Christine Hedge, August 26, 2009

NOAA Teacher at Sea
Christine Hedge
Onboard USCGC Healy
August 7 – September 16, 2009 

Mission: U.S.-Canada 2009 Arctic Seafloor Continental Shelf Survey
Location: Beaufort Sea, north of the arctic circle
Date: August 26, 2009

Science and Technology Log 

This is what we see in the Science Lab of the Healy before the data is processed.  It is like a cross-section through the top 50-100 meters of the sea floor.  Here you can see it was flat and then climbed uphill.  The numbers represent round trip travel time in seconds.
This is what we see in the Science Lab of the Healy before the data is processed. It is like a cross-section through the top 50-100 meters of the sea floor. Here you can see it was flat and then climbed uphill. The numbers represent round trip travel time in seconds.

Is There a Bird in My Room? 

When I first got on the Healy, I thought there was a bird in my room.  Then I realized the chirp that I kept hearing every 9 seconds or so was not just in my room.  It got louder as I went down the ladders to the deepest part of the ship near the laundry. I found out that this chirp is the sound transmitted by the subbottom profiling system.  This instrument is being used on the Healy to collect data about the depth of the water and the nature of the sea floor. These subbottom profiler transducers are mounted on the hull of the ship. The “chirp” sound reflects (echos) off the bottom of the ocean and also reveals the sediment layers below the bottom.  This is one of the systems I watch on a computer screen when I am working.

Using Sound as a Tool to See Inside the Earth 

Sound is an amazing tool in the hands of a geophysicist, who is a person who studies the physics of the earth. The subbottom profiler uses a low frequency sound. Low frequency will penetrate further into the earth than the higher frequencies used by echosounders. This helps scientists to “see” about 50 meters below the surface, depending on the type of sediment (clay, sand, etc).  By looking at how the sound waves are reflected back to the ship, scientists can see layering of sediments, infer sediment type (REMEMBER SAND, SILT, CLAY???), and sometimes see evidence of channels under the sea floor.

The subbottom profiler data is processed and an image is generated for scientists to analyze.  This is an image from the 2005 Healy trip to the Arctic.  You can see the types of features the sound waves can “see” for us.
The subbottom profiler data is processed and an image is generated for scientists to analyze. This is an image from the 2005 Healy trip to the Arctic. You can see the types of features the sound waves can “see” for us.

FOR MY STUDENTS:  DO YOU REMEMBER STUDYING SOUND IN 6TH GRADE?  WHAT DOES FREQUENCY REFER TO?  

These pictures appear on many doors of the Healy
These pictures appear on many doors of the Healy

Why Is This Important? 

Geologically speaking, the Arctic Basin is poorly understood. We are not sure how some of the major features formed or even where the plate boundaries are.  When you look at maps of the tectonic plates, you might notice that they are not clearly marked in the Arctic. Understanding how the sea floor is shaped and what lies beneath will give us clues to understand the history of the Arctic Basin. From a practical standpoint, geology can tell us where important natural resources might occur. When companies are searching for natural gas or petroleum, they are using clues from the geology of the sea floor to decide where to look.

Personal Log 

More About Sound – From A Personal Perspective 

Lieutenant Commander Doug Petrusa wearing protective headset
Lieutenant Commander Doug Petrusa wearing protective headset

As far as I can tell there is no place on a ship where it is completely silent.  There are fans, air compressors, engines, doors opening and closing and of course on this ship ice breaking and chirping.  There are some places on the ship where we are warned to use ear protection because the machine noise could, over long periods, cause hearing loss.  Many doors on the ship have pictures reminding us to wear ear protection in certain areas to protect our hearing.   The crew spends time working in areas with high intensity noise – so they are often seen wearing protective headsets.

In addition, all over the ship, there are boxes of earplugs. These are available for people to use whenever they need them.  My first week, I slept with earplugs every night.  The constant chirping, the sound of the engines and the doors opening and closing were more than I could handle. I thought I would need to use earplugs for the entire journey. Now, I am sleeping like a baby even with the additional sound of us plowing through ice. I guess the human body can get used to just about anything.

Earplugs are found near every doorway that leads into an area with dangerous noise levels.
Earplugs are found near every doorway that leads into an area with dangerous noise levels.

Christine Hedge, August 25, 2009

NOAA Teacher at Sea
Christine Hedge
Onboard USCGC Healy
August 7 – September 16, 2009 

Mission: U.S.-Canada 2009 Arctic Seafloor Continental Shelf Survey
Location: Beaufort Sea, north of the arctic circle
Date: August 25, 2009

Weather Data from the Bridge 
Temperature: 30.150F
Latitude: 81.310 N
Longitude: 134.280W

Science and Technology Log 

This multibeam image of the new seamount is what I saw in the Science Lab.
This multibeam image of the new seamount is what I saw in the Science Lab.

A Day of Discovery… 

Today, our planned route took us near an unmapped feature on the sea floor.  A 2002 Russian contour map showed a single contour (a bump in the middle of a flat plain) at 3600 meters.  This single contour line also appeared on the IBCAO (International Bathymetric Chart of the Arctic Ocean) map.  We were so close that we decided to take a slight detour and see if there really was a bump on this flat, featureless stretch of sea floor. 

The contour was labeled 3600 meters and the sea floor in the area averaged about 3800 meters so a 200 meter bump was what the map suggested.  As the Healy traveled over the area we found much more than a bump!  The feature slowly unfolded before our eyes on the computer screen.  It got taller and taller and excitement grew as people realized this might be over 1000 meters tall.  If a feature is 1000 meters or more, it is considered a seamount (underwater mountain) and can be named.  Finally, the picture was complete, the data was processed, and a new seamount was discovered. The height is approximately 1,100 meters and the location is 81.31.57N and 134.28.80W.

The colors on this 3-D image of the newly discovered seamount indicate depth.
The colors on this 3-D image of the newly discovered seamount indicate depth.

Why Isn’t the Arctic Mapped? 

Some areas of the sea floor have been mapped and charted over and over again with each improvement in our bathymetric technology.  Areas with lots of ship traffic such as San Francisco Bay or Chesapeake Bay need to have excellent bathymetric charts, which show depth of the water, and any features on the sea floor that might cause damage to a ship.  But in the Arctic Ocean, there isn’t much ship traffic and it is a difficult place to collect bathymetric data because of all the ice. Therefore, in some areas the maps are based on very sparse soundings from lots of different sources. Remember, older maps are often based on data that was collected before multibeam  echosounders and GPS navigation – new technology means more precise data!  

Personal Log 

This is the IBCAO.  (International Bathymetric chart of the Arctic Ocean)  It is a great resource for ships exploring the Arctic Basin.
This is the IBCAO. (International Bathymetric chart of the Arctic Ocean) It is a great resource for ships exploring the Arctic Basin.

It is still very foggy. We are about 625 miles north of Alaska and plowing through ice that is 1-2 meters thick.  This time of year it is the melt season.  Increased evaporation means more water in the atmosphere and more fog.  Even though we are usually in water that is 90% covered by ice (REMEMBER 9/10 ice cover?) we rarely have to back and ram to get through.  It is noisier lately and the chunks of ice that pop up beside the ship are more interesting to look at.  There are blue stripes, brown patches of algae and usually a thin layer of snow on top.

I cannot send a current sound file because of our limited bandwidth on the Healy. When we are this far north it is difficult to get Internet access. But, if you would like to hear what it sounds like when the Healy is breaking ice, click on this link  from a past trip through Arctic sea ice.

Sea Ice at 810N after the Healy has broken through
Sea Ice after the Healy has broken through