Commit ee74eb7f authored by Marion Bandet's avatar Marion Bandet

update fig ADCP V50 20140506 experiment

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<div class="section" id="experiment-on-may-06-2014">
<h1>Experiment on May 06, 2014<a class="headerlink" href="#experiment-on-may-06-2014" title="Permalink to this headline"></a></h1>
<p>In this experiment, 8 buoys were deployed in the Lower Saint Lawrence Estuary (LSLE). Each buoy was instrumented with a GPS and a SPOT. Each buoy had its drogue at various depths in order to sample the water column.</p>
<p>On May 6, 2014, eight (8) buoys were deployed in the Lower Saint Lawrence Estuary. Each buoy was instrumented with a Global Positioning System (GPS) and a SPOT (<a class="reference external" href="https://www.findmespot.ca/en/">https://www.findmespot.ca/en/</a>). Each buoy was designed with a boyant surface float linked to a drogue via a chain. Three (3) different chain lengths were used in order to observe the effect of the dynamics of the water masses at various depths along the trajectories of the buoys. Each chain length (5, 205 and 750 cm, respectively) was duplicated. Additionally, two buoys were deployed without drogue and allowed to float freely at the water surface.
GPS were programmed to sample every 10 seconds and spots every 5 min.</p>
<p>The buoys were deployed by pairs of matching drogue&#8217;s depth, however due to satellite communication issues, not all GPSs provided data right after deployment. A delay of up to ?? min was observed.</p>
<p>A RDInstrument 300 kHz Acoustic Doppler Current Profiler (ADCP) was deployed for four (4) hours on May 7, 2014 while the buoys were drifting. The ADCP was mounted at the center of a donut-shaped float on a swivel ring to minimize the effects of pitch and roll. The ADCP was programmed to sample the water column using twenty-six (26) 0.5m bins. Vertical velocity profiles were exploited to compare with other estimates of velocity components.</p>
<p>A portable YSI CTD was used to sample vertical profiles of temperature and conductivity at 10 locations in the study area. The data were used to identify different water masses.</p>
<p>In addition, velocity field from MOGSL model output was obtained for comparison purposes.</p>
<p>Tides were obtained from <a class="reference external" href="http://tides.gc.ca/eng/data/table/2014/">http://tides.gc.ca/eng/data/table/2014/</a> at Rimouski.
Hourly wind data were downloaded from <a class="reference external" href="http://climat.meteo.gc.ca/">http://climat.meteo.gc.ca/</a> at station Pointe-au-Père, QC.
Simulated wave data were obtained from the wave model WAVEWATCH III (<a class="reference external" href="http://polar.ncep.noaa.gov/waves/index2.shtml">http://polar.ncep.noaa.gov/waves/index2.shtml</a>) outputs run at UQAR for the area of interest.</p>
<p>ADCP V50 data
/home/bandma01/Dropbox/UQAR/MEOPAR_Marion/Matlab_scripts/ADCP/html/ADCP_V50_May2014.html</p>
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<h1>Data from ADCP V50 (from routine<a class="headerlink" href="#data-from-adcp-v50-from-routine" title="Permalink to this headline"></a></h1>
<p>roll - pitch - heading</p>
<div class="figure align-center">
<img alt="_images/ADCP_V50_May2014_01.png" src="_images/ADCP_V50_May2014_01.png" />
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<img alt="_images/ADCP_V50_May2014_03.png" src="_images/ADCP_V50_May2014_03.png" />
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<img alt="_images/ADCP_V50_May2014_04.png" src="_images/ADCP_V50_May2014_04.png" />
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<img alt="_images/ADCP_V50_May2014_05.png" src="_images/ADCP_V50_May2014_05.png" />
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<p>range</p>
<div class="figure align-center">
<img alt="_images/ADCP_V50_May2014_08.png" src="_images/ADCP_V50_May2014_08.png" />
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<p>Percent Good</p>
<div class="figure align-center">
<img alt="_images/ADCP_V50_May2014_09.png" src="_images/ADCP_V50_May2014_09.png" />
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<p>Correlation</p>
<div class="figure align-center">
<img alt="_images/ADCP_V50_May2014_10.png" src="_images/ADCP_V50_May2014_10.png" />
</div>
<p>Intensity</p>
<div class="figure align-center">
<img alt="_images/ADCP_V50_May2014_11.png" src="_images/ADCP_V50_May2014_11.png" />
</div>
<p>Velocity (ENUErr)</p>
<div class="figure align-center">
<img alt="_images/ADCP_V50_May2014_12.png" src="_images/ADCP_V50_May2014_12.png" />
</div>
<p>Averaged velocity</p>
<div class="figure align-center">
<img alt="_images/ADCP_V50_May2014_13.png" src="_images/ADCP_V50_May2014_13.png" />
</div>
<p>Averaged Intensity</p>
<div class="figure align-center">
<img alt="_images/ADCP_V50_May2014_14.png" src="_images/ADCP_V50_May2014_14.png" />
</div>
<p>Averaged Correlation</p>
<div class="figure align-center">
<img alt="_images/ADCP_V50_May2014_15.png" src="_images/ADCP_V50_May2014_15.png" />
</div>
<p>Vertical Profiles of averaged velocity components</p>
<div class="figure align-center">
<img alt="_images/ADCP_V50_May2014_16.png" src="_images/ADCP_V50_May2014_16.png" />
</div>
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<img alt="_images/ADCP_V50_May2014_17.png" src="_images/ADCP_V50_May2014_17.png" />
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<img alt="_images/ADCP_V50_May2014_18.png" src="_images/ADCP_V50_May2014_18.png" />
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<img alt="_images/ADCP_V50_May2014_19.png" src="_images/ADCP_V50_May2014_19.png" />
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Experiment on May 06, 2014
==========================
In this experiment, 8 buoys were deployed in the Lower Saint Lawrence Estuary (LSLE). Each buoy was instrumented with a GPS and a SPOT. Each buoy had its drogue at various depths in order to sample the water column.
On May 6, 2014, eight (8) buoys were deployed in the Lower Saint Lawrence Estuary. Each buoy was instrumented with a Global Positioning System (GPS) and a SPOT (https://www.findmespot.ca/en/). Each buoy was designed with a boyant surface float linked to a drogue via a chain. Three (3) different chain lengths were used in order to observe the effect of the dynamics of the water masses at various depths along the trajectories of the buoys. Each chain length (5, 205 and 750 cm, respectively) was duplicated. Additionally, two buoys were deployed without drogue and allowed to float freely at the water surface.
GPS were programmed to sample every 10 seconds and spots every 5 min.
The buoys were deployed by pairs of matching drogue's depth, however due to satellite communication issues, not all GPSs provided data right after deployment. A delay of up to ?? min was observed.
A RDInstrument 300 kHz Acoustic Doppler Current Profiler (ADCP) was deployed for four (4) hours on May 7, 2014 while the buoys were drifting. The ADCP was mounted at the center of a donut-shaped float on a swivel ring to minimize the effects of pitch and roll. The ADCP was programmed to sample the water column using twenty-six (26) 0.5m bins. Vertical velocity profiles were exploited to compare with other estimates of velocity components.
A portable YSI CTD was used to sample vertical profiles of temperature and conductivity at 10 locations in the study area. The data were used to identify different water masses.
In addition, velocity field from MOGSL model output was obtained for comparison purposes.
Tides were obtained from http://tides.gc.ca/eng/data/table/2014/ at Rimouski.
Hourly wind data were downloaded from http://climat.meteo.gc.ca/ at station Pointe-au-Père, QC.
Simulated wave data were obtained from the wave model WAVEWATCH III (http://polar.ncep.noaa.gov/waves/index2.shtml) outputs run at UQAR for the area of interest.
ADCP V50 data
/home/bandma01/Dropbox/UQAR/MEOPAR_Marion/Matlab_scripts/ADCP/html/ADCP_V50_May2014.html
......
Data from ADCP V50 (from routine
*******************************************
roll - pitch - heading
.. figure:: figures/20140506/html/ADCP_V50_May2014_01.png
:align: center
.. figure:: figures/20140506/html/ADCP_V50_May2014_03.png
:align: center
.. figure:: figures/20140506/html/ADCP_V50_May2014_04.png
:align: center
.. figure:: figures/20140506/html/ADCP_V50_May2014_05.png
:align: center
range
.. figure:: figures/20140506/html/ADCP_V50_May2014_08.png
:align: center
Percent Good
.. figure:: figures/20140506/html/ADCP_V50_May2014_09.png
:align: center
Correlation
.. figure:: figures/20140506/html/ADCP_V50_May2014_10.png
:align: center
Intensity
.. figure:: figures/20140506/html/ADCP_V50_May2014_11.png
:align: center
Velocity (ENUErr)
.. figure:: figures/20140506/html/ADCP_V50_May2014_12.png
:align: center
Averaged velocity
.. figure:: figures/20140506/html/ADCP_V50_May2014_13.png
:align: center
Averaged Intensity
.. figure:: figures/20140506/html/ADCP_V50_May2014_14.png
:align: center
Averaged Correlation
.. figure:: figures/20140506/html/ADCP_V50_May2014_15.png
:align: center
Vertical Profiles of averaged velocity components
.. figure:: figures/20140506/html/ADCP_V50_May2014_16.png
:align: center
.. figure:: figures/20140506/html/ADCP_V50_May2014_17.png
:align: center
.. figure:: figures/20140506/html/ADCP_V50_May2014_18.png
:align: center
.. figure:: figures/20140506/html/ADCP_V50_May2014_19.png
:align: center
......@@ -240,9 +240,67 @@ No school
- same for PAB: Process_TimePeriod_wera.sh -s PAB -d 2014126 -f 2014130
- do_process_SORT_pol 2014126 2014130 /home/wera/data2/PAB
**1er fevrier 2016**
- transfer data on local machine from wera server
./do_filetransferssh.sh PAO 2014126 2014130
./do_filetransferssh.sh PAB 2014126 2014130
- departure for Calgary/Banff MEOPeer training meeting Feb 1-5, 2016
**10-11-12 feb, 2016**
- work on data processing and comparisons, correlation, RMS diff with new procesing in hope it will improve the data...
**17 feb, 2016**
- wrap up of last data analyis
- getting ready for field work
**18-19 feb, 2016**
- field work parc du Bic - BinWin 2016
**24-25-26 feb, 2016**
**2-3 Mar, 2016**
- spring break
**4 Mar, 2016**
**9-10-11 Mar 2016**
- Download data from wera server to create movie of combined currents
- work on script
- make movie: CombinedCurrents_20150421-20160203fig.avi
**16 Mar, 2016**
- modifiy script to make a monthly movie of combined currents
**17 Mar 2016**
- implemente script, generate movies for each month between April 2015 and January 2016
- update repository Matlab_scripts on gitlasso
- download .csv files from wera server
- make package for Louis Maltais with hourly data for Dec1-2 2015 (csv files + movie)
**18 Mar 2016**
- send package to Louis Maltais
- write paper of HF radars and buoy comparison
**29 Mar 2016**
- MEOPAR report for Dany
- work on paper
- comparison SPOT and GPS data with Paul (year 2014) for archive on Mingan
**30 Mar 2016**
- work on paper
- download tide data for may 2014
- download wind data for May 5, 6, 7, 8 2014
**6 & 7 jun 2016**
- work on paper: estimate coverage area of radial velocities for each site: HFR_coverage_May2014.m
- write bash script to transfer data from CODAR server to external HD: fileTransferCODAR.sh
- transfer data from PAP for May 1-10, 2014
- transfer data from STF fro May 1-10, 2014
- apply matlab routine make_ruv2matMBtest.m to convert binary data to .mat
- run HFR_coverage_May2014.m for PAO, PAB, PAP, STF
......@@ -359,6 +359,49 @@ No school</p>
- transfer data on local machine from wera server
./do_filetransferssh.sh PAO 2014126 2014130
./do_filetransferssh.sh PAB 2014126 2014130</p>
<ul class="simple">
<li>departure for Calgary/Banff MEOPeer training meeting Feb 1-5, 2016</li>
</ul>
<p><strong>10-11-12 feb, 2016</strong>
- work on data processing and comparisons, correlation, RMS diff with new procesing in hope it will improve the data...</p>
<p><strong>17 feb, 2016</strong>
- wrap up of last data analyis
- getting ready for field work</p>
<p><strong>18-19 feb, 2016</strong>
- field work parc du Bic - BinWin 2016</p>
<p><strong>24-25-26 feb, 2016</strong></p>
<p><strong>2-3 Mar, 2016</strong>
- spring break</p>
<p><strong>4 Mar, 2016</strong></p>
<p><strong>9-10-11 Mar 2016</strong>
- Download data from wera server to create movie of combined currents
- work on script
- make movie: CombinedCurrents_20150421-20160203fig.avi</p>
<p><strong>16 Mar, 2016</strong>
- modifiy script to make a monthly movie of combined currents</p>
<p><strong>17 Mar 2016</strong>
- implemente script, generate movies for each month between April 2015 and January 2016
- update repository Matlab_scripts on gitlasso
- download .csv files from wera server
- make package for Louis Maltais with hourly data for Dec1-2 2015 (csv files + movie)</p>
<p><strong>18 Mar 2016</strong>
- send package to Louis Maltais
- write paper of HF radars and buoy comparison</p>
<p><strong>29 Mar 2016</strong>
- MEOPAR report for Dany
- work on paper
- comparison SPOT and GPS data with Paul (year 2014) for archive on Mingan</p>
<p><strong>30 Mar 2016</strong>
- work on paper
- download tide data for may 2014
- download wind data for May 5, 6, 7, 8 2014</p>
<p><strong>6 &amp; 7 jun 2016</strong>
- work on paper: estimate coverage area of radial velocities for each site: HFR_coverage_May2014.m
- write bash script to transfer data from CODAR server to external HD: fileTransferCODAR.sh
- transfer data from PAP for May 1-10, 2014
- transfer data from STF fro May 1-10, 2014
- apply matlab routine make_ruv2matMBtest.m to convert binary data to .mat
- run HFR_coverage_May2014.m for PAO, PAB, PAP, STF</p>
</div>
......
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Experiment on May 06, 2014
==========================
In this experiment, 8 buoys were deployed in the Lower Saint Lawrence Estuary (LSLE). Each buoy was instrumented with a GPS and a SPOT. Each buoy had its drogue at various depths in order to sample the water column.
On May 6, 2014, eight (8) buoys were deployed in the Lower Saint Lawrence Estuary. Each buoy was instrumented with a Global Positioning System (GPS) and a SPOT (https://www.findmespot.ca/en/). Each buoy was designed with a boyant surface float linked to a drogue via a chain. Three (3) different chain lengths were used in order to observe the effect of the dynamics of the water masses at various depths along the trajectories of the buoys. Each chain length (5, 205 and 750 cm, respectively) was duplicated. Additionally, two buoys were deployed without drogue and allowed to float freely at the water surface.
GPS were programmed to sample every 10 seconds and spots every 5 min.
The buoys were deployed by pairs of matching drogue's depth, however due to satellite communication issues, not all GPSs provided data right after deployment. A delay of up to ?? min was observed.
A RDInstrument 300 kHz Acoustic Doppler Current Profiler (ADCP) was deployed for four (4) hours on May 7, 2014 while the buoys were drifting. The ADCP was mounted at the center of a donut-shaped float on a swivel ring to minimize the effects of pitch and roll. The ADCP was programmed to sample the water column using twenty-six (26) 0.5m bins. Vertical velocity profiles were exploited to compare with other estimates of velocity components.