Ben (left) and Darren (the shy guy who hasn't written in the blog yet) enjoying themselves in temperate climes during our port call in Santa Cruz de Tenerife |
I am usually found sailing into stormy seas in the high latitude
North Atlantic and the Southern Ocean. The last time I sailed on Discovery the wind hardly dropped below
force 10 (wind speed of about 60 mph). So this time it’s quite refreshing to pack
a bag containing shorts and sun cream, rather than wooly hats, scarves and thermals.
My role on this RAPID cruise is to oversea all the underway data collection and
processing the CTD data. What’s a CTD?
I’m glad you asked.
A CTD is the physical oceanographers main instrument. Alex is stood next to one in a previous post. It is lowered from the ship on wire to within
about 10m of the seabed and then hauled back on board. This can take a while,
as the seabed is currently 5000m below us! During this journey instruments measure
how the temperature and conductivity of the water varies with depth. Temperature
and conductivity are used to calculate the waters salinity (or saltiness). The
MicroCat instruments (picture here) on the moorings are in effect little CTDs so we attach them
to the CTD and use their bigger, and slightly more accurate, brother to check
that they are working correctly.
We not only check that the new MicroCat instruments going out on the
new moorings are OK we also attach the ones we have recovered onto the CTD and
fly them into the depths as well. As if they haven’t had enough, they have been
out in the darkness all alone for a year already!
Ben Moat
Ben Moat
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