Woods Hole Oceanographic Institution

Cruise Planning Synopsis


KN203-04

Ship

R/V Knorr

Cruise Party

Craig Lee: Chief Scientist, Principal Investigator
Applied Physics Laboratory, University of Washington 1013 NE 40th St Seattle, WA USA 98105-6698
+1 206 685 7656
craig@apl.washington.edu
- removed Jason Gobat as Principal Investigator on Aug 9, 2013 1:49 PM by Eric Benway
- added Craig Lee as Principal Investigator on Aug 9, 2013 1:49 PM by Eric Benway
- added Craig Lee as Chief Scientist on Aug 31, 2011 10:04 AM by Chad Smith
- added Jason Gobat as Principal Investigator on Aug 31, 2011 10:04 AM by Chad Smith

Departure: Oct 2, 2011

Nuuk, Greenland

Arrival: Oct 21, 2011

Nuuk, Greenland

Operations Area

Davis Strait region, from Southern Baffin Bay to Northern Labrador Sea (61 N - 74 N).
- Davis Strait region, from Southern Baffin Bay to Northern Labrador Sea (61 N - 74 N). on Aug 31, 2011 10:04 AM by Chad Smith
Lat/Lon:
Depth Range: min / max (m)
- set max to max (m) on Aug 31, 2011 10:04 AM by Chad Smith
Will the vessel be operating within 200 NM of a foreign country? Greenland, Canada
- Greenland, Canada on Aug 31, 2011 10:04 AM by Chad Smith
Are visas or special travel documents required? no
- set to no on Aug 31, 2011 10:04 AM by Chad Smith

Science Objectives

As part of a coordinated international effort to quantify (and eventually monitor) the variability of fluxes connecting the Arctic and Atlantic Oceans and to understand the role played by the Arctic and sub-Arctic in steering decadal scale climate variability, an integrated observing system will provide year-round measurements of volume, liquid freshwater and ice fluxes across Davis Strait. Fluxes through the Strait represent the net integrated Canadian Archipelago throughflow, modified by terrestrial inputs and oceanic processes during its southward transit through Baffin Bay. By the time they reach Davis Strait, Arctic waters already embody most of the transformations they undergo prior to exerting their influence on the deepwater formation sites in the Labrador Sea. This makes the Strait an ideal site for monitoring temporal and spatial variability in the critical upstream boundary condition for Labrador Sea convection. Measurements at Davis Strait will be used to study how fluctuations in the Arctic freshwater system modulate deep water formation to the south, thus influencing the associated meridional overturning circulation (MOC).

The system employs complementary techniques, combining mature technologies with recent developments in autonomous gliders (presently undertaking their first extended science missions) to address all aspects of flow through Davis Strait, including some measurements that have not previously been technologically feasible. System components include: 

  • A sparse array of five subsurface moorings, each instrumented with an upward looking sonar, an Acoustic Doppler Current Profiler (ADCP) and a single conductivity-temperature (CT) sensor, will provide time series of upper ocean currents, ice velocity and ice thickness. These measurements will be used to estimate the ice component of freshwater flux, provide an absolute velocity reference for geostrophic shears calculated from Seaglider hydrographic sections, and derive error estimates for our lower-frequency flux calculations.
  • Seven trawl and iceberg resistant bottom landers, instrumented with ADCPs and CT sensors, will be deployed across the Baffin and Greenland shelves to quantify variability associated with strong, narrow coastal flows.
  • Acoustically navigated Seagliders will provide year-round, repeated, high-resolution hydrographic sections across the Strait.  The resulting sections will be combined with the moored array data to produce sections of absolute geostrophic velocity and to estimate volume and freshwater fluxes. The glider navigation system includes eight acoustic sources operating at 780 Hz, 180 db. Each source will transmit 3-6 times per day, with each transmission lasting approximately 90 seconds. Sources will be anchored at widely spaced positions (roughly 50-100 km separation) north and south of the mooring line.

By quantifying, with robust error estimates, the spatial and temporal variability of the Canadian Archipelago throughflow system at a location critical for assessing its impact on deep water formation in the North Atlantic, this observing system will make a major contribution to SEARCH and ARCSS objectives.  In addition to the immediate impacts of improved estimates of freshwater inputs to the Labrador Sea, the array will provide an initial data set with which to study the relationships between Arctic freshwater system variability and large scale atmospheric fluctuations (e.g. the North Atlantic Oscillation (NAO)). The combination of emerging and existing technologies implemented in the observing system may serve as a prototype for accurate long-term monitoring of freshwater and ice fluxes in high latitude environments subject to seasonal or permanent ice cover. Finally, acoustically navigated autonomous gliders capable of extended missions in ice covered environments will provide a significant new observational tool, opening important regions of high latitude oceans to intensive measurement programs.

 

This project involves one cruise per year (September/October 2004, 2005, 2006 and 2007, 2008, 2009, 2010) to service the moored array. During these cruises, we would like to conduct limited hydrographic surveys of the Davis Strait region (please see attached chart), during which we will measure temperature, salinity, dissolved oxygen, chlorophyll concentration and selected chemical properties. To facilitate proper deployment of the moored array, we would also like to conduct a bathymetric survey. This would be performed using the R/V Knorr’s multi-beam system at the start of the 2004 field effort. In addition to these cruises, smaller filed operation will be conducted from chartered fishing boats (likely from Nuuk) to service Seagliders. The glider effort will entail at least one small boat operation per year (2005, 2006, 2007, 2008, 2009, 2010), with additional excursions undertaken as necessary to rescue and service vehicles experiencing unexpected problems.
-

As part of a coordinated international effort to quantify (and eventually monitor) the variability of fluxes connecting the Arctic and Atlantic Oceans and to understand the role played by the Arctic and sub-Arctic in steering decadal scale climate variability, an integrated observing system will provide year-round measurements of volume, liquid freshwater and ice fluxes across Davis Strait. Fluxes through the Strait represent the net integrated Canadian Archipelago throughflow, modified by terrestrial inputs and oceanic processes during its southward transit through Baffin Bay. By the time they reach Davis Strait, Arctic waters already embody most of the transformations they undergo prior to exerting their influence on the deepwater formation sites in the Labrador Sea. This makes the Strait an ideal site for monitoring temporal and spatial variability in the critical upstream boundary condition for Labrador Sea convection. Measurements at Davis Strait will be used to study how fluctuations in the Arctic freshwater system modulate deep water formation to the south, thus influencing the associated meridional overturning circulation (MOC).

The system employs complementary techniques, combining mature technologies with recent developments in autonomous gliders (presently undertaking their first extended science missions) to address all aspects of flow through Davis Strait, including some measurements that have not previously been technologically feasible. System components include: 

  • A sparse array of five subsurface moorings, each instrumented with an upward looking sonar, an Acoustic Doppler Current Profiler (ADCP) and a single conductivity-temperature (CT) sensor, will provide time series of upper ocean currents, ice velocity and ice thickness. These measurements will be used to estimate the ice component of freshwater flux, provide an absolute velocity reference for geostrophic shears calculated from Seaglider hydrographic sections, and derive error estimates for our lower-frequency flux calculations.
  • Seven trawl and iceberg resistant bottom landers, instrumented with ADCPs and CT sensors, will be deployed across the Baffin and Greenland shelves to quantify variability associated with strong, narrow coastal flows.
  • Acoustically navigated Seagliders will provide year-round, repeated, high-resolution hydrographic sections across the Strait.  The resulting sections will be combined with the moored array data to produce sections of absolute geostrophic velocity and to estimate volume and freshwater fluxes. The glider navigation system includes eight acoustic sources operating at 780 Hz, 180 db. Each source will transmit 3-6 times per day, with each transmission lasting approximately 90 seconds. Sources will be anchored at widely spaced positions (roughly 50-100 km separation) north and south of the mooring line.

By quantifying, with robust error estimates, the spatial and temporal variability of the Canadian Archipelago throughflow system at a location critical for assessing its impact on deep water formation in the North Atlantic, this observing system will make a major contribution to SEARCH and ARCSS objectives.  In addition to the immediate impacts of improved estimates of freshwater inputs to the Labrador Sea, the array will provide an initial data set with which to study the relationships between Arctic freshwater system variability and large scale atmospheric fluctuations (e.g. the North Atlantic Oscillation (NAO)). The combination of emerging and existing technologies implemented in the observing system may serve as a prototype for accurate long-term monitoring of freshwater and ice fluxes in high latitude environments subject to seasonal or permanent ice cover. Finally, acoustically navigated autonomous gliders capable of extended missions in ice covered environments will provide a significant new observational tool, opening important regions of high latitude oceans to intensive measurement programs.

 

This project involves one cruise per year (September/October 2004, 2005, 2006 and 2007, 2008, 2009, 2010) to service the moored array. During these cruises, we would like to conduct limited hydrographic surveys of the Davis Strait region (please see attached chart), during which we will measure temperature, salinity, dissolved oxygen, chlorophyll concentration and selected chemical properties. To facilitate proper deployment of the moored array, we would also like to conduct a bathymetric survey. This would be performed using the R/V Knorr’s multi-beam system at the start of the 2004 field effort. In addition to these cruises, smaller filed operation will be conducted from chartered fishing boats (likely from Nuuk) to service Seagliders. The glider effort will entail at least one small boat operation per year (2005, 2006, 2007, 2008, 2009, 2010), with additional excursions undertaken as necessary to rescue and service vehicles experiencing unexpected problems.
on Aug 31, 2011 10:04 AM by Chad Smith

Science Activities

Activities will include:
  • Hydrographic surveys of the Davis Strait region, during which we will measure temperature, salinity, dissolved oxygen, chlorophyll concentration and selected chemical properties.
  • Recovery and deployment of the Davis Strait mooring array.
  • Deployment of 4 Greenlandic moorings for the acoustic monitoring of marine mammals.
  • Deployment of Seaglider long-endurance autonomous gliders.


- Activities will include:
  • Hydrographic surveys of the Davis Strait region, during which we will measure temperature, salinity, dissolved oxygen, chlorophyll concentration and selected chemical properties.
  • Recovery and deployment of the Davis Strait mooring array.
  • Deployment of 4 Greenlandic moorings for the acoustic monitoring of marine mammals.
  • Deployment of Seaglider long-endurance autonomous gliders.


on Aug 31, 2011 10:04 AM by Chad Smith

Additional Info

Pre-cruise Planning Meeting: Teleconference
- Teleconference on Aug 31, 2011 10:04 AM by Chad Smith
- on Aug 31, 2011 10:04 AM by Chad Smith

Stations:

Supporting documentation:

Funding

Funding Agency: NSF
Grant or contract number: ARC1022472

Scientific Instrumentation for R/V Knorr

Shipboard Equipment

Bathymetry System 12 kHz,
ADCP 300 kHz,
Multibeam ,
Deionized Water System,
Science Underway Seawater System,
ADCP 75 kHz
-added ADCP 300 kHz on Aug 31, 2011 10:04 AM by Chad Smith
-added ADCP 75 kHz on Aug 31, 2011 10:04 AM by Chad Smith
-added Bathymetry System 12 kHz on Aug 31, 2011 10:04 AM by Chad Smith
-added Deionized Water System on Aug 31, 2011 10:04 AM by Chad Smith
-added Multibeam on Aug 31, 2011 10:04 AM by Chad Smith
-added Science Underway Seawater System on Aug 31, 2011 10:04 AM by Chad Smith

Shipboard Communication

Basic Internet access via HiSeasNet
-added Basic Internet access via HiSeasNet on Aug 31, 2011 10:04 AM by Chad Smith

CTD/Water Sampling

911+ Rosette 24-position, 10-liter bottle Rosette with dual T/C sensors,
SBE43 oxygen sensor,
Seapoint STM turbidity sensor,
Wet Labs C*Star transmissometer (660nm wavelength),
Wet Labs ECO-AFL fluorometer
-added 911+ Rosette 24-position, 10-liter bottle Rosette with dual T/C sensors on Aug 31, 2011 10:04 AM by Chad Smith
-added SBE43 oxygen sensor on Aug 31, 2011 10:04 AM by Chad Smith
-added Seapoint STM turbidity sensor on Aug 31, 2011 10:04 AM by Chad Smith
-added Wet Labs C*Star transmissometer (660nm wavelength) on Aug 31, 2011 10:04 AM by Chad Smith
-added Wet Labs ECO-AFL fluorometer on Aug 31, 2011 10:04 AM by Chad Smith

Critical CTD Sensors

Hydrographic Analysis Equipment

Dissolved Oxygen Titration System (Brinkmann Titrator)
-added Dissolved Oxygen Titration System (Brinkmann Titrator) on Aug 31, 2011 10:04 AM by Chad Smith

MET Sensors

Air temperature,
Barometric Pressure,
Precipitation,
Relative Humidity,
Short Wave Solar Radiation,
Wind speed and direction
-added Air temperature on Aug 31, 2011 10:04 AM by Chad Smith
-added Barometric Pressure on Aug 31, 2011 10:04 AM by Chad Smith
-added Precipitation on Aug 31, 2011 10:04 AM by Chad Smith
-added Relative Humidity on Aug 31, 2011 10:04 AM by Chad Smith
-added Short Wave Solar Radiation on Aug 31, 2011 10:04 AM by Chad Smith
-added Wind speed and direction on Aug 31, 2011 10:04 AM by Chad Smith

Sample Storage

Freezer -70°C 3.2 cu. ft. ea.,
Freezer -70°C 25 cu. ft.
-added Freezer -70°C 3.2 cu. ft. ea. on Aug 31, 2011 10:04 AM by Chad Smith
-added Freezer -70°C 25 cu. ft. on Aug 31, 2011 10:04 AM by Chad Smith
Storage Notes:

Navigation

Will you be using Long Base Line (LBL) navigation? no
- added no on Aug 31, 2011 10:04 AM by Chad Smith
How many nets? null
How many tansponders? null
Will you be using Doppler/GPS navigation?no
- added no on Aug 31, 2011 10:04 AM by Chad Smith

Navigation

GPS
-added GPS on Aug 31, 2011 10:04 AM by Chad Smith
Navigation Notes:

Winches

CTD Winch with .322" Electro-mechanical wire,
Mooring / TSE winch,
Trawl Winch with 9/16th trawl wire
-added CTD Winch with .322" Electro-mechanical wire on Aug 31, 2011 10:04 AM by Chad Smith
-added Mooring / TSE winch on Aug 31, 2011 10:04 AM by Chad Smith
-added Trawl Winch with 9/16th trawl wire on Aug 31, 2011 10:04 AM by Chad Smith
Winch Notes: trawl winch would be used only if we needed to drag for moorings.
- added trawl winch would be used only if we needed to drag for moorings. on Aug 31, 2011 10:04 AM by Chad Smith
Wire Notes:

Standard Oceanographic Cables

Slip ring required? no Number of conductors: 
Non-standard wire required? no Type: 
Traction winch required? no Describe: 

Specialized Deck Equipment

Mooring Deployment/Recovery Equipment Required: no Type: 
Cruise Specific Science Winch Required: no Type: 
Nets Required: no Type: 

Over the Side Equipment

Will you be bringing any equipment (winches, blocks, etc.) that lowers instruments over the side? no

Special Requirements

Elecrical Power: no Identify: 
Equipment Handling: no Identify: 
Inter/intraship Communications: no Identify: 
Science Stowage: no Identify: 
Water: no Identify: 

Additional Cruise Items/Activities

Explosive Devices:no
Portable Air Compressors:no
Flammable Gases:no
Small Boat Operations:yes
SCUBA Diving Operations:no

Hazardous Material

Will hazardous material be utilized?yes
- added yes on Aug 31, 2011 10:04 AM by Chad Smith
Describe deployment method and quantity:
LI primary batteries in gliders
- added LI primary batteries in gliders on Aug 31, 2011 10:04 AM by Chad Smith

Radioactive Material

Radioiosotopes:no

Additional Information

Is night time work anticipated on this cruise?yes
- added yes on Aug 31, 2011 10:04 AM by Chad Smith
Specialized tech support (Seabeam, coring, other):
Other required equipment and special needs:

Checklist & Notes

Checklist

U.S. Customs Form: no
- added no on Aug 9, 2013 1:49 PM by Eric Benway
Diplomatic Clearance: no
- added no on Aug 9, 2013 1:49 PM by Eric Benway
Date Submitted:
Date Approved:
Agent Information:
Countries:
Notes:
Isotope Use Approval: no
- added no on Aug 9, 2013 1:49 PM by Eric Benway
Isotope Notes:
SCUBA Diving: no
- added no on Aug 9, 2013 1:49 PM by Eric Benway

Checklist

SSSG Tech: