The brand-new CTD from ICBM – Germany’s largest CTD – is being used for the first time during this research cruise with the Sonne. In addition to valuable data, the CTD brings 24 large bottles of seawater from different depths on deck. Not ‘just’ water, but up to 480 liters with every cast. Continue reading
There are regular safety drills on board, so that everyone knows what to do in case of an emergency. The safety drill was announced ahead of time; once the alarm bells rang, we rapidly collected our life vests and met at the assembly point on deck.
We have been on board Sonne already for 15 days; it feels like we have been here since forever. We know where everything is and we are so used to our working space. But it was not always like this…
The microorganisms in the ocean enjoy the sun and warmth of the equator, just as we scientists do when we are not working. Here in the equatorial upwelling zone, microorganisms grow well because of the extra nutrients that are brought to the ocean’s surface by upwelling (upwards movement) of water from the deep ocean. As a consequence, in certain depths of the water column, oxygen is consumed faster than it is supplied via circulation
This morning at 6 a.m. we ended our 24-hour sampling at this station, and continued our journey north. Neptune, of course, noticed that we had passed the equator without permission; he visited us in person.
We have finally reached the equator – the boundary between the northern and southern hemispheres at 0 N and 0 South. But we aren’t just anywhere on the equator: we are exactly at the point at which one step in the right direction can turn today into yesterday, and visa versa. Our station is exactly on the international date line between 180 W and 180 E.
We are rapidly approaching the equator. Tomorrow, we will begin our first twenty-four hour continuous station, in order to sample the water column for an entire day/night cycle. We will have a very long work-day! Someone else is also waiting for us: Neptune, the ruler of the ocean…
I want to give blog visitors an explanation for the long pause between the last blog entries. We are going through such a remote region of the Pacific that we only have limited (and sporadic) internet connectivity.
We eagerly awaited these samples, the first from the very bottom of the ocean to reach the deck. These samples were especially exciting because the bottom of the ocean at this station is at 4200 m water depth; moreover, it was our very first use of this sampler in the deep sea, which the ICBM just recently acquired.
On this research expedition we are using two classical methods to characterize the surface water of the ocean. These methods were developed in the 19th century, so they do not require advanced technology or power supplies.