Andreas Muenchow

Andreas Muenchow

Feb 06, 2015

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Ocean sensors arrived

Two ocean sensors arrived from Germany where I used them last in an experiment off the coast of Greenland last year. I bought them in 2002 and they have been in Arctic waters most of the time where they measure ocean temperature and conductivity very accurately a few times every second. Conductivity of seawater is what oceanographers measure when they want to talk about salinity and Arctic oceanographers must know salinity if they want to talk about ocean density. Water from cold melting ice and glaciers is less dense (because it is fresh) than the warm and salty water from the Atlantic Ocean that does the melting. You need heat to melt ice, but the heat that melts Greenland from below by the ocean comes from the Atlantic. The heat is at depth 200-400 meters deep, because of salt in the water that makes it dense and sink.

Oceanography and physics are fun, but here are the photos of what I work with over the weekend at home ... maybe in my garden, too, to practice for the Arctic deployment, you may even watch me do it on the web-cam in my garden pointing towards the heated bird-bath. Geeks at play, science is fun:

The housing of these two instruments are rated for 7,000-m depth, I will have to install the lithium batteries ($4.80 for a single AA battery); each instrument needs 12 of those. Since 2003 we deployed a number of these in the Arctic where they collected data for over 3 years every 15 minutes. One of my students, Berit Rabe now works in Scotland and her dissertation and peer-reviewed publication was based on data from a single 2003-06 deployment of about 20 such instruments.

The instruments connect via a serial cable to the computers. In the past I had problems with instruments bought 12 years ago, because computers develop much faster than oceanographic instrumentation. So, new is not always better, so I bought an old Dell Windows XP machine on e-Bay for $200 (actually I bought 2) to ensure that my sensors match software, CPU, and operating systems of the time that the instruments were bought. In order to "talk" to the sensors, I will need to put the lithium batteries into them. I am very much looking forward to do this over the weekend.

To be continued ...

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About This Project

Greenland is melting and as more of its ice and water move into the ocean, sea level will rise. We will measure ocean temperature and salinity below 200 to 600 meter thick ice of Petermann Glacier in North Greenland for several years. Holes will be drilled through the ice to reach the ocean below where we place about 10 instruments. The holes will freeze over quickly, the instruments will never return, but a cable connects the mysteries of the dark ocean to the surface and via satellite to anyone with an internet connection. More details are posted at my web-log http://IcySeas.org where I share my excitement about science.

More Lab Notes From This Project

Blast off!

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