Wednesday, September 23, 2015

Nearing the End

Hello Everyone,

We will be back in Nuuk on the morning of September 25th.  That means, just a little over 30 hours and we'll be back on land.  We are pushing our way Northeast along the Northern Labrador Sea East Line and we are currently completing our last operation at NLSE_05, just 100 nm away from the Greenland Coast.

Almost done!  Just one more night.
 For our oceanographers, this is the section plot for the NLSW line:

Section plot for the NLSW line.

Tuesday, September 22, 2015

1001 Page Views!!

Hi Everyone,

We've had 1001 page views on this blog (and they are not all mine).  Thanks for tuning in!  We are back at the CTD stuff today after a very exciting night of harrowing rescues at sea. I'm going to bed now, but I'll try to make another post before the end of the day.

Andrew

Monday, September 21, 2015

All Safe

Hello Everyone,

We've been called off the rescue. All crew of the Atlantic Charger are now safe and on board a vessel in the area (not sure which one yet).  I will provide an update when more information is filtered down directly from the Captain or Chief Scientist at a later date.

Andrew

Rescue at Sea.

Hello Everyone,

The Atlantis was notified at ~ 1630 UTC that there was a fishing crew in distress to our southwest (The Atlantic Charger) and we were diverting our course to rendezvous with their location as soon as possible.  We had confirmation from the Atlantis Captain that all 9 men are safe and unharmed. We've been informed that there are other ships in the area but it is quite possible that the Atlantis could be the first ship on the scene to extract the crew from their life raft. Our estimates put us less than 1.5 hours away.  We are readying warm clothing, qualified personelle and a contingency plan has been created by the crew for extraction.

We'll keep you posted on developments as they become available.

A file photo of the Atlantic Charger, registered in 2012 in St. John's, is reportedly taking on water in Frobisher Bay.
Atlantic Charger (File photo courtesy of CBC).

Halfway to Nowhere!

Time: 07:38 UTC
Latitude: 63° 6.035' N
Longitude: 60° 15.437' W
Conditions: Yeeee Haaaa (2-3 m waves, 30 kts)

Hi Everyone,

We just finished up a night on the Northern Labrador Sea Line.  I put on my Go Pro helmet cam tonight so I'm hoping I got some good imagery of the CTD deployment/recovery and water sampling. I'll post it when I can but large videos could take a while.

Anyway, we are nearing station NLSW_11 and we should be there in ~50 minutes.  Hopefully by then I'll be snug as a bug in my cabin.  Well, off to a breakfast for champions.

Cruise track as of ~0738 UTC on September 21, 2015

Sunday, September 20, 2015

Northern Lights

Hello Everyone,

We had an amazing light show tonight.  It is notoriously difficult to get good photos of the Northern Lights because they are relatively faint and because the high exposure required often makes for blurry picture.  I tried a 30 second exposure in "nigh mode" tonight with the AZMP GoPro Silver 4 and it did a pretty good job of it. I did not get good shots at the height of the light show, but the ones I did get turned out considering the ship is a moving platform.  I've posted some below:

All images captured on the night of September 20th, ~60-70 nautical miles east of Baffin Island.









Saturday, September 19, 2015

Time: 2337 UTC
Latitude: 65° 39.393' N
Longitude: 58° 27.426' W
Conditions: Rock'n and Roll'n (2-3 m seas and 21 kt winds)

At the moment we are on a southeast heading steaming at a steady 11 kts.  We hope to arrive on the western most portion of  the Northern Labrador Sea Line by ~11 am on the 20th of September.  Four days of intense 24 hour CTD operations will see us arrive in Nuuk on the 25th of September.  I'm looking forward to a few more days of deck operations. I've learned a great deal from the crew and scientists aboard the ship. I'd like to take an early opportunity to extend my thanks to everyone for making me feel so at home on the Atlantis.
That little red triangle is us and we are heading towards the western end of the Northern Labrador Sea Line.  We are on the home stretch!

Gumby and Pokey enjoy a ride on the Gas Chromatograh (happy Dave?).
 

Eric Boget - Principal Engineer in the Ocean Engineering Department at the Applied Physics Laboratory, University of Washington (APL-UW)

Eric Boget.  Photo from the APL-UW Website
My name is Eric Boget and I am a Principal Engineer in the Ocean Engineering Department at the Applied Physics Laboratory University of Washington (APL-UW). I graduated from the U.S. Merchant Marine Academy and spent the early years of my career working as crew on merchant vessels, tugs and tall ships. I came to APL-UW in 1990 and was originally hired to manage and operate their small fleet of coastal research vessels.  In the mid-90’s, I began going to sea with various scientists from APL-UW in support of their oceanographic research programs.  Over the years, I’ve been involved with many different oceanographic systems and platforms, included: undulating towed bodies, moored systems, large acoustic arrays, Autonomous Underwater Vehicles (AUV’s), etc. These days, I spend about 3-5 months a year at sea and the remainder of my time in the office primarily working on design and analysis of oceanographic mooring systems and continuing to manage the APL vessels and scuba diving program.  I have been involved with the Davis Strait program since it began in 2004 and my primary focus has been servicing the oceanographic moorings. I look forward to this trip each year and really enjoy working in Greenland. 

Eric and the team deploy a mooring.  See the YouTube Time Lapse.
The primary focus of the Davis Strait program is to provide year-round measurements of the freshwater flux (liquid and ice) flowing from the Arctic through the Davis Strait into the Atlantic Ocean. As part of an integrated observing system, we have maintained 15 moorings in the Davis Strait; 6 central moorings across the strait, 6 smaller shelf moorings on the Greenland and Baffin Island shelves plus 3 off-axis acoustic source moorings.  In the beginning, the moorings were turned every year but 5 years ago we switched to a two-year cycle.  The moorings are instrumented with upward looking sonar to measure ice draft, conductivity-temperature (CT) sensors, acoustic doppler current profilers (ADCP) plus conventional current meters and hydrophones listening for marine mammals. Additionally, the central and off-axis moorings have 780HZ sounds sources (6 total) that provide a navigational array for under-ice glider operations.  The gliders are equipped with CT and oxygen sensors.  To compliment the mooring array and gliders, the program re-occupies over 100 CTD stations collecting data and water samples at each of these sites.  We’ve been fortunate to have partnered with Bedford Institute ofOceanography (BIO).  BIO manages the hydrological sampling and analysis effort and additionally provides instrumentation and mooring expertise. 



There have been a few innovative technologies developed during the program.  The gliders use the acoustic array to navigate under the ice in the winter.  They fly back and forth across the Davis Strait and are able to surface on the Greenland side where the warmer West Greenland current keeps this area ice free all or most of the year (See figure at bottom of post.  There are other areas in Davis Strait that remain ice free during the harsh winter months and are called polynyas).   The top of the moored array is at a depth of 104 m to avoid the majority of the large icebergs in the strait.  In order for us to sample closer to the surface (20 m), we developed the “ice cat” which consisted of one or more CT sensor attached to a polyethylene (PE) jacketed wire rope with some flotation at the top.  The ice cat wires are attached to the top of the main moorings using a 600 lb weak link.  The CT sensors communicated inductively through the mooring wire to a logger mounted on the main mooring.  If the ice cat gets caught in the ice, it will break the weak link instead of causing damage to the main mooring. Despite the loss of the instrument, we will have collected all of the CT data in the logger which remains attached to the main mooring.  In addition, development of a smaller hydrophone for marine mammal monitoring has been ongoing for the past couple of years.

(Thank you to Eric for being a good sport and contributing the text for this blog post!).

*********************************************************************************

The rescue craft is prepared for launch to
transport science staff to Sisimiut.
Today, our approach to Sisimiut Harbor was stunning  (BTW, and I did not know this, Sisimiut Harbour is the worlds northern most harbor that does not freeze over in the winter, attributable to the Western Greenlandic Current that brings relatively warm Atlantic water up the coast of Western Greenland).  A blue sky with high wispy clouds provided the perfect back drop for colorful houses dotting the rugged coastline with the snow capped mountains looming large over the second largest city in Greenland.  Just as the sun was peaking over the horizon, Eric and other members of the science party disembarked via a rescue craft held by a crane over the water. I'm told that they will enjoy a hike in the surrounding mountains followed quickly, I'm sure, by a nice meal and some socializing. 

The air was crisp and a slight breeze put blush in our cheeks as we snapped pictures and longed for just one step on shore.  As soon as the boat returned from transport of its human cargo, we were off once more, heading back into the now choppy waters of eastern Davis Strait.  We now make our way towards the western side of the Northern Labrador Sea Line where we will begin nearly nonstop CTD operaitons until our arrival in Nuuk on the 25th.


The view on approach to Sisimiut.  Wow!
Sisimiut sunrise. Not bad eh?

A Temperature section of the Northern Line from Baffin Island to Greenland (hot off the press).  Note the northerly flowing warm water attributable to the Western Greenlandic Current invading the shelf.  This is what keeps Sisimiut Harbor ice free during the winter.  It's all relative, the dark red is only 4 degrees so no need to break out the bikinis.

Thursday, September 17, 2015

Holly Hogan - Seabird Observer for Canadian Widlife Service, Environment Canada (AKA Birdiologist)


Northern Fulmar image capture during AT3002.  Photo by Lance Wills.

I grew up in St. John’s NewfoundIand, were I also did my MSc. Degree; at Memorial University of Newfoundland (MUN).

Newfoundland is an island stuck well out into the flow of the Labrador Current.   For this reason, the Island is famous for both it’s cold wet foggy terrible weather and it’s incredible diversity of marine life. Located forty-five minutes from St. John’s is the second largest colony of Leach’s Storm-Petrels in the world, and the largest Atlantic Puffin Colony in North America (Witless Bay IslandsEcological Reserve).  Add another hour and a half to the drive and you are on the doorstep of the largest Leach’s Storm-Petrel Colony in the world (Baccalieu Island Ecological Reserve) or the second largest Northern Gannet Colony in North America (Cape St. Mary’sEcological Reserve).  As someone with an affinity for the natural world, the attraction is obvious.  I worked for the Canadian Wildlife Service, Environment Canada for close to a decade, and then managed both the Witless Bay and Baccalieu Ecological Reserves for the provincial government, Department of Environment andConservation.  In recent years I have been conducting offshore seabird surveys for the Canadian Wildlife Service, under the Environment Canada Seabirds At Sea (ECSAS) program.

These surveys provide important data on pelagic seabird distribution throughout the year, including patterns of dispersal from breeding areas, migration routes and wintering areas. Over time, these data will show not only patterns of dispersal, but also trends in species abundance, diversity and distribution.  Of particular interest on this cruise is the post-breeding dispersal of Dovekies, or Little Auks (Alle alle) from their breeding colonies to wintering areas. Several million Dovekies (approximately 80% of the world’s population) breed in northwestern Greenland.  Many of these migrate to coastal waters of northeastern North America via the Davis Strait. Dovekie chicks generally leave the colony with one parent (usually male); however, the amount of time spent with the family group is not well understood. During this cruise, I will be paying particular attention to Dovekie parent/chick associations whenever viewing conditions permit.  Adults and chicks have different plumages, which allows the distinction to be made: the adults have a solid white cheek patch that rises well above the eye.  The cheek patch of the chick is more buffy; appears less striking and does not rise as far above the eye.  In the right light, the dark brown hue on the chick’s back can be seen. These data will add to the growing body of data on family group dispersal during migration, and will provide important insight to this question.


As would be expected,  Dovekies and Northern Fulmars have been the most abundant species seen to date.

Are We There Yet?

Time: 0538 UTC
Latitude: 68° 51.046' N
Longitude: 56° 50.554' W
Conditions: As good as it gets! (Calm, clear and no wind)

We should be at NL_22 within the hour and by noon today (September 18th) we should be finished the Northern Line and beginning our steam south towards Sisimiut to drop off the mooring team.  We will then head even further south to begin work on some other (yet to be determined) sections.

The weather has been absolutely fantastic, in Arctic terms anyway. The coastlines, icebergs, seabirds and sunrises have made the trip fly by so far. Speaking of birds, the next post will be by Holly Hogan, an Environment Canada/Canadian Wildlife Service "birdiologist". OK, birdiologist is not her official title, but it seems to have become the affectionate nickname given by the crew for those who identify and enumerate sea birds/mammals during transits between stations.  I've sailed with Holly before on the Atlantic Zone Monitoring Program missions and she's a woman of many talents.  In addition to her "birdiologist" skills, she's a Body Flow instructor and an accomplished musician (new CD coming out. Plug plug!). She makes her home in St. John's Newfoundland and we're glad to have her on board with us.

Wednesday, September 16, 2015

Viewer Comments!!

Time: 0414 UTC
Latitude: 68° 19.006' N
Longitude: 61° 12.718' W
Conditions: I can't see!!! (Oh wait, just thick fog, sorry!)

Hi Everyone,

Yesterday I had some great comments from Brian Petrie, an Emeritus Scientist at the Bedford Institute of Oceanography in Dartmouth, Nova Scotia.  Brian wanted a regular updated cruise track. Good point Brian, and something I should have done before now!  Below is the cruise track as of the end of the 16th of September, 2015.  You can see we started in Nuuk, headed north to Disko Bay and then west along the Mooring Line and from west to east on the Northern Line. I'll try to have regular updates of the cruise track on the blog from now on:

Current location of the Atlantis (red triangle) and the cruise track (blue) since the beginning of the trip on September 6th until
September 16th, 2015
Brian also suggested that I produce some section plots for temperature and salinity.  I've provided a section plot below for the Northern Line (stations 1 through 10).  I've asked Brian (and others) to provide some interpretation of the plots and I'll make another post with their comments as soon as they are provided.

Interpolated contour plots for the Norther Line for the stations completed as of September 16, 2015.

Tuesday, September 15, 2015

The Northern Line

Time: 2140 UTC
Latitude: 67 32.77 N
Longitude:61 52.57 W
Conditions: Ahhhhhhh yeah! (Light winds and clear skies)

Hello Everyone,

We are 2 hours from the first station on the western most station on the Northern Line.  After a short period of cool and windy weather, we've now been granted a brief respite.  Currently, the temperature hovers near 2 degrees Celcius and the winds are gently blowing ~ 6 kts.  In Arctic terms, the perfect day really!  A night where we might be able to glimpse the northern lights.

I've run out of interesting things to say.  I know that some of you would counter that with, "nothing you say is interesting Andrew".  Fine then!  I've asked others on the ship to start pulling together short biographies and a brief summary of what they do and why they do it.  I'm sure they will more than spice things up a little. In the mean time, you will have to be happy with this very brief status update.


Saturday, September 12, 2015

CTD eh?

Time: 2032 UTC
Longitude: 59 05.1 W
Latitude: 66 19.5 N
Conditions: wicked good (5-10 kts wind, fog)
Upcoming Conditons: ughhhhhh (Monday - 40 kts wind)

The SSSG Technician manages the deployment of the CTD
aboard the R/V Atlantis (photo by Lorenza Raimondi)
What is a CTD, you say?  Right now, it seems like a self induced water torture device designed to make the victim experience piercing pain in each finger as you purposefully collect bone numbing water sample after bone numbing water sample, but I digress.  The acronym stands for Conductivity, Temperature and Depth; each parameter represented by a different sensor which collects these data and either stores them internally or transmits them through a cable back to the ship where they are viewed live and stored by operators.  OK, Coles Notes version (you can stop here if you want).

The name, "CTD", vastly understates the complexity of this bundle of oceanographic wizardry. It was originally branded the STD (Salinity, Temperature, Depth - Wow, poor acronym choice!) in 1960 but was later sold as the CTD in 1970 (Phew, that was close!  Find out more by reading Instrumentation and Metrology in Oceanography by Marc Le Menn). Since that time, the CTD has gained momentum, with new sensors occasionally being developed to add to the ever growing arsenal of this "Swiss Army Tool" of water sampling. As such, a world wide community of CTD users and data providers are established and require high levels of instrument precision and accuracy based on a generally agreed upon set of international standards.  Data generated by CTD's are sent by organizations the world over to central data repositories like the World Ocean Database (formerly, the National Oceanographic Data Center).  

Niskin bottles with tops open connected to the rosette carousel.
Photo by Lorenza Raimondi.
A modern CTD, like the one aboard the Atlantis, is truly amazing!  When combined, the bundle of probes which measure water column characteristics, is about the size of a large microwave oven.  The list of sensors on the CTD aboard the Atlantis is extensive and includes a primary and secondary set of temperature and conductivity (salinity) probes, oxygen, fluorometer, pH, Photosynthetically Active Radiation (PAR), pressure,(depth) and an altimeter. Whoa, that's a lot going on at the same time! Each instrument requires it's own form of baby sitting that could involve: soaking in fresh water between casts, bathing in a standard solution, covering a sensor head, etc... To further complicate the issue (or compliment probe measurements I suppose), this hyper-complicated mass of temperamental electronics is housed in a large cylindrical frame, upon which mounts 24 - 20L Niskin bottles.  These vertically positioned bottles employ an ingenious series of high tension bands that run through the center of the bottle to caps on either end.  Small but strong plastic wires at the top of the bottles radiate to ridged hooks on a central "carousel", holding the bottles open.  

A large electro-magnetic cable is "terminated" to the "CTD Rosette".  Many kilometers of cable (~6 km in our case), snakes its way through a "block" or wheel on the crane which protrudes from the starboard side of the ship.  The cable is wound tightly on a winch drum, which pays out the desired amount of cable required for the depth of deployment. The data from the CTD makes it's way up the cable during the cast and is visualized using software at the "Command and Control Center" in the Computer Room on the Atlantis. The bottles are fired at pre-determined depths, and each bottle contains enough water (hopefully) to meet the sampling demands of our scientists in the lab.


Note the large CTD cable attached to the central
part of the rosette.
Underway information provided by the ship.  Note the Time
Until Station used in the lab to determine when to prep
for deployment.
Alrighty then, here is our typical order of events.  You might want to grab a drink or get up and stretch a little before reading. Long before the cast, a spreadsheet of required sampling is produced along with the depths samples are required from. Depending on the area being sampled, different questions are being asked and require a unique subset of our analytical suite.  Each bottle on the rosette is then labelled with a unique sequential numerical identifier (a little sticker with numbers). All samples drawn from a bottle inherit this identifier for analysis.  As we transit towards our stations, we are watching a screen which provides us with an approximate arrival time.  We typically use this time to prepare our sample bottles and label them with stickers. Approximately 20 minutes from station, we make sure the rosette bottles are labelled with stickers, cock the bottles, remove sensor coverings and tubing and tie on tag lines to rings on the rosette frame. Once on station, the ship's SSSG (Shipboard Scientific Support Group) technicians correspond with the bridge to acquire approval for launching the gear over the starboard side of the ship.  The technician coordinates with the winch operator (housed in the next level up from the working deck) and the deck crew to deploy the CTD over the rail of the ship and into the water (science staff BTW - we don't sit at computers or stand in labs with coffee cups all day discussing the latest pocket protectors and episodes of Big Bang Theory.  OK, that happens sometimes, but who doesn't love a good pocket protector, right!) 

The Computer Room CTD Command Center aboard the R/V Atlantis
An operator in the Computer Room at the CTD control center (me) turns the CTD on via the "Deck Unit". Some time is required for pumps to engage that will move water through the CTD sensor package, and then the system is brought to the surface. The CTD acquisition software is turned on to log the data and the descent is initiated by a command to the winch operator to descend to 100 m at 30 m/min.  At 100 m, control of the winch is assumed by the SSSG technician in the Computer Room and descent to the final depth is initiated at 60 m/min until near the bottom where the speed of descent is reduced to minimize the likelihood of impact (and making lots of people very agitated).  The SSSG technician and the CTD computer operator can acquire the water depth from a sounder or on board multibeam system.  At 5 m off bottom, the CTD is stopped and the sensors are given time (~1 min) to come to equilibrium prior to firing the first bottle.  The SSSG technician then brings the CTD up to the next required depth and the process is repeated at predefined intervals until the CTD is at the surface.  At the surface, the science crew and SSSG tech prepare for receiving the CTD on the starboard side of the ship.  The CTD deck unit is shut off and the deck crew use long poles with hooks on the end to latch on to the CTD and use small tugger winches in coordination with the crane to bring the CTD back up over the rail and into position on the deck.  Once on deck, the CTD is ratcheted down and the science staff assume their positions to acquire samples from the rosette. OMG, I'm tired just thinking about it!

Water sampling order posted on white board in the lab for
a reminder when we start to lose our marbles.
The rosette sampling order is completed the same way each time based on the volatility of the parameter being investigated.  I'll have another post describing laboratory analysis, so I won't beat the point to death right now. Anyway, we all play "ring around the rosette" until samples are collected. This is the torture part I mentioned above.  The water is below zero at some depths and really makes you question your choice of career as it cascades over your increasingly useless and painful digits. Coupled with the wind and freezing temperatures on the open deck, it can be a less than pleasant experience.  Once the water has reduced your hands to frozen stumps, water sampling is complete. The water is then paraded back to the lab (just feet from the CTD for those of you on the Hudson) for sample preparation and/or storage.  The torture now enters it's second stage as feeling returns to your fingers. Joking aside, time at the rosette can be a pleasant experience.  Scientists emerge bleary eyed from the lab to take samples and usually return to the lab full of energy after getting some much needed arctic air and great conversation as we make our way around the rosette.  
Scenes of torture portrayed - parental guidance is recommended!  Steve rinses a flask in preparation for taking an oxygen sample.
The CTD is then cleaned and prepped for the next cast and the process repeats itself.  This is not meant to be an in depth review.  I've simplified a great deal and left out some information for the sake of brevity (OK, that did not work - sorry).  If you'd like to see a time lapse of the deck operations then click here for the YouTube video.  It's a messy business.  Water sampling at the end of the cast gets the lens wet, but you'll more than get the idea by then.

Thanks again for tuning in.  I'd like to have Steve Punshon go through the laboratory analysis for the next post, but he does not know this yet. Now you know how we get the water and monitor the environment, but the next question is, "Why Bother?". 

I'm Sleepy!!

Hi Everyone,

No blog post today.  We've put in a very long day (17 hrs now) so I'm going to make this short. Things are going well and the weather is great.  I hope to make a long post in the day or so discussing our CTD operations.  I made a time lapse video of our night time CTD operations.  I'll write some text around this video with help from my friends, to describe to you what data/samples we are collecting and what these data are used for.  It'll have to wait though because I'm going to fall to ......

zzzzzzzzzzzzz!

Friday, September 11, 2015

Lorenza Raimondi

Time: 0757 UTC
Longitude: 56 44.45 W
Latitude: 67 03.62 N
Conditions: Snow/Rain mix, 18 kt winds (Not enough snow for a snowman though, darn!)

Hi Everyone,

My name is Lorenza and today I will be writing for Andrew’s blog. I am originally from Napoli (Italy) but one and a half years ago I moved to Halifax to start my PhD in Chemical Oceanography under the supervision of Dr. Kumiko Azetsu-Scott (BIO) and Dr. Doug Wallace (Dalhousie University). I am currently on board of the RV Atlantis collecting samples across the Davis Strait.

Lorenza Raimondi running Winkler titration samples in the lab aboard 
My PhD project focuses on CO2 and O2 exchanges between ocean and atmosphere along the Labrador Sea, so this cruise is not really part of my PhD project but it’s indirectly linked with it since the Labrador Sea and the Davis Strait are adjacent areas strictly connected through water mass circulation. 

Why are we specifically observing the Labrador Sea area? As you may well know, there are areas in our oceans where deep waters are formed, triggering the entire ocean circulation known as Ocean Conveyor Belt. The Labrador Sea is one of these areas and contributes as a source to the North Atlantic Deep Water through deep convection. 

Our main goal is therefore to understand how winter convection affects the carbon chemistry in this key region. Do they serve as a source of carbon dioxide, releasing CO2 produced by remineralization at depth to the atmosphere, or as a sink, enhancing surface uptake and storage at depth?

During my PhD I will also focus on the anthropogenic fraction of carbon stored in the Labrador Sea. The anthropogenic carbon signal is very small compared to the natural background and different indirect estimates have been developed during last 20 years. So we would like to apply several methods and compare them to gain a clearer understanding of how human activities are affecting this important region.

Last but not least, we are also interested in dissolved oxygen trends during last decade. Are the concentrations changing over time? If yes, why is this happening?
Lorenza collects water samples aboard the
CCGS Hudson in April of 2014.

So now you are wondering, how can we measure these changes? Well, this is the reason why researchers need to conduct fieldwork and go at sea for weeks: to sample and measure the water column along transects and obtain data that will hopefully describe patterns and trends of different parameters. 

To characterize the carbon cycle we use 4 parameters, that we are currently sampling on board of the Atlantis: Total Alaklinity (TA), Dissolved Inorganic Carbon (DIC), pH and Partial Pressure of CO2 (pCO2). We also collect samples for Dissolved Oxygen and analyze them on board using the Winkler Titration method

Once back home, the data obtained will be processed and then, after hours and hours spent in front of the computer, will be used to present our results to the scientific community and open discussion on whether these results are comparable in similar regions or they completely disagree from previous works. Finally, this information will be “translated” for the general public in an effort to increase public awareness of anthropogenic impacts on the environment. 

Certainly this last part of our job does not sound very exciting compared to the adventures at sea, the time spent among whales, icebergs and astonishing northern lights but it’s the real target of our work. It’s the reason why we are doing all this: produce knowledge and share it with decision makers and the general public to shape future policies.

CTD Rosette bottles, ready for action (Photo by L. Raimondi)
Personally, I have contrasting feelings about the different steps that a scientist has to go through. When I spend days in my laboratory or office I feel like I'd rather be at-sea with the smell of sea in my lungs; however, if all that time pouring over data in a cramped space results in an idea or conclusion that can change public perception or policy for the better, then the hours of toil will be worth the effort!





Thursday, September 10, 2015

Mooring Operations - Time Lapse

Time: 0054 UTC
Longitude: 55 40.675 W
Latitude: 67 10.222 N
Conditions: 12 kt winds, partially cloudy, rain/sleet/snow

It was a beautiful day on the water.  Fair winds and blue skies dominated the weather throughout most of the day.  Mooring operations went smoothly and we've begun our CTD operations this evening, starting with ML_15 and moving west.

For those of you looking to avoid work this morning (OK, that's everyone), I've uploaded a mooring deployment time lapse done earlier today.  The mooring deployed at WG_01 is pretty short (~40 m) and was deployed pretty much all at once off the stern of the ship.  It consists of an ADCP (Acoustic Doppler Current Profiler), 2 SBE-37 Microcats which record temperature and conductivity, and an acoustic release attached to a train wheel anchor (see associated mooring diagram). Click here to see the deployment in it's entirety.  I've recorded the deployment of a much longer mooring done earlier in the day, but the bandwidth available on the ship precludes me from posting it on YouTube. Lorenza's post is coming soon!

Short mooring deployed at WG_01 on September 10th, 2015 - 60 nautical miles west of Sisimiut, Greenland.

Wednesday, September 9, 2015

Mooring Line - We're on it!

Time: 0537 UTC
Longitude: 54 41.119 W
Latitude: 67 14.635 N
Conditions: Awesome (OK, 1-2 m seas, 18 kt winds for those who care)

Hello everyone, we have begun work on the Mooring Line.  During the day, The University of Washington group and the Atlantis Crew worked on mooring recoveries and deployments on the Mooring Line.  Tonight, we are following right behind them, conducting CTD casts and collecting water for many different types of analysis.  

Tomorrow, you can expect a blog post from PhD student Lorenza Raimondi.  She is specializing in "Carbon Cycle Chemistry" at Dalhousie University, but I won't ruin it by giving too much away.  Expect more guest posts over the next few days as I've become increasingly boring.
This is our current location.  We are generally heading west as we complete the mooring line.  The air temperature right now is about 2.3 degrees Celsius.

Tuesday, September 8, 2015

Let's get it started!

Time: 0346
Location: Disko Bay
Longitude:53 53.05 W
Latitude:68 59.304 N
Conditions: Ahhhhh! Nice.

Photo courtesy of Lance Wills.
Finally, the bad weather seems to have subsided for now at least. Today, we saw operations begin in Disko Bay with the first CTD of the mission at DKM_08.  Ring nets were also deployed along with CTD's at stations across the Disko Bay channel,  The weather today was nothing short of spectacular.  As advertised, the ship was circled by ice bergs.  Mountainous peaks, mixed with glacial valleys loomed large in the distance.  It was a perfect day for us to learn about how the Atlantis crew goes about CTD operations on Atlantis.  Their operations are impressive and I'll go through them at length another time.

The day was a success and there were very few technical challenges.  The crew of the Atlantis walked us through their process and made us feel right at home.  Thank you everyone.

As an aside, during the evening there was a bright display of northern lights off the port side of the ship.  At times they lit up the sky from horizon to horizon. I tried to take some photos and I've attached the best of what I could produce.
Station occupations in Disko Bay included CTD's at DKM_08, DKM_06, DKM_04 and DKM_02 and ring nets at DKM_04 and DKM_06.
Saw some northern lights tonight.  These buggers are hard to photograph on a rolling ship but worth the effort.

Our second CTD deployment.  Steve handles it in style.

Yay, icebergs.  The bridge was not so happy to see them though, I guess they sink boats sometimes;)


Monday, September 7, 2015

Tomorrow - it's only a day a way!

We've been told by the Chief Scientist that our arrival in Disko Bay should be around 1400 to 1900 on September the 8th.  The forecast is for high winds on Tuesday (40 kts) and then turning to light on Wednesday afternoon.  Fingers crossed we can get started soon!

How much longer now Papa Smurf?

Time: 1022 UTC
Latitude:65 58.183 N
Longitude:55 03.784 W
Conditions: Ughhh!

In another 70 miles (or ~10 hrs) the ship will begin mooring operations at WG_04. Upon completion, the intent is to sail towards Disko Bay and complete select stations at the DKM and/or DKOT stations before proceeding to the eastern most end of the NL line.  Much of this plan is largely contingent on the sea/ice state.  Disko Bay is home to an armada of ice bergs, a Dr. Seuss like wonderland of sea and ice. The Captain, in consultation with the Chief Scientist, will decide on whether stations can be occupied given the constraints. 

Last evening we began switching over to our regular shifts.  I made it to 3 am before my eyes betrayed me and I fell to sleep watching Avatar on a rolling ship (pretty trippy).  I will be working 6 pm until 6 am throughout the majority of the mission.  Despite this, I'll try my best to provide you with day time images of our operations and the places we visit.

Steve, Lorenza and I will review chemistry sampling protocols this morning before I head back to the rack and get some z's. That's all for now.


Sunday, September 6, 2015

Gumby and Pokey

Gumby and Pokey say "Hi" from Greenland.  "Sure looks rough on the west coast of Greenland Pokey!"
Keep your eye's open for Gumby and Pokey throughout the mission. They wanted to come with me to the arctic this year and I can't blame them.  The love going to sea and no matter what is happening they always smile, unlike me.

Ughhhhh!

Time: 2240 UTC
Latitude: 65 34.8409 N
Longitude: 052 41.2060 W 
Conditions: Ughhh!

Me no feel good.
I have a confession to make to all the world!  I get sea sick.  There, that feels better.  OK, so I don't get sick all the time, only when it is really rough and usually at the front end of a mission when I've not had time to adjust. Some people never get sea sick, others develop symptoms as they age and others lose them as they "mature". 

"A marine biologist that gets sick at sea?" you say.  Well, it's more common that you think.  Right now for instance, there is more than one person on this ship experiencing some measure of gastrointestinal melt down.  For me, it starts with a general sleepy feeling followed unpleasantly by a light sweat, an urge to swallow repeatedly and then an uncontrollable urge to, well, expel my stomach contents.  Unlike when you are sick with the flu, vomiting seems to provide no relief.  The only things that seem to help are:
  1. Looking at the horizon - which stinks because the only good view during rough weather is generally on the bridge and sometimes moving higher on the ship makes it worse.
  2. Drugs - which generally make me drop 20-50 IQ points and want to fall asleep anywhere.
  3. Sleeping
The Atlantis plows through a wave!

Well, what do you do when those things are not an option. I need all of my IQ points (I have none to spare), I can't generally sleep on the job despite what some people think of government workers and I find it hard to work/sleep while vomiting.  You see my dilema! 

The reason I'm providing you with this generally useless bit of information is that I am currently sea-sick. Well, I'm well enough to write this blog, so not entirely bed ridden, but still generally not well.  The seas were very rough as we departed Nuuk today.  The wind is consistent at 35 kts, the swell is 15-20 ft and seems to come from every direction at once. Our current speed reflects the rough weather as we slog through the storm, moving north at ~5-7 kts. The ship pitches, groans and occasionally shudders as it punches through waves.  Every half hour or so, a combination of rollers sends the ship into a wild pitch forward that causes all of the furniture to slide and cabinet doors to open. This is usually coincident with a sudden jarring that causes you to lose balance, and in my case lunch.  Despite what you might think of sea sick marine biologists, ship's captains, and oceanographers, to me it just show the dedication that these people display (sometimes for decades) for their chosen career.  

Despite the rough weather, it's still amazing to be at sea.
I hope that the weather is better tomorrow.  For now, I'm going to find a nice place to relax and keep my supper down.


Underway


The view leaving Nuuk.  Bye Nuuk!
We are finally underway.  The internet connection is very slow so I hope that the few photos that I took this morning will load.  We had a safety and security meeting yesterday and this morning proceeded with the fire and evacuation drills.  The seas are definitely choppy, but the ship is comfortable and pretty quiet.  

This morning I modified the display settings for the CTD acquisition software.  For those of you that are unfamiliar with a CTD (Conductivity, Temperature and Depth), it is really just a bank of sensors that collect environmental data.  The sensors are placed onto a frame that allows for a full profile of the water column and allows us to collect water samples on a "rosette" at pre-determined depths.  For more information concerning CTD's and how they work, visit http://oceanexplorer.noaa.gov/facts/ctd.html.  

We have a science meeting at 1 pm this afternoon, but I expect us to get sciency (not a real word) very quickly. 

Pre-cruise ship familiarization meeting.

Gumby has a friend.

Saturday, September 5, 2015

Bye Nuuk (sniff, sniff)

Gumby and Pokey say farewell to Seaman's Home in Nuuk Greenland.
Well, it's time to say goodbye to the Seaman's Home.  We board the Atlantis today to begin our 20 day journey across Davis Strait and Baffin Basin.  There is still more to do before we leave, like packing away boxes and making sure our equipment is properly secured.  It'll get pretty rough out there so equipment needs to be tied down.

I explored a little of Old Nuuk this morning on my jog and it was picturesque.  The view of the fjord is fantastic and definitely worth a visit if you are in town.

It will be nice to get the science started tomorrow and start sharing that with all of you.  The internet on the ship is slow and may or may not allow me to provide posts at the intervals I would like.  Stay tuned!