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Cruise
Log: Sunday, March 28, 2004
Contributor: Rona Thompson Before I even left
the comfort of my bunk I knew we were in for a rough day. As the Tangaroa
pitched downward I was thrown from my pillow almost crashing my head on
the bunk above. Outside tremendous waves broke on the bow and their white
caps tailed off in a fine mist. High wind speeds (around 50 knots) were
going to prevent us from doing many of the things planned for the day.
In these conditions it is impossible to do a CTD cast because of the risk
of cracking the cage against the hull, or snapping the steel cable. So
there were no seawater samples today. Atmospheric oxygen and carbon dioxide Atmospheric scientists,
however, don't need seawater for their experiments. Instead they were
kept occupied by securing air-sampling lines against strong gusts of wind.
The atmospheric group is made up mostly of chemists, some making measurements
of trace gases and others measuring aerosols. Oxygen and carbon
dioxide are being measured amongst other gases. Both these gases are biologically
produced and consumed through the processes of photosynthesis and respiration.
Photosynthesis is used by phytoplankton to manufacture carbohydrates using
dissolved carbon dioxide and sunlight, which releases oxygen as a by-product.
Its converse, respiration, produces carbon dioxide and consumes oxygen.
Therefore, the concentrations of oxygen and carbon dioxide are anti-correlated
and this can be seen on land as well as at sea.
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