center. Let us decompose one file name into its different parts:\\
-\texttt{dep0007\_socib-rv\_scb-sbe9002\_L1\_2014-05-25.nc}
+\texttt{dep0007\_socib-rv\_scb-sbe9002\_L1\_2014-05-25}
\begin{description}
\item[\tt dep0007] indicates the number of the deployment, where deployment is the equivalent to the start of a mission or survey with a given platform. The deployment ends when the mission is over or if the platform stops acquiring data.
\item[\tt socib-rv] is the code for the platform, in this case the SOCIB coastal research vessel.
@@ -512,545 +500,15 @@ A set of programs in Python to read the files and represent their content as in
\disclaimer{The authors do not accept any liability for the correctness and appropriate interpretation of the data or their suitability for any use.}
\begin{acknowledgements}
-AlborEx was conducted in the framework of PERSEUS EU-funded project (Grant agreement no.~287600). Glider operations were partially funded by JERICO FP7 project. AP acknowledges support from the Spanish National Research Program (E-MOTION/CTM2012-31014 and PRE-SWOT/CTM2016-78607-P). SR and AP are also supported by the Copernicus Marine Environment Monitoring Service (CMEMS) MedSUB project. AO was supported by the Jerico-TNA program, through the FRIPP (FRontal Dynamics Influencing Primary Production) project. The profiling floats and some drifters were contributed by the Argo-Italy program. The proceedings of such an ambitious mission would not have been possible without the involvement of a numerous staff both at sea and on land: A.~Massanet, M.~Palmer, I.~Lizaran, C.~Castilla, P.~Balaguer, M.~Menna, K.~Sebastián, S.~Lora, and A.~Bussani .
+We wish to thank the three anonymous reviewers for their constructive comments and the extensive check of the data files. AlborEx was conducted in the framework of PERSEUS EU-funded project (Grant agreement no.~287600). Glider operations were partially funded by JERICO FP7 project. AP acknowledges support from the Spanish National Research Program (E-MOTION/CTM2012-31014 and PRE-SWOT/CTM2016-78607-P). SR and AP are also supported by the Copernicus Marine Environment Monitoring Service (CMEMS) MedSUB project. AO was supported by the Jerico-TNA program, through the FRIPP (FRontal Dynamics Influencing Primary Production) project. The profiling floats and some drifters were contributed by the Argo-Italy program. The proceedings of such an ambitious mission would not have been possible without the involvement of a numerous staff both at sea and on land: A.~Massanet, M.~Palmer, I.~Lizaran, C.~Castilla, P.~Balaguer, M.~Menna, K.~Sebastián, S.~Lora, and A.~Bussani .
\end{acknowledgements}
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+\bibliographystyle{copernicus}
+\bibliography{AlborexData.bib}
\end{document}