README FILE FOR BERING STRAIT MOORING DATA                           May 
2019
=============================================================================
12345678901234567890123456789012345678901234567890123456789012345678901234567
Bering Strait Moorings 2017-2018

This is an archive of data from moorings deployed in Bering Strait from
summer 2017 to summer 2018.

Mooring deployments were funded by the NSF-Arctic Observing Network
award PLR-1304052 (PI: Woodgate, Heimbach and Nguyen).

The mooring work required 2 dedicated cruises:
- in 2017 (7th - 15th July), a ~ 9 day cruise on the US vessel
Norseman2 deployed the moorings.  Some CTD sections were run on this 
cruise,
and those data are archived separately.
- in 2018 (10th - 19th August), a ~ 10 day cruise on the US vessel
Norseman2 deployed the moorings.  Some CTD sections were run on this 
cruise,
and those data are archived separately.

For 2017 to 2018, a total of three moorings were deployed:
- two moorings (A2 and A4) in the US channel of the strait,
- one mooring (A3) at a site just north of the strait.
In what follows, mooring names include a two digit suffix to represent
year of deployment.

Sites A2, and A3 were established in 1990. A2 and A3 have been occupied
almost continuously (all years except 96-97) since then. Site A4
was established in 2001.
Mooring location A2 is in the middle of the eastern (Alaskan side) 
channel.
Mooring location A3 is just north of the strait, immediately east of the
Russian-US EEZ (Exclusive Economic Zone) line.
Experience has shown that site A3 samples both eastern and western
channel water.
Mooring location A4 is close to the Alaskan coast and allows
measurement of the Alaskan Coastal Current.

For an overview of previous and on-going Bering Strait mooring work,
please see http://psc.apl.washington.edu/BeringStrait.html.

Moorings carry a variety of instruments, listed in the table below.
All records are year-round, sampling hourly or more frequently (Time
Int. in table below).
Data from instruments marked with * are not included in this archive.
For access to these data, please contact the named PI in list below table.

12345678901234567890123456789012345678901234567890123456789012345678901234567
--------------------------------------------------------------------------
ID  Deployed Latitude  Longitude  Instrument      S/N  Time   Inst.  Water
     in Year   (N)        (W)                          Int.   Depth Depth
--------------------------------------------------------------------------

A3-17  2017  66 19.59  168 57.13  ISCAT         14906   5min   16m    57m
                                  ISCAT-Logger     22  30min   ...    57m
                                  300kHz-ADCP    2234  30min   43m    57m
                                  SBE16          1698  60min   43m    57m
                                  AURAL M2*      94LF    -     49m    57m

A2-17  2017  65 46.88  168 34.08  ISCAT         14905   NR     15m    55m
                                  ISCAT-Logger     21  30min   ...    55m
                                  300kHz-ADCP    2269  30min   44m    55m
                                  SBE16          2341  60min   49m    55m
                                  AURAL M2*     246LF   -      49m    55m

A4-17  2017  65 44.76  168 15.78  ISCAT         14907   NR     16m    48m
                                  ISCAT-Logger     24  30min   ...    48m
                                  300kHz-ADCP    2232  30min   37m    48m
                                  SBE16          1700  60min   41m    48m
                                  APL Marine Rec*  01    -     43m    48m
--------------------------------------------------------------------------
Depths are estimated from mooring design and pressure sensors where 
available,
and are good to 1-2m.
  NR=instrument not recovered     ND=No data
Instruments with data included here:
 ISCAT - SBE37IM in ice resistant float, telemetering data inductively to
   a Logger below (system developed at APL-UW)
 300KHz-ADCP - 300kHz RDI/Teledyne Workhorse Acoustic Doppler Current 
Profiler
 SBE37 Microcat - Seabird SBE 37 Temperature Salinity Pressure recorder
 SBE16woptic - Seabird SBE16plus with optical data (including some or all 
of
               fluorescence, turbidity, transmissivity and PAR) - see 
headers
 SBE26p-BPG - Seabird SBE26plus Bottom Pressure Gauge
 RCM9Turb - Aanderaa RCM9 acoustic current meter with turbidity sensor
 RCM9LW   - Aanderaa Lightweight RCM9 acoustic current meter
Instruments with data not included here:
 AARI-CM&CTD - Current meter and CTD from AARI (Arctic and Antarctic 
Research
               Institute, Russia), PI: Igor Lavrenov, AARI
 ISUS - ISUS Nitrate sensor, PI: Terry Whitledge, UAF
 AURAL M2* - Aural Marine Mammal Acoustic Recorder, PI: Kate Stafford, UW
 APL Marine Rec* - APL Marine Recorder, PI: Kate Stafford, UW.

Each data file contains the data from one instrument-year - the listed 
year
in the mooring name is the year in which the mooring was deployed.

For RCMs and SBEs, calibrated data are recorded in one file per instrument
per year, with naming convention:
   BeringStrait_yyyy_ID_III_#####.ttt
yyyy=Deployment year; ID=mooring ID; III=instrument type; #####=serial 
number;
ttt=indicates calibration, with .pre=pre-deployment calibration used,
.ppp=pre and post deployment calibrations merged.
The SBE-16 and 37 hexidecimal files (unaltered from the download) are also
included, indicated by extension .hex or .asc

For the ADCPs, there are multiple files per instrument.
   BeringStrait_yyyy__ID_#####ADCPraw.000 = Binary download from the ADCP
(see notes below for multiple .000 files)
   BeringStrait_yyyy__ID_#####_ADCPdeploytests.txt = pre deployment tests
   BeringStrait_yyyy__ID_#####_ADCPrecoverytest.txt = post deployment 
tests
The remainder are ASCII conversions of the data, corrected for clock drift
and magnetic declination.
   BeringStrait_yyyy__ID_#####.btm = ASCII bottom track data
        (including ice range and velocity)
   BeringStrait_yyyy__ID_#####.ins = ASCII instrument data
        (e.g. heading, pitch, roll, temperature)
   BeringStrait_yyyy__ID_#####_bin01.rdat = ASCII water velocity data in 
Bin 1
   BeringStrait_yyyy__ID_#####.bin02.rdat = ASCII water velocity data in 
Bin 2
    etc.  (Bin depths are given in the data files)
Header information is included in each data file.

-----------------------------------------------------------------------------
For details of the measurements and their interpretation, please see:
   Woodgate, R.A., K.M.Stafford and F.G.Prahl (2015) A synthesis of
   year-round interdisciplinary mooring measurements in the Bering
   Strait (1990-2014) and the RUSALCA years (2004-2011), Oceanography
   28(3):46-67, doi:10.5670/oceanog.2015.57
and
   Woodgate, R.A., 2018, Increases in the Pacific inflow to the Arctic 
   from 1990 to 2015, and insights into seasonal trends and driving 
   mechanisms from year-round Bering Strait mooring data, 
   Progress in Oceanography, 160, 124-154, 
doi:10.1016/j.pocean.2017.12.007.

Please use both 2015 and 2018 citations for these data.

For an overview of cruises and project, please see:
   http://psc.apl.washington.edu/BeringStrait.html

For relevant papers, please see:
Roach, A.T., K. Aagaard, C. H. Pease, S.A. Salo, T. Weingartner, V. 
Pavlov,
   and M. Kulakov (1995) Direct measurements of transport and water 
properties
   through Bering Strait, J. Geophys. Res., 100, 18,443-18,457.
Woodgate, R.A., and K. Aagaard (2005) Revising the Bering Strait 
freshwater
   flux into the Arctic Ocean, Geophys. Res. Lett., 32, L02602,
   doi:10.1029/2004GL021747.
Woodgate, R.A., K. Aagaard, and T. Weingartner (2005) Monthly temperature,
   salinity, and transport variability of the Bering Strait throughflow,
   Geophys. Res. Lett., 32, No. 4, L04601, doi:10.1029/2004GL021880.
Woodgate, R. A., K. Aagaard, and T. J. Weingartner (2005) A year in the
   physical oceanography of the Chukchi Sea: Moored measurements from 
autumn
   1990-1991,Deep-Sea Res., Part II, 52, 3116-3149,
   doi: 10.1016/j.dsr2.2005.10.016.
Woodgate, R. A., K. Aagaard, and T. J. Weingartner (2006) Interannual 
changes
   in the Bering Strait fluxes of volume, heat and freshwater between 1991
   and 2004, Geophys. Res. Lett., 33, L15609, doi:10.1029/2006GL026931.
Woodgate, R. A., T. Weingartner, and R. Lindsay (2010), The 2007 Bering
   Strait oceanic heat flux and anomalous Arctic sea-ice retreat,
   Geophys. Res. Lett., 37, L01602, doi:10.1029/2009GL041621.
Woodgate, R.A., T. Weingartner, and R. Lindsay (2012), Observed increases
   in Bering Strait oceanic fluxes from the Pacific to the Arctic from
   2001 to 2011 and their impacts on the Arctic Ocean water column,
   Geophys. Res. Lett., 39, L24603, doi:10.1029/2012GL054092.
Woodgate, R.A., (2018), Increases in the Pacific inflow to the Arctic from
   1990 to 2015, and insights into seasonal trends and driving mechanisms
   from year-round Bering Strait mooring data, Progress in Oceanography,
   160, 124-154,  doi:10.1016/j.pocean.2017.12.007.


For queries, please contact:
   Rebecca Woodgate   woodgate@uw.edu   (206) 221-3268
   Polar Science Center, Applied Physics Lab, University of Washington
   1013 NE 40th, Seattle, WA  98105-6698   USA

------------------------------------------------------------------------------

Meta data
=========

1) Platform: Subsurface oceanographic moorings

2) Project title: Bering Strait

3) Data collection dates: July 2017 to August 2018

4) PI:   Rebecca Woodgate (woodgate@uw.edu)

5) Data collection method:
     Year-round moorings carrying
     - Sea-Bird temperature/conductivity and pressure recorders (SBE)
     - RDI 300kHz Workhorse Acoustic Doppler Current Profilers (ADCP)
     - APL data loggers for inductive data from ISCAT system

6) Data calibration method:
     Unless noted otherwise in the header on each data file, timestamps
     have been corrected for observed instrument clock drift.
     All times are given in GMT.
     For SBEs, calibration coefficients are given in header file.

  SBEs:
     - Generally pre and post calibrated by the manufacturer (indicated
       by suffix .ppp)
     - pre and post calibrations linearly time-weighted through the
       deployment.
     - .pre suffix indicates only pre-cruise calibration used
     - just prior to recovery, a CTD cast was performed in the vicinity
       of the mooring as an attempt to provide and inwater calibration.
       Immediately after recovery, SBE instruments were placed in a 
stirred
       tank of sea water, to check immediate post deployment calibrations
       (figure included here).  These are both just informational checks
       to assess how well the post-cruise manufacturer's calibration 
captures
       the final in-water state. The final post-cruise calibration used is
       that from the manufacturer.

  ADCPS:  Tested by APL/manufacturer pre deployment.
     - compasses calibrated as per manufacturer's
       specifications in Seattle prior to deployment.  Estimated
       compass error is included in the header file
     - where available, at sea compass check also included in header file
     - direction corrected to true north, magnetic declination used is 
cited
       in the header.
     - data requiring speed of sound in water is corrected by the ADCP 
using
       the water temperature measured by the ADCP.
     - intensity of returned signals is not specially calibrated.

7) Instrumentation used:  (see table for sampling frequencies)
     Sea-Bird SBE16 recorders
     ISCAT loggers (SBE37 Microcat logging data to an APL-Logger)
     RDI 300 kHz Workhorse ADCP - bin size typically 2m (but see 
exceptions below)

8) Quality control procedures:
     Quality control provided by Rebecca Woodgate.
     ADCP data rely on ADCP internal temperature for speed of sound
       corrections.
     ADCP Data files are included for all bins up to the surface although
       bins near the surface contain much larger errors (likely due to
       surface effects) and should be treated with caution.

9) Data format:
     SBE data - ASCII, format given in individual headers
        (uncalibrated "hex" or "asc" data also included for SBEs)
     ADCP data - 2 formats: a) BINARY download file from ADCP and
                            b) ASCII conversion of these files (in 2m 
bins)

10) Data collection problems:
    By Mooring:
      - no significant problems.  All moorings released without incident. 
      - biofouling is a typical issue in the strait, but
    biofouling was moderate this year.  For these recoveries, A2-17
    was the most heavily fouled.  Fouling was mostly by barnacles, up
    over 2cm long, with some bryozoam-like growth on several parts of
    the moorings.  Overall, release hooks and salinity cells were 
generally
    clear of biofouling, with some exceptions (see below). As discussed 
    below, salinity drifts are still significant.
    Photographic documentation of biofouling on recovery is available
    via cruise reports, included here and on the Bering Strait website:
    http://psc.apl.washington.edu/BeringStrait.html.


    By Instrument:

    === ISCATS (Loggers and SBE37s)
       A217  - SBE37  14905 - lost 28th Jan 2019, coupler also lost
             - Logger 21 - Data good
                 - logger clock 14min slow by end of deployment, but
                   time stamps taken from SBE37
                 - post cal not available, but other data show sensor        
                   drift in the strait may be as large as 0.05-0.1psu too      
                   fresh by end of year deployment                             
                 - comparison to underlying SBE in winter suggests           
                   no salinity drift issues                                    

       A317  - SBE37 14906 - recovered 
                 - bad biofouling, sensor intake still clear on recovery, 
                   but exit was blocked with small mussels                                  
                 - clock 0 min fast by end of deployment                     
                 - post cal shows salinity change of 0.08psu
			 - record linearly interpolated between pre & post 
cals      
			 - final data ~0.04psu fresher than reference in 
recovery testtank  
                 - final data ~0.2psu fresher than recovery CTD, but 
temperature also 
			   different on this case, so CTD may be sampling 
other waters
                 - final data often denser than underlying SBE, suggesting          
                   ~0.1psu error, between iscat and sbe combined and 
winter freezing point 
                   temperatures suggest this is most likely an error in 
the sbe calibration     
             - Logger 22 - Data good, but only SBE37 data given here

       A417  - SBE37  14907 - lost 11th Jan 2018, coupler also lost
             - Logger 24 - Data good
                 - logger clock 18min slow by end of deployment, but
                   time stamps taken from SBE37
                 - post cal not available, but other data show sensor        
                   drift in the strait may be as large as 0.05-0.1psu too      
                   fresh by end of year deployment                             
                 - comparison to underlying SBE in winter suggests           
                   no salinity drift issues                                    

   === ADCPs
      Note that ADCP range measurements are not corrected
      for pitch and roll.  For full discussion and correction,
      see: Woodgate and Holroyd, 2011, included in archive.


      A217_adcp02269
         - ran on original (2m bin and bottom tracking) plan from
         deployment until 23:00 7th May 2018, and then stopped
         - restarted at 03:11 on 16:11 8th May 2018 on a factory
         plan (4m bins, no bottom track) having also lost individual
         compass calibration, and thus running on factory compass
         calibration.  
         - separate files are included for the first and second
         parts of the deployment (p1 and p2)
         For the first part (p1):
         - post deployment compass check not available as plan changed
         - bin 1 has high velocity errors
         - bin 11 has some high velocity errors
         - pitch and roll generally < 10 deg, peaking at 20 deg
         - range measurements not corrected for pitch and roll
         - data generally good until Bin15 (~12m)
         - temperature data not quality controlled
         For the second part (which has 4m bins) 
         - using factory compass calibration, but at sea tests suggest
         good to ~ 5deg
        - data generally good until bin7 or 8 (~14-10m) 

      A317_adcp02234
         - returned a full year of data and was still recording on
         recovery.  
         - bin 1 has high velocity errors
         - pitch and roll generally < 10 deg, peaking at 20 deg
         - pitch is typically ~ 5deg likely due to SBE on frame
        - range measurements not corrected for pitch and roll
         - data generally good until Bin14 (~13m)
         - temperature data not quality controlled

      A417_adcp02232
         - although one of the power pins on the communications plug
         was corroded away, this ADCP functioned well throughout
         the deployment and was still recording on recovery
         - bin 1 has some high velocity errors
         - pitch and roll generally < 10 deg, peaking at 20 deg
         - range measurements not corrected for pitch and roll
         - data generally good until Bin12 (~11m)
         - temperature data not quality controlled

    === SBE16
       A217_2341
         - on recovery, cell top clear, bottom with exterior growth  
         - 0.07 psu change between pre and post cals
         - record linearly interpolated between pre & post cals      
         - final data ~0.05psu fresher than reference in recovery testtank  
         - final data ~0.05psu fresher than recovery CTD                    
         - final data consistent with overlying iscat 
         - 4 obvious temperature spikes removed from raw data        
           by interpolation at records 5619, 6821, 6979, 7303          
                      
       A317_1698
         - on recovery, cell clear 
         - 0.09 psu change between pre and post cals
         - record linearly interpolated between pre & post cals      
         - final data ~0.04psu fresher than reference in recovery testtank  
         - final data ~0.15psu fresher than recovery CTD but temperature 
also 
	      different on this case, so CTD may be sampling other waters
         - final data often less dense than overlying iscat, suggesting          
           ~0.1psu error, between iscat and sbe combined, and winter 
           freezing point temperatures suggest this is most likely an 
error 
           in the sbe calibration                      
                     
       A417_1700
         - on recovery, cell top clear, bottom partially blocked  
         - 0.14 psu change between pre and post cals
         - record linearly interpolated between pre & post cals      
         - final data ~0.03psu fresher than reference in recovery testtank  
         - final data in agreement with recovery CTD                    
         - final data consistent with overlying iscat 


11) Other related data sets:
       This data set is a continuation of mooring measurements made in the
       Bering Strait almost continuously since 1990.  Mooring data have
       already been archived via the SBI project, managed by JOSS/EOS,
       and at NODC.
       For details see
        http://psc.apl.washington.edu/BeringStrait.html
        http://www.eol.ucar.edu/projects/sbi/
        http://sbi.utk.edu/
        http://www.nodc.noaa.gov
       Since 2000, CTD sections have been run in the Bering Strait on
       the mooring cruises.  This data is also accessible via the http
       links above.

12) Conditions for use or citation:
       Data freely available
       Please, as a courtesy, contact the PIs before using these data and 
cite as
       Woodgate et al., 2015 and Woodgate, 2018, viz:
           Woodgate, R.A., K.M.Stafford and F.G.Prahl (2015) A synthesis 
of
             year-round interdisciplinary mooring measurements in the 
Bering
             Strait (1990-2014) and the RUSALCA years (2004-2011), 
Oceanography
             28(3):46-67, doi:10.5670/oceanog.2015.57
       and
           Woodgate, R.A., 2018, Increases in the Pacific inflow to the 
Arctic 
             from 1990 to 2015, and insights into seasonal trends and 
driving 
             mechanisms from year-round Bering Strait mooring data, 
             Progress in Oceanography, 160, 124-154, 
doi:10.1016/j.pocean.2017.12.007.

13) Data qualifications or warnings:
       See also Data collection problems.
       For data issues relevant to a specific deployment, see the
       individual headers.  In general:
       SBE data: Standard Sea-Bird limitations apply
            - estimated accuracy 0.02 deg C, 0.0012 S/m
              (corresponding to 0.02 psu), and < 1 db.
            - see header files for difference between pre and post 
calibration
              which are usually 0.03 psu or greater.
            - Note that post-calibrations on the SBE16s
              suggests salinity sensor drift during deployment of between
              0.02 and 0.1psu, and this should be considered if post
              calibrations are not available
            - Note also that clogging of the salinity cell during
              deployment will not be captured by the post calibration
              and thus generally ends of records should be suspected
              for anomalously low salinities, especially if the SBE
              is not mounted vertical.
       ADCP data: Standard RDI limitations apply
            - estimated accuracy
              ~ 0.5 cm/s for water velocities (~100 pings per ensemble)
              Estimated errors (given in the files) vary with bin and time
              ~ 1 cm/s for ice velocities (2 or 5 pings per ensemble)
              Estimated errors (given in the files) vary with time
              ~ 1 deg in direction (see header files)
              Range to ice - accurate to 1% of range to surface (i.e. ~ 
0.4 m)
              ~ 0.4 deg C in temperature
              Note that ADCP range measurements are not corrected
              for pitch and roll.  For full discussion and correction,
              see: Woodgate and Holroyd, 2011, included in archive.

14) Grant numbers:
      Mooring sponsorship came from
      - National Science Foundation (NSF) Arctic Observing Network (AON)
      program, grant PLR-1304052 (PI: Woodgate, Heimbach and Nguyen)

15) Sample repository locations:
        National Ocean Data Center (http://www.nodc.noaa.gov)
        University of Washington (http://psc.apl.washington.edu/HLD)

16) Please use the following 2 citations for these data:
   Woodgate, R.A., K.M.Stafford and F.G.Prahl (2015) A synthesis of
       year-round interdisciplinary mooring measurements in the Bering
       Strait (1990-2014) and the RUSALCA years (2004-2011), 
       Oceanography, 28(3):46-67, doi:10.5670/oceanog.2015.57
and
   Woodgate, R.A., 2018, Increases in the Pacific inflow to the Arctic 
       from 1990 to 2015, and insights into seasonal trends and driving 
       mechanisms from year-round Bering Strait mooring data, 
       Progress in Oceanography, 160, 124-154, 
       doi:10.1016/j.pocean.2017.12.007.

==============================================================================

==============================================================================

FILE LISTING
=============

Total number of files:  113 including 5 subdirectories

Size (b)   Name
---------  ----
= Metadata file (1 file)
    30920  Bering_Strait_Moorings_2017-2018_NSFAON_ReadMe.txt

= Cruise reports (2 files) and 1 technical note (1 file)
 15004519  
BeringStrait2017CruiseReport_Norseman2_22ndJuly2017witheventlog.pdf
  7397725  BeringStrait2018CruiseReport_Norseman2_23rdMay2019withEL.pdf
  1853097  WoodgateandHolroyd2011_BTrangeCorrection.pdf

= ISCAT data  (4 files)
  - 2 ICLog*.pre of pre calibrated logger data
  - 1 ICsbe37*.ppp pre-post calibrated SBE37 data
  - 1 ICsbe37*.asc raw SBE37 data
   778082  BeringStrait_2017_A2_ICLog21_14905.pre
  9848495  BeringStrait_2017_A3_ICsbe37_14906.ppp
  6233786  BeringStrait_2017_A3_ISCsbe37_14906raw.asc
   719724  BeringStrait_2017_A4_ICLog24_14907.pre

= SBE16 (6 files)
  - 3 .hex files of raw data
  - 3 .ppp files of pre-post calibrated data
  (see also con file directory)
   813186  BeringStrait_2017_A2_sbe16_2341.ppp
   194006  BeringStrait_2017_A2_sbe16_2341raw.hex
   812980  BeringStrait_2017_A3_sbe16_1698.ppp
   193982  BeringStrait_2017_A3_sbe16_1698raw.hex
   812942  BeringStrait_2017_A4_sbe16_1700.ppp
   193982  BeringStrait_2017_A4_sbe16_1700raw.hex

.. and the 5 subdirectories,

One subdirectory of SBE .con calibration files
./BeringStrait_2017_SBEconfiles:
   - 6 calibration files for SBEs
 4764  1698posJan19.con
 4761  1698preAug16.con
 4763  1700posJan19.con
 4770  1700preAug16.con
 4765  2341posJan16.con
 4765  2341preNov15.con

Four subdirectories of ADCP data, naming conventions
as described above, containing also 2 subdirectories of
raw instrument files:

./BeringStrait_2017_A2_adcp2269_part1:
  3465289  BeringStrait_2017_A2_02269_p1.btm
  1789237  BeringStrait_2017_A2_02269_p1.ins
  2612567  BeringStrait_2017_A2_02269_p1_bin01.rdat
  2612567  BeringStrait_2017_A2_02269_p1_bin02.rdat
  2612567  BeringStrait_2017_A2_02269_p1_bin03.rdat
  2612567  BeringStrait_2017_A2_02269_p1_bin04.rdat
  2612567  BeringStrait_2017_A2_02269_p1_bin05.rdat
  2612567  BeringStrait_2017_A2_02269_p1_bin06.rdat
  2612567  BeringStrait_2017_A2_02269_p1_bin07.rdat
  2612567  BeringStrait_2017_A2_02269_p1_bin08.rdat
  2612567  BeringStrait_2017_A2_02269_p1_bin09.rdat
  2612567  BeringStrait_2017_A2_02269_p1_bin10.rdat
  2612567  BeringStrait_2017_A2_02269_p1_bin11.rdat
  2612567  BeringStrait_2017_A2_02269_p1_bin12.rdat
  2612567  BeringStrait_2017_A2_02269_p1_bin13.rdat
  2612567  BeringStrait_2017_A2_02269_p1_bin14.rdat
  2612567  BeringStrait_2017_A2_02269_p1_bin15.rdat
  2612567  BeringStrait_2017_A2_02269_p1_bin16.rdat
  2612567  BeringStrait_2017_A2_02269_p1_bin17.rdat
  2612567  BeringStrait_2017_A2_02269_p1_bin18.rdat
  2612567  BeringStrait_2017_A2_02269_p1_bin19.rdat
  2612567  BeringStrait_2017_A2_02269_p1_bin20.rdat
  2612567  BeringStrait_2017_A2_02269_p1_bin21.rdat
  2612567  BeringStrait_2017_A2_02269_p1_bin22.rdat
    36172  BeringStrait_2017_A2_02269part1_ADCPdeploytests.txt
 10010624  BeringStrait_2017_A2_02269part1ADCPraw.000

./BeringStrait_2017_A2_adcp2269_part2:
  292514 JBeringStrait_2017_A2_02269_p2.ins
  422396 JBeringStrait_2017_A2_02269_p2_bin01.rdat
  422396 JBeringStrait_2017_A2_02269_p2_bin02.rdat
  422396 JBeringStrait_2017_A2_02269_p2_bin03.rdat
  422396 JBeringStrait_2017_A2_02269_p2_bin04.rdat
  422396 JBeringStrait_2017_A2_02269_p2_bin05.rdat
  422396 JBeringStrait_2017_A2_02269_p2_bin06.rdat
  422396 JBeringStrait_2017_A2_02269_p2_bin07.rdat
  422396 JBeringStrait_2017_A2_02269_p2_bin08.rdat
  422396 JBeringStrait_2017_A2_02269_p2_bin09.rdat
  422396 JBeringStrait_2017_A2_02269_p2_bin10.rdat
   20183 ABeringStrait_2017_A2_02269part2_ADCPrecoverytests.txt
 1746264 ABeringStrait_2017_A2_02269part2ADCPraw.000

./BeringStrait_2017_A3_adcp2234:
  4561159  BeringStrait_2017_A3_02234.btm
  2353297  BeringStrait_2017_A3_02234.ins
    30039  BeringStrait_2017_A3_02234_ADCPdeploytests.txt
    18517  BeringStrait_2017_A3_02234_ADCPrecoverytests.txt
  3437867  BeringStrait_2017_A3_02234_bin01.rdat
  3437867  BeringStrait_2017_A3_02234_bin02.rdat
  3437867  BeringStrait_2017_A3_02234_bin03.rdat
  3437867  BeringStrait_2017_A3_02234_bin04.rdat
  3437867  BeringStrait_2017_A3_02234_bin05.rdat
  3437867  BeringStrait_2017_A3_02234_bin06.rdat
  3437867  BeringStrait_2017_A3_02234_bin07.rdat
  3437867  BeringStrait_2017_A3_02234_bin08.rdat
  3437867  BeringStrait_2017_A3_02234_bin09.rdat
  3437867  BeringStrait_2017_A3_02234_bin10.rdat
  3437867  BeringStrait_2017_A3_02234_bin11.rdat
  3437867  BeringStrait_2017_A3_02234_bin12.rdat
  3437867  BeringStrait_2017_A3_02234_bin13.rdat
  3437867  BeringStrait_2017_A3_02234_bin14.rdat
  3437867  BeringStrait_2017_A3_02234_bin15.rdat
  3437867  BeringStrait_2017_A3_02234_bin16.rdat
  3437867  BeringStrait_2017_A3_02234_bin17.rdat
  3437867  BeringStrait_2017_A3_02234_bin18.rdat
  3437867  BeringStrait_2017_A3_02234_bin19.rdat
  3437867  BeringStrait_2017_A3_02234_bin20.rdat
  3437867  BeringStrait_2017_A3_02234_bin21.rdat
  3437867  BeringStrait_2017_A3_02234_bin22.rdat
 13078971  BeringStrait_2017_A3_02234ADCPraw.000

./BeringStrait_2017_A4_adcp2232:
  4561710  BeringStrait_2017_A4_02232.btm
  2353620  BeringStrait_2017_A4_02232.ins
    31061  BeringStrait_2017_A4_02232_ADCPdeploytests.txt
    22444  BeringStrait_2017_A4_02232_ADCPrecoverytests.txt
  3438302  BeringStrait_2017_A4_02232_bin01.rdat
  3438302  BeringStrait_2017_A4_02232_bin02.rdat
  3438302  BeringStrait_2017_A4_02232_bin03.rdat
  3438302  BeringStrait_2017_A4_02232_bin04.rdat
  3438302  BeringStrait_2017_A4_02232_bin05.rdat
  3438302  BeringStrait_2017_A4_02232_bin06.rdat
  3438302  BeringStrait_2017_A4_02232_bin07.rdat
  3438302  BeringStrait_2017_A4_02232_bin08.rdat
  3438302  BeringStrait_2017_A4_02232_bin09.rdat
  3438302  BeringStrait_2017_A4_02232_bin10.rdat
  3438302  BeringStrait_2017_A4_02232_bin11.rdat
  3438302  BeringStrait_2017_A4_02232_bin12.rdat
  3438302  BeringStrait_2017_A4_02232_bin13.rdat
  3438302  BeringStrait_2017_A4_02232_bin14.rdat
  3438302  BeringStrait_2017_A4_02232_bin15.rdat
  3438302  BeringStrait_2017_A4_02232_bin16.rdat
  3438302  BeringStrait_2017_A4_02232_bin17.rdat
  3438302  BeringStrait_2017_A4_02232_bin18.rdat
  3438302  BeringStrait_2017_A4_02232_bin19.rdat
  3438302  BeringStrait_2017_A4_02232_bin20.rdat
  3438302  BeringStrait_2017_A4_02232_bin21.rdat
  3438302  BeringStrait_2017_A4_02232_bin22.rdat
 13080321  BeringStrait_2017_A4_02232ADCPraw.000

+++++++++ END OF FILE LISTING ++++++++++++++++++++++++++++++ 
