README FILE FOR BERING STRAIT MOORING DATA                      8th June 2020
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Bering Strait Moorings 2018-2019

This is an archive of data from moorings deployed in Bering Strait from
summer 2018 to summer 2019.

Mooring deployments were funded by the NSF-Arctic Observing Network
award PLR-1758565 (PIs: Woodgate and Peralta-Ferriz).

The mooring work required 2 dedicated cruises:
- 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.
- in 2019 (5th - 15th September), a ~ 11 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 2018 to 2019, 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.

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

A2-18  2018  65 46.87  168 34.08  ISCAT          8964   5min   16m    55m
recovered by dragging             ISCAT-Logger      4  30min   ...    55m
                                  300kHz-ADCP   13758  30min   45m    55m
                                  SBE16          0008   ND     50m    55m

A3-18  2018  66 19.62  168 57.08  ISCAT         14550     NR   15m    57m
                                  ISCAT-Logger     23  30min   ...    57m
                                  300kHz-ADCP    2332  30min   43m    57m
                                  SBE16          1224  60min   43m    57m
                                  AURAL M2*      96LF    -     49m    57m

A4-18  2018  65 44.76  168 15.77  ISCAT         20128   5min   16m    48m
recovered by dragging             ISCAT-Logger     26  30min   ...    48m
                                  300kHz-ADCP   10926  30min   37m    48m
                                  SBE16          0005  60min   41m    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: August 2018 to September 2019

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.
       This is found to be of inconsistent quality as a calibration check.
       Immediately after recovery, SBE instruments were placed in a stirred
       tank of sea water, to check immediate post deployment calibrations.
       For full details, see cruise report. 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", "asc" or "XML" 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.  Two moorings (A2 and A4) required
    dragging due to biofouling.  Mooring A3 released without dragging 
      - biofouling is a typical issue in the strait, and was still
    sigificant on these moorings, although lighter than last year
    possibly as the mooorings were deployed later in the season.
    All moorings were fouled to a similar level. 
    As in past year, fouling was mostly by barnacles, up
    over 2cm long, with some bryozoan-like growth on several parts of
    the moorings.  
    On A3 and A4 salinity cells (SBEs and ISCATs) were clear, but
    on A2, the bottom of the SBE cell was blocked and both ends of the
    ISCAT cell were blocked with mussels.
    As discussed below, salinity drifts are still significant.
    Release hooks were mostly clear on A3, but A2 release hook was
    significantly biofouled by bryzoans, and A4 release hook was
    significantly biofouled by barnacles.  Although all three moorings
    should have been painted with fresh biofouling paint before deployment,
    pre deployment photographs suggest perhaps the paint was thinner
    and more worn than usual, possibly explaining release hook biofouling.
    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)
      A218  - SBE37  8964 - recovered
			- cell blocked with mussels
			- clock 0min fast on recovery
			- post cal shows salinity change of 0.11psu
			- record linearly interpolated between pre & post cals      
			- final data ~0.1psu fresher than reference in test tank  
			- pre recovery CTD cast inconclusive due to strong gradients
			- winter freezing temperatures suggest salinities ok then
			- comparison to underlying SBE impossible as no SBE data
			- Conclude: end of record maybe up to 0.1psu too fresh
             - Logger 04 - - Data good, but only SBE37 data given here

       A318  - SBE37 14550 - lost 31st May 2019, at block below iscat
			(tether recovered with mooring and appears to have influenced
			ADCP compass detrimentally) 
             - Logger 23 - Data good
                - logger clock 26min 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                             
			- winter freezing temperatures suggest salinities ok then
                - underlying SBE16 data suggest SBE37 ok
               - Conclude: no obvious salinity issues

       A418  - SBE37 20128 - recovered
			- cell clear, though much silt in iscat
                - clock 0 min fast by end of deployment, but 3 records      
                     missing, i.e., 15min time ambiguity.                        
                  - adjusted linearly here to match time out of water         
			- post cal shows salinity change of 0.19psu
			- record linearly interpolated between pre & post cals      
			- final data ~0.1psu fresher than reference in test tank  
			- pre recovery CTD cast inconclusive due to strong gradients
			- winter freezing temperatures suggest salinities ok then
                - underlying SBE16 data suggest SBE37 ends ~0.1psu too fresh
			- Conclude: end of record maybe up to 0.1psu too fresh
            - Logger 26 -Data good, but only SBE37 data given here


    === SBE16
       A218_0008
         - failed before deployment, no in-the-water data

       A318_1224
         - despite moderate biofouling, cell clear on recovery
         - 0.08 psu change between pre and post cals
         - Clock 8min slow on recovery, but went back 1min in time   
                 during comms pre downloading                                
         - record linearly interpolated between pre & post cals  
         - stopped in test tank even though said logging afterwards  
         - in tank only wrote 1 good and 2 dud records               
         - test tank data inconclusive, but possibly reading fresh
         - final data ~0.3psu fresher than recovery CTD
         - winter freezing temperatures suggest ~0.1psu too fresh
         - overlying SBE37 data suggest SBE16 ends ~0.2psu too fresh
         - Conclude: end of record maybe up to 0.2psu too fresh

       A418_0005
         - despite moderate biofouling, cell clear on recovery
         - clock 6 min slow on recovery
         - 0.04 psu change between pre and post cals
         - record linearly interpolated between pre & post cals  
         - final data ~0.02psu fresher than reference in test tank
         - final data ~0.1psu fresher than recovery CTD
         - winter freezing temperatures suggest no salinity issue
         - overlying SBE37 data suggest SBE16 salinities ok
         - Conclude: end of record salinities ok

   === 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.

	A218_adcp13758
         - returned a full year of data and was still recording on
         recovery.  
	    - bin 1 has some high velocity errors
	    - bins 11/12, have some high velocity errors
	    - data generally good until Bin15 (~13m) 

	A318_adcp02332
         - returned a full year of data and was still recording on
         recovery.  
         - after iscat lost on 31st May, ADCP velocity headings change
         abruptly, possibly due to magnetic iscat tether falling near
         ADCP compass. Thus all directions after this time are deemed
         erroneous and set here to 9999.9
	    - bin 1 has some high velocity errors
	    - bin 10 has some high velocity errors
	    - data generally good until Bin14 (~13m) 

	A418_adcp10926
         - returned a full year of data and was still recording on
         recovery.  
	    - bin 1 has some high velocity errors
	    - bin 8 has some high velocity errors
	    - data generally good until Bin11 (~13m) 


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.  These data are 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-1758565 (PI: Woodgate and Peralta-Ferriz)

15) Sample repository locations:
        National Ocean Data Center (http://www.nodc.noaa.gov)
          (now called National Centers for Environmental Information)
        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:  97 including 4 subdirectories

Size (b)   Name
---------  ----
= Metadata file (1 file)
    29204  Bering_Strait_Moorings_2018-2019_NSFAON_ReadMe.txt

= Cruise report (1 files) and 1 technical note (1 file)
 18579073  BeringStrait2019CruiseReport_Norseman2_2ndJune2020withEL.pdf
  1853097  WoodgateandHolroyd2011_BTrangeCorrection.pdf

= ISCAT data  (5 files)
  - 1 ICLog*.pre of pre calibrated logger data
  - 2 ICsbe37*.ppp pre-post calibrated SBE37 data
  - 2 ICsbe37*.XML raw SBE37 data
  9719248  BeringStrait_2018_A2_ICsbe37_08964.ppp
  3653371  BeringStrait_2018_A2_ICsbe37_08964raw.XML
  1128303  BeringStrait_2018_A3_ICLog23_14550.pre
  9721240  BeringStrait_2018_A4_ICsbe37_20128.ppp
  3654466  BeringStrait_2018_A4_ICsbe37_20128raw.XML

= SBE16 (4 files)
  - 2 .hex files of raw data
  - 2 .ppp files of pre-post calibrated data
  (see also con file directory)
   802136  BeringStrait_2018_A3_sbe16_1224.ppp
   195357  BeringStrait_2018_A3_sbe16_1224raw.hex
   805962  BeringStrait_2018_A4_sbe16_0005.ppp
   192328  BeringStrait_2018_A4_sbe16_0005raw.hex

.. and the 5 subdirectories,

One subdirectory of SBE .con calibration files
./BeringStrait_2018_SBEconfiles:
   - 4 calibration files for SBEs
 4760 0005posFeb20.con
 4760 0005preNov17.con
 4764 1224posFeb20.con
 4789 1224preAug16.con

Three subdirectories of ADCP data, naming conventions
as described above, (each 27 files)

./BeringStrait_2018_A2_adcp13758:
  4507660  BeringStrait_2018_A2_13758.btm
  2325790  BeringStrait_2018_A2_13758.ins
    29952  BeringStrait_2018_A2_13758_ADCPdeploytests.txt
    15202  BeringStrait_2018_A2_13758_ADCPrecoverytests.txt
  3397592  BeringStrait_2018_A2_13758_bin01.rdat
  3397592  BeringStrait_2018_A2_13758_bin02.rdat
  3397592  BeringStrait_2018_A2_13758_bin03.rdat
  3397592  BeringStrait_2018_A2_13758_bin04.rdat
  3397592  BeringStrait_2018_A2_13758_bin05.rdat
  3397592  BeringStrait_2018_A2_13758_bin06.rdat
  3397592  BeringStrait_2018_A2_13758_bin07.rdat
  3397592  BeringStrait_2018_A2_13758_bin08.rdat
  3397592  BeringStrait_2018_A2_13758_bin09.rdat
  3397592  BeringStrait_2018_A2_13758_bin10.rdat
  3397592  BeringStrait_2018_A2_13758_bin11.rdat
  3397592  BeringStrait_2018_A2_13758_bin12.rdat
  3397592  BeringStrait_2018_A2_13758_bin13.rdat
  3397592  BeringStrait_2018_A2_13758_bin14.rdat
  3397592  BeringStrait_2018_A2_13758_bin15.rdat
  3397592  BeringStrait_2018_A2_13758_bin16.rdat
  3397592  BeringStrait_2018_A2_13758_bin17.rdat
  3397592  BeringStrait_2018_A2_13758_bin18.rdat
  3397592  BeringStrait_2018_A2_13758_bin19.rdat
  3397592  BeringStrait_2018_A2_13758_bin20.rdat
  3397592  BeringStrait_2018_A2_13758_bin21.rdat
  3397592  BeringStrait_2018_A2_13758_bin22.rdat
 13031616  BeringStrait_2018_A2_13758ADCPraw.000

./BeringStrait_2018_A3_adcp02332:
  4507279  BeringStrait_2018_A3_02332.btm
  4046734  BeringStrait_2018_A3_02332.ins
    46946  BeringStrait_2018_A3_02332_ADCPdeploytests.txt
    36647  BeringStrait_2018_A3_02332_ADCPrecoverytests.txt
  3397385  BeringStrait_2018_A3_02332_bin01.rdat
  3397385  BeringStrait_2018_A3_02332_bin02.rdat
  3397385  BeringStrait_2018_A3_02332_bin03.rdat
  3397385  BeringStrait_2018_A3_02332_bin04.rdat
  3397385  BeringStrait_2018_A3_02332_bin05.rdat
  3397385  BeringStrait_2018_A3_02332_bin06.rdat
  3397385  BeringStrait_2018_A3_02332_bin07.rdat
  3397385  BeringStrait_2018_A3_02332_bin08.rdat
  3397385  BeringStrait_2018_A3_02332_bin09.rdat
  3397385  BeringStrait_2018_A3_02332_bin10.rdat
  3397385  BeringStrait_2018_A3_02332_bin11.rdat
  3397385  BeringStrait_2018_A3_02332_bin12.rdat
  3397385  BeringStrait_2018_A3_02332_bin13.rdat
  3397385  BeringStrait_2018_A3_02332_bin14.rdat
  3397385  BeringStrait_2018_A3_02332_bin15.rdat
  3397385  BeringStrait_2018_A3_02332_bin16.rdat
  3397385  BeringStrait_2018_A3_02332_bin17.rdat
  3397385  BeringStrait_2018_A3_02332_bin18.rdat
  3397385  BeringStrait_2018_A3_02332_bin19.rdat
  3397385  BeringStrait_2018_A3_02332_bin20.rdat
  3397385  BeringStrait_2018_A3_02332_bin21.rdat
  3397385  BeringStrait_2018_A3_02332_bin22.rdat
 13029573  BeringStrait_2018_A3_02332ADCPraw.000

./BeringStrait_2018_A4_adcp10926:
  4508365  BeringStrait_2018_A4_10926.btm
  2326153  BeringStrait_2018_A4_10926.ins
    25444  BeringStrait_2018_A4_10926_ADCPdeploytests.txt
    17403  BeringStrait_2018_A4_10926_ADCPrecoerytests.txt
  3398123  BeringStrait_2018_A4_10926_bin01.rdat
  3398123  BeringStrait_2018_A4_10926_bin02.rdat
  3398123  BeringStrait_2018_A4_10926_bin03.rdat
  3398123  BeringStrait_2018_A4_10926_bin04.rdat
  3398123  BeringStrait_2018_A4_10926_bin05.rdat
  3398123  BeringStrait_2018_A4_10926_bin06.rdat
  3398123  BeringStrait_2018_A4_10926_bin07.rdat
  3398123  BeringStrait_2018_A4_10926_bin08.rdat
  3398123  BeringStrait_2018_A4_10926_bin09.rdat
  3398123  BeringStrait_2018_A4_10926_bin10.rdat
  3398123  BeringStrait_2018_A4_10926_bin11.rdat
  3398123  BeringStrait_2018_A4_10926_bin12.rdat
  3398123  BeringStrait_2018_A4_10926_bin13.rdat
  3398123  BeringStrait_2018_A4_10926_bin14.rdat
  3398123  BeringStrait_2018_A4_10926_bin15.rdat
  3398123  BeringStrait_2018_A4_10926_bin16.rdat
  3398123  BeringStrait_2018_A4_10926_bin17.rdat
  3398123  BeringStrait_2018_A4_10926_bin18.rdat
  3398123  BeringStrait_2018_A4_10926_bin19.rdat
  3398123  BeringStrait_2018_A4_10926_bin20.rdat
  3398123  BeringStrait_2018_A4_10926_bin21.rdat
  3398123  BeringStrait_2018_A4_10926_bin22.rdat
 13033659  BeringStrait_2018_A4_10926ADCPraw.000

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