RV Nuliajuk
Seabed Mapping Cruise Report October 18th to 31st 2013 Pangnirtung to Iqaluit |
John E. Hughes Clarke and
Weston Renoud Ocean Mapping Group Dept. Geodesy and Geomatics Engineering University of New Brunswick |
Master: Cecil Bannister
First Mate: Anton Snarby
Crew: Jeff Cheater and Levi
Ishulutaq
|
As it happened, the flights in and out of Pang on the 18th and 19th were aborted or cancelled losing two days at the beginning. To make up for this (and to avoid bad weather) a through-night transit was made. The end result required that one day be dropped from the Inside Passage investigations and the first day of the CHS work included (useful) transit data along the north side of outer Frobisher Bay.
- Pangnirtung to Iqaluit Transit - 3 days
- GN Objectives: Inside Passage Small-Craft Shipping Lanes - 2 days
- CHS Objectives: Charting and tide gauge recovery - 7 days
Primary positioning is provided by the F-185 on COM1 (GGA, HDT, VTG, ZDA) at 1 HzSingle Beam: a 38 kHz Furuno FCV-30 is the standard fisheries echosounder on the Nuliajuk. It is capable of bottom tracking in excess of 1500m. It is a split beam system, and also capable of forming multiple simultaneous beams (up to 5) for fish school shape determination. For fisheries biomass, the full waveform of a single channel can be exported in the HAC format. No bottom tracking is maintained in the HAC format, however, (or heave or orientation). And when recording to an external disk (the internal disk is too small), it slows down the ping rate and often freezes the sonar for up to a minute at a time. Thus for this leg, full waveform logging was not used.
Attitude and orientation is provided by the F-185 on COM2 in EM1000 format at 100 Hz
Secondary positioning is provided by the C-Nav 3050 on COM2 in NMEA (GGA, VTG, ZDA) at 1 Hz
Timing is provided by the F-185 via ZDA and 1PPS (Falling Edge)
CNAV 2000: The output is recorded using a serial logger. The logged data is converted to Rinex format using a proprietary CNAV converter that must be run on 32-bit Windows. Files are split by the serial logger 24 hours from logging start.Positioning and Orientation:
CNAV 3050: Is the secondary positioning for EM3002 and provides RTCM correctors to F-185. Logged by C-Setup to a proprietary format. Can be converted to Rinex with C-Nav converter.
COM1: configured to output GGA, VTG, ZDA at 1 Hz, supplied to EM3002 as secondary positioning.
COM2: configured to output RTCM 9 correctors to the F-185
Frobisher Bay SV Profiles (T and Sv, Salinity derived):
All SV-T-S(derived) profiles obtained in Frobisher Bay
Map showing locations of 4 of the 5 SV profiles collected.
Anomalous differences between the surface sound speed and the lowered probe were only noted in Lewis Bay (presumably the result of remnant river run off). As the gondola SV probe was used for beam steering and the surface brackish layer was thin, the consequences are minimal.
port side
waterline |
stern waterline |
stbd side water line |
would be better with a cuddy... |
showing transceiver/display mounting |
showing antenna and transducer transom setup. |
showing detail of transducer installation |
Arctic9 model coverage |
Arctic8 model coverage (blue) NW Atlantic model (green) Hudson Bay model (red) |
Polygons defining default
model choice for ArcticNet surveys prior to 2012 |
M2 amplitude - white line 0.1m
contours, black line 1m contours. 3.4m amplitude at head, 2.5m at mouth |
M2 phase -range : -11 to -60
degrees (1 degree is roughly 2 minutes delay for an M2 tide) |
example performance envelope
in low backscatter sediments |
example performance envelope in high backscatter sediments |
water column imagery - grids
spacing at 10m intervals |
zoom of watercolumn showing intensity trace for the specific mistracking beam |
animation of 10 succesive pings |
still of one ping |
still of another ping |
northern Anderson Channel
constriction |
central Anderson Channel
constriction |
southen Anderson Channel
constriction |