Flow Dynamics

Flow Dynamics of Saanich Inlet

By Roberta C. Hamme | University of Victoria

Ocean Networks Canada

University of Victoria

Natural Sciences and Engineering Research Council of Canada

 

 

Saanich Inlet is Famous for its Oxygen Depleted Bottom Water

Sill at North End Blocks Water from Flushing the Deep Saanich Inlet Basin

Bottom Map

 

Water Flushes Deep Inlet in Late Summer / Early Fall

Dissolved Oxygen

Manning, Hamme, Bourbonnais (2010) Mar Chem

 

Water Flushes Deep Inlet in Most Years

Figure courtesy of Steve Hallam at UBC

 

Picture an Aquarium (bathtub / tank) with a Partition Through the Middle. You’ve Put Water on One Side and Air on the Other. What Will Happen if You Suddenly Remove the Partition?

 

Saanich Inlet Experiences a Bottom Water “Renewal” When Dense Water Outside the Inlet Spills Over the Sill

 

Dense Salty Water Comes from the 0cean

Masson and Cummins (2004) J Mar Res

 

Tides Mix up the Water as it Flows Over Sills on the Way to Saanich Inlet

 

Tidal Currents Vary Over Time

One month record of tidal currents in Active Pass

WWW Tide/Current Predictor: http://tbone.biol.sc.edu/tide

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Ocean Networks Canada Observations in Saanich Inlet

Intensive experiment 2016-2017 to study chemical changes after renewals (Saanich Inlet Redox Experiment: SaanDox).

Chemical Changes

Sill Mooring Records High Density Water Spilling into Saanich Inlet When Current Speeds are Lowest

Current Speeds

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Sill Mooring Records High Oxygen Water Spilling into Saanich Inlet When Current Speeds are Lowest

Current Speeds

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Ocean Networks Canada Observations in Saanich Inlet

Buoy Profiling System

Buoy Profiling System
Chemical Changes

Profiling Mooring Records High Density Water Filling Deep Saanich Inlet When Current Speeds are Lowest

Profile Mooring

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Profiling Mooring Records Oxygenated Water Filling Deep Saanich Inlet When Current Speeds are Lowest

Profile Mooring

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Oxygen In Renewed Deep Water is Consumed Quickly

Deep Water Record

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Summary

  • Dense oxygenated water enters deep Saanich Inlet in late summer / early fall
  • Requires very low tidal currents to preserve high density waters outside of inlet
  • Renewal happens via several events
  • Oxygen is consumed within 2-3 weeks

Future questions

  • Why do some years experience no renewal?
  • Is starting density of water or tidal currents more important?