14 August 2014

Rough Seas - Update #8

These few days were interesting as the weather patterns brought some rain that we wanted, but also some rough weather.  The ship's motion went from a gentle rolling to feeling more like an amusement park ride!

Day 13
Around mid-morning, we made it back to our eddy #2 and the three drifters we had previously deployed.  At first glance, it looked like two of the drifters had gotten tangled together, despite being deployed 1km apart.  We went ahead and did a normal and trace metal CTD cast.


Preparing the trace metal CTD for deployment
The weather outlook for the next day or so is not that great.  We are expecting rain, which is good for the project, but the winds are supposed to pick up as well.  Already we can tell the seas are beginning to get a bit rough.  Since day 15 will be our last science day, and might still be rough, we decided to pick up two of the drifters now.

We went for the two that were tangled together, but they ended up not being tangled, just floating side by side.  After battling some large waves, during which almost everyone on the back deck got soaked, we managed to pull in both drifters.

Pulling the drifter over the side railing

Rinsing off the drifters with freshwater after retrieving them.
Then, we traveled back to the last drifter and did a PAR cast as well as another CTD cast.  It was too rough to deploy the towfish, so we stopped sampling for the day and waited for the rain to arrive.

One drifter had a passenger that we returned to the sea


Day 14
The rain did arrive today, but the seas were very rough.  Too rough, in fact, to deploy any sort of scientific equipment.  The danger is, in rough seas, that the boat rolls quite a bit side to side.  It has to be stationary to deploy the CTD, and that leaves us at the mercy of the swell.  If the swell is too much, the cable holding the CTD will lose tension as we roll to one side, then snap back tight as we roll to the other.  Too much of a snap and the cable breaks!

It rained pretty good in the morning, but we were unable to collect any because the salt spray was reaching the height of the bucket, which is several decks up.  The seas calmed down a bit later on - not enough to deploy any equipment, but we were able to collect rain from a second shower in the afternoon.

The rest of the day was spent planning out our final science day tomorrow and discussing packing up and loading up to go back home.

Atmospheric chemistry
If you think about the process we are studying, where rain deposits nutrients to the surface ocean, causing the phytoplankton to respond, atmospheric chemistry comes in at the very beginning.  We want to know how the nutrients got in the rain to begin with.

The majority of the atmosphere is made up of nonreactive chemical compounds, mainly oxygen and nitrogen.  We are interested in the ~1% that is reactive, specifically, how pollutants get into the rainwater.  The main indicator of man-made pollution is nitric oxide, or NO.  During the process of combustion, say when you drive your car, or when our ship is steaming through the ocean, the heat from the process breaks apart N2 molecules and produces nitric oxide.  There are a few natural sources of nitric oxide, including lightning and certain soil microbes, but they are episodic or not significant enough to be important in a marine environment.

Setting up instruments on the fly bridge before we departed - Photo courtesy of Doug Martins
Once nitric oxide is produced, it can react with ozone (O3) in the atmosphere to form nitrogen dioxide (NO2).  If there is sunlight available, the nitrogen dioxide can split back up into nitric oxide and oxygen, which goes back to ozone.  Essentially, it is a balanced reaction.  Both processes happen at once, keeping the relative levels the same in the atmosphere.  However, since one process requires energy input by sunlight, the balance levels are different overnight than they are during the day.  So at night, there is a tendency to build up nitrogen dioxide.

Now let's talk about how these molecules get into rainwater.  Nitrogen dioxide is more soluble in water than nitric oxide, which means it can more easily dissolve and be included in the water.  Nitrogen dioxide can also react with water to form nitric acid, which is super soluble.  Once nitric acid gets into the rain water, it splits apart to form nitrate, a form that phytoplankton can use.  The rest of the process is straightforward - the nitrate-filled rain falls and supplies nutrients to the surface ocean.

Performing some maintenance on the atmospheric chemistry insturments
In order to measure this process occurring in the atmosphere, we measure nitrogen dioxide and nitric oxide (NO2 and NO).  The air in general over the ocean is very clean.  Thus, anything we measure is from air masses than used to be over land and have picked up pollution from sources there.  There has been a slight problem with the ship's smoke plume interfering with the instruments.  About 50% of the time, we end up measuring air that is contaminated by the plume.  The relative ratios of the two molecules we are measuring are so different in the plume versus in clean ocean air, that it isn't an issue to identify those points and remove them from our analysis.

Our atmospheric chemist hard at work analyzing data.
As a side project, we are also measuring nitrogen dioxide and ozone in the total atmospheric column above us.  In part this is to detect plumes of pollution that are above the bottom atmospheric layer, which our other instrument would not detect.  The other part is to validate satellite measurements. We can measure the same molecules in the atmosphere via satellite, but we need observations on the surface to make sure those calculations are done correctly.  This is only the third time this instrument has been used over water (instead of land), and the first time it is out on the open ocean (instead of coastal zones).

Eventually, the measurements we make will be analyzed to help us learn more about the process of depositing nutrients from rain.  They will help increase the accuracy of satellite measurements of the atmosphere, and will also be used to help validate an atmospheric model.

Thanks for reading!  As you know, we are getting to the end of our cruise.  The next post will be the last of the daily updates, and I'll also talk about what lies ahead for us after this phase of the project finishes.


More posts in this series:
Update #6 
Update #7
Update #9