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Mooring “C”. The anchor and buoyant floats are the first to be lowered into
the ocean.
Left: McLane Moored Profiler attached to the mooring wire and ready to measure ocean currents and seawater temperature and salinity from 50 to 2000 meters depth with a resolution of approximately 1 meter. Right: The final operations of the mooring deployment. Seconds later the top flotation sphere was released and submerged. With the mooring anchor at the bottom, the sphere is at 46-meter depth, keeping the mooring wire taut and allowing the profiler to travel up and down along the wire while collecting oceanic data.
Barren snow-covered icefloe (left) and caravan for buoy deployment (right).
Drilling a 10” hole through the 240 cm thick icefloe using an ice auger can be a laborious and time consuming activity.
Being hoisted back to the ship (left). Landed on an ice floe to check its thickness during the last sea ice reconnaissance flight (left to right: Scott Payment, Kiyoshi Hatakeyama, and Adrian Godin) (right).
Seascape changes rapidly from wide areas of open water to 100% ice concentration conditions.
Cruise - 2003 Dispatches
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Dispatch 10 - August 24-27, 2003
By Andrey Proshutinsky

Beaufort Gyre Freshwater Observing System is in place

The Beaufort Gyre Freshwater Observing System has been successfully established.

On August 24th, we prepared two surface buoys and the third mooring for deployment. Our second buoy was deployed in the afternoon of August 25th. Later that evening, we found an appropriate ice floe for the third buoy installation, but could not begin the deployment due to fog and low visibility.

The following day, August 26th, was the busiest of our expedition. At 6:00 a.m. we installed our second buoy. From 8:30 to 11:30 a.m. we completed a sea ice reconnaissance flight on the helicopter to search for multiyear thick ice and prepared another buoy. From 3 to 7 p.m. we deployed our third mooring system, and from 8 to 10 PM we installed the fourth (and last) surface buoy.

The three moorings and four buoys will acquire data in the Beaufort Gyre for one year, and the moorings will be recovered or re-deployed in summer/fall of 2004.

All WHOI deployments are completed, but our expedition is not finished. Our colleagues from IOS and JAMSTEC will continue to measure water properties along several sections of the Beaufort Gyre. This information will allow us to assess the fresh water content in the Beaufort Sea in August 2003 and compare it with climatological data.

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