Woods Hole Oceanographic Institution

Cruise Planning Synopsis


SDOTS-Kirincich NE mid shelf

Ship

R/V Tioga

Cruise Party

Anthony Kirincich: Chief Scientist, Principal Investigator
Woods Hole Oceanographic Institution Clark 343c, MS#21 Woods Hole, Ma. USA 02543
+1 508 289 2629
akirincich@whoi.edu
- added Anthony Kirincich as Chief Scientist on Apr 9, 2018 9:41 AM by Ian G. Hanley
- added Anthony Kirincich as Principal Investigator on Apr 9, 2018 9:41 AM by Ian G. Hanley

Departure: May 21, 2018

WHOI dock

Arrival: May 23, 2018

WHOI dock

Operations Area

South of Martha's Vineyard, over the mid-shelf
- South of Martha's Vineyard, over the mid-shelf on Apr 9, 2018 9:41 AM by Ian G. Hanley
Lat/Lon: 41° 0.0′ N / 71° 0.0′ W
- set lat to 41° 0.0′ N, set lon to 71° 0.0′ W on Apr 9, 2018 9:41 AM by Ian G. Hanley
Depth Range: 40 / 50
- set min to 40, set max to 50 on Apr 9, 2018 9:41 AM by Ian G. Hanley
Will the vessel be operating within 200 NM of a foreign country? no

Science Objectives

To observe and diagnose the coastal mesoscale and submesoscale dynamics over the middle part of the New England Shelf (NES), identifying their role in driving exchange across the shelf. 

-

To observe and diagnose the coastal mesoscale and submesoscale dynamics over the middle part of the New England Shelf (NES), identifying their role in driving exchange across the shelf. 

on Apr 9, 2018 9:41 AM by Ian G. Hanley

Science Activities

Our approach pairs remote and in situ observations of the NES to characterize SMC variability and quantify across-shelf ex- changes with process modeling studies to explore the mecha- nisms of the SMCs. The field program will utilize a novel land- based HF radar system geared towards high spatial resolution in complex flow conditions. Deployments of autonomous surface vehicles around a centralized mooring array will provide obser- vations of critical vertical and horizontal gradients of density and velocity over a seasonal cycle. 

The in situ components include:

(1) A trio of simple hydrographic surface moorings and one subsurface mooring will be deployed in the center of the HF radar coverage area (i.e. Fig. 8) for two 6- month periods starting in spring 2018 to collect detailed timeseries of horizontal and vertical temperature and salinity gradients, local meteorological forcing, and velocity profiles over a full annual cycle of NES stratification, surface forcing, and flow conditions. The central surface mooring will sample meteorological observations using a Vaisala WXT520 weather station and water column hydrography using 11 temperature/conductivity (CT) sensors (SBE37 Microcats). A nearby subsurface mooring will support upward- and downward-looking T-RDI ADCPs to collect high resolution velocity profiles of the top 10 m and coarser resolution velocity profiles of the lower 40 m of the water column, as well as a Seagauge to observe bottom pressure. The two additional surface moorings, each with 6-8 CT sensors, will be located 6 km away from the central mooring in both the across- and along-shelf directions to allow estimates of the depth-dependent lateral hydrographic gradients and fluxes.  

(2) Two WHOI-owned, Liquid Robotics Wave Glider autonomous surface vehicles (ASVs) will be deployed for 4-months during each of the two mooring periods. Outfitted with AirMar 2-axis sonic anemometers, SeaBird CT sensors at water depths of 0.3 and 6.5-m, and speed sensors, the ASVs will follow pre-determined regular survey patterns, focused on resolving horizontal gradients of temperature and salinity within the surface layer at multiple scales around the mooring locations

 

-

Our approach pairs remote and in situ observations of the NES to characterize SMC variability and quantify across-shelf ex- changes with process modeling studies to explore the mecha- nisms of the SMCs. The field program will utilize a novel land- based HF radar system geared towards high spatial resolution in complex flow conditions. Deployments of autonomous surface vehicles around a centralized mooring array will provide obser- vations of critical vertical and horizontal gradients of density and velocity over a seasonal cycle. 

The in situ components include:

(1) A trio of simple hydrographic surface moorings and one subsurface mooring will be deployed in the center of the HF radar coverage area (i.e. Fig. 8) for two 6- month periods starting in spring 2018 to collect detailed timeseries of horizontal and vertical temperature and salinity gradients, local meteorological forcing, and velocity profiles over a full annual cycle of NES stratification, surface forcing, and flow conditions. The central surface mooring will sample meteorological observations using a Vaisala WXT520 weather station and water column hydrography using 11 temperature/conductivity (CT) sensors (SBE37 Microcats). A nearby subsurface mooring will support upward- and downward-looking T-RDI ADCPs to collect high resolution velocity profiles of the top 10 m and coarser resolution velocity profiles of the lower 40 m of the water column, as well as a Seagauge to observe bottom pressure. The two additional surface moorings, each with 6-8 CT sensors, will be located 6 km away from the central mooring in both the across- and along-shelf directions to allow estimates of the depth-dependent lateral hydrographic gradients and fluxes.  

(2) Two WHOI-owned, Liquid Robotics Wave Glider autonomous surface vehicles (ASVs) will be deployed for 4-months during each of the two mooring periods. Outfitted with AirMar 2-axis sonic anemometers, SeaBird CT sensors at water depths of 0.3 and 6.5-m, and speed sensors, the ASVs will follow pre-determined regular survey patterns, focused on resolving horizontal gradients of temperature and salinity within the surface layer at multiple scales around the mooring locations

 

on Apr 9, 2018 9:41 AM by Ian G. Hanley

Additional Info

Pre-cruise Planning Meeting: Visit WHOI
- Visit WHOI on Apr 9, 2018 9:41 AM by Ian G. Hanley
- on Apr 9, 2018 9:41 AM by Ian G. Hanley

Stations:

Supporting documentation:

Funding

Funding Agency: NSF
Grant or contract number: 1736930

Scientific Instrumentation for R/V Tioga

Shipboard Equipment

ADCP 300 kHz,
Flow Through System (14.5 gpm)
-added ADCP 300 kHz on Apr 9, 2018 9:41 AM by Ian G. Hanley
-added Flow Through System (14.5 gpm) on Apr 9, 2018 9:41 AM by Ian G. Hanley

MET Sensors

Air temperature
-added Air temperature on Apr 9, 2018 9:41 AM by Ian G. Hanley

Equipment Deployment

What type of equipment will you deploy?
Moorings and Wave gliders
What are the dimensions?
medium sized.3
- added medium sized. on Apr 9, 2018 9:41 AM by Ian G. Hanley
What is the weight in air?
500-1000 lbs
- added 500-1000 lbs on Apr 9, 2018 9:41 AM by Ian G. Hanley

Hazardous Material

Will hazardous material be utilized?no
- added no on Apr 9, 2018 9:41 AM by Ian G. Hanley
Describe deployment method and quantity:

Additional Information

Brief operations description or comments:
Other required equipment and special needs:

Checklist & Notes

Checklist

U.S. Customs Form: no
Diplomatic Clearance: no
Date Submitted:
Date Approved:
Agent Information:
Countries:
Notes:
Isotope Use Approval: no
Isotope Notes:
SCUBA Diving: no

Checklist

SSSG Tech: