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BIO’s CATS Field, modelling, chemistry and instrumentation work November 2006 Simon Prinsenberg, Jim Hamilton and Peter Rhines
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1 - Field work +Data 2 - Modelling 3 - Instrumentation Salinity δ 18 O (‰) 0 -30 035 seawater Meteoric water (rain, snow, river runoff, glacial meltwater) Sea-ice meltwater 4 - Chemistry
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Field/Data – Jim Hamilton Muray Scotney Roger Petipas Peter Rhines Modelling – Charles Hannah Dave Greenberg Youyu Lu Fred Dupont Instrumentation – George Fowler Brain Beamlands Greg Siddall Peter Rhines Chemistry – Kumico Atzuo-Scott
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Project’s aim is to monitor and simulate The fluxes through the CAA as part of the Arctic-Atlantic ocean conveyor belt circulation From G. Holloway CAA- Canadian Arctic Archipelago Barrow Strait - Lancaster Sound
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Three major straits through the CAA Survey area (red Box) Grid show the diagnostic finite element model domain (20058 elements )
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Observation Problems: Magnetic north pole Mobile ice cover Modelling Problems: Complex topography Lack of bathymetric and oceanographic data North Pole
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Lancaster Sound year-long mooring 2004-05 southnorth
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Software and hardware to measure current direction in Low-horizontal Magnetic field with mid-water floats Magnetic direction 88 O in CAA Vertical direction 90 O by Jim Hamilton normally ADCP with role/tilt compass
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-Watson Compass provides role-tilt and magnetic Pole direction -This provides current magnetic direction data -Corrected by Resolute magnetic data for wandering magnetic North Pole. -To finally provide current direction to true north -Special data processing Measuring current direction in Low-horizontal Magnetic field 2004 True North Magnetic North
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Lancaster sound survey - Deployment of ADCP and battery pack
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ULS mounted between two A2-SUBs Ice draft measurements (2sec. data)
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Lancaster Sound August 2004 - First 6-years of field data
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Ocean statistics from time series data Surface current Barrow Strait 3 month average from bi-hourly data
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Ocean and pack ice statistics from time series data Plots? Tables? Website? Currents at 80m Barrow Strait 3 month average from bi-hourly data
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Ocean and pack ice statistics from time series data Plots? Tables? Website? Ice velocity Barrow Strait 3 month average from bi-hourly data
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Ice draft plot monthly max., mean and Std. Dev. from 2sec time series data
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Weekly and monthly fluxes for Aug. 98 to July 05 (7 years of data) (seasonal weighted 2/3 southern site data and 1/3 northern site data) Summer
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Yearly and seasonal mean estimated fluxes passing through Lancaster Sound in units of Sv (= 10 6 m 3 /s). YearFallWinterSpringSummer 1998/99Volume0.4-0.00.40.50.7 Freshw.0.030.00.03 0.04 1999/00Volume0.90.30.91.11.3 Freshw.0.060.020.06 0.08 2000/01Volume1.0 0.8 1.2 Freshw.0.06 0.05 0.07 2001/02Volume0.60.10.40.9 Freshw.0.040.010.020.060.07 2002/03Volume0.90.60.51.21.1 Freshw.0.060.050.030.080.9 2003/04Volume0.60.30.50.61.2 Freshw.0.050.040.030.040.09 2004/05Volume0.50.10.60.70.9 Freshw.0.040.010.040.050.-6
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Monthly mean volume flux through eastern Barrow Strait derived from 6-year of mooring data (Aug. 1998 – Aug. 2004).
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Transports from mooring data and their variability NAO
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2 - Modelling
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Modelling Problems: Complex topography Lack of bathymetric and oceanographic data D. Greenberg, C. Hannah F. Dupont
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Summer surface currents (arrows) for -10cm Baffin Bay set-up color code is for depth contours
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Ice concentration during the 1 year run coupled to AIM Sep 89 June 1990 July 1990 August 1990 Sep 1990
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Surface ocean current during the 1 year run coupled to AIM Sep 89 Dec 89 Mars 90 June 1990Sep 1990
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WebTide C. Hannah
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WebTide Tidal Currents Future: wind effects
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Increased # grids 3-4km at transect Good for shore erosion, ship mooring sites and harbours
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Ocean module based on NEMO (OPA) and CICE ice module Domain covers Arctic Ocean and sub-polar NA; a subset of global 1/4º MERCATOR grids Minimum grid size 6 km in CAA and maximum15 km in Arctic Ocean and up to 40 vertical levels 480x468x40 grids Youyu LU Large scale Ice-ocean Model (DFO and IPY) Ice thickness
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3 - Instrumentation
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Sensor Float Midwater Float Acoustic Release EM Cable ICYCLER #2 ICYCLER: Surface layer CTD profiler moored beneath mobile pack ice Problem: Can not moor instruments in surface layer because of mobile ice cover, and yet there is where the large variability in the oceanographic parameters occur. 25m 50m By George Fowler
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ICYCLER #1 provided yearlong CTD-Chl data set 2003-2004 from Lancaster Sound
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Fluorescence Temperature Yearlong Aug 2003- Aug 2004
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Freshwater flux is underestimated by 30m MicroCat data seasondays ICYCLER MCatDeltaS.V cm/s%∆ fw Sum034029.8331.13-1.4035-28 Fall039130.4231.23-0.8115-19 Win049131.2531.41-0.1607-04 Spr049131.4331.74-0.3108-10 Sum044231.0831.76-0.6815-18
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SeaMotor
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Seacat pressure data Lost-found ICYCLER Aug. 04 – Aug. 06
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- Profiler line spooled out - Buoyancy tank imploded but sealed - Baterry dead and Corrosion
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Salinity δ 18 O (‰) 0 -30 035 seawater Meteoric water (rain, snow, river runoff, glacial meltwater) Sea-ice meltwater 4 - Chemistry
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How to use oxygen isotope composition (δ 18 O) to quantify the fresh water compositions Water is a mixture of seawater and meteoric water Water is a mixture of seawater, meteoric water and sea-ice meltwater Water is a mixture of seawater and sea-ice meltwater Salinity δ 18 O (‰) 0 -30 035 seawater Meteoric water (rain, snow, river runoff, glacial meltwater) Sea-ice meltwater light oxygen (O-16) enriched heavy oxygen (O-18) enriched
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How to use Total Alkalinity to quantify the fresh water compositions Water is a mixture of seawater and sea ice meltwater Water is a mixture of seawater, river runoff and sea-ice meltwater Water is a mixture of seawater and river runoff salinity Total Alkalinity Seawater Sea Ice, rain, snow meltwater River runoff 035 0 2300
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Barrow Strait 1980 1977 2003 Seasonality ? Time series data Salinity δ 18 O (‰) 0 -30 035 seawater Meteoric water (rain, snow, river runoff, glacial meltwater) Sea-ice meltwater
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Yearlong water sampler to determine δ 18 O MicroLab by Environtech
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Where are we heading with the CAA research -Moorings in until August 2007????? -Modelling effort reduced at moment effort on data processing - Waiting for B-Base funding cycle to clear PERD (by early 2007) -Waiting for B-Base funding cycle to clear IPY (by early 2007)
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