Tag: Humpback whale

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Deborah Moraga, June 21, 2010

NOAA Teacher at Sea Log: Deborah Moraga
NOAA Ship: Fulmar
Cruise Dates: July 20‐28, 2010

Mission: ACCESS
(Applied California Current Ecosystem Studies)
Geographical area of cruise: Cordell Bank, Gulf of the Farallones and Monterey Bay National Marine Sanctuaries
Date: June 21, 2010

The R/V Fulmar

Overview
The R/V Fulmar sets out from the dock early each morning. This ACCESS cruise has 5 members of the scientific team and myself (the NOAA Teacher at Sea.) There are two crew members for a total 8 people onboard.

The three central California National Marine Sanctuaries and the ports where the R/V Fulmar docks
The three central California National Marine Sanctuaries and the ports where the R/V Fulmar docks
Applied California Current Ecosystem Studies
Applied California Current Ecosystem Studies
National Marine Sanctuaries
National Marine Sanctuaries

ACCESS is an acronym for Applied California Current Ecosystem Studies. This is a partnership between PRBO Conservation Science, Cordell Bank National Marine Sanctuary and the Gulf of the Farallones National Marine Sanctuary. These groups of conservation scientists are working together to better understand the impacts that different organisms have on the marine ecosystem off the coast of central California.

Immersion suit for safety

They do this so that policy makers (government groups) have the most accurate data to help them make informed decisions on how the productive waters off the coast can be a resource for us and still protect the wildlife. You can read a more in depth explanation at http://www.accessoceans.org

Flying Bridge

The R/V Fulmar is a 67 foot Marine Grade Aluminum catamaran (a multi hulled vessel.) This vessel can travel 400 miles before refueling and can reach 27 knots (30 miles per hour) with a cruising speed of 22 knots (25.3 miles per hour.) Although that may sound slow compared to the cars we drive… you have to take into account that there can be 10 foot waves to go over out on the ocean.

The Fulmar’s homeport (where the boat ties up to dock most of the time) is in Monterey Bay, CA. For this cruise we will come into port (dock) in Bodega Bay, Sausalito, and Half Moon Bay. Each morning the crew wakes up an hour before the time we start out for the day. They check the oil and look over the engines, start the engines, disconnect the shore power and get the boat ready to sail out for a ten hour day.

Today (July 23, 2010) we left at 0700 (7:00 a.m.) out of Bodega Bay. Bodega Bay is on the coast of Sonoma county, California. It is from Bodega Bay that we will travel offshore to the “lines” that we will be surveying. Today we will survey lines one and two.

Then after the day’s work is done, we will sail into port, tie up to the dock and have dinner. The scientists and crew members sleep on the boat in the berths (bunks) that are located in the hulls of the boat.

Surveys
“Okay, take a survey of the types of pets your classmates have at home. Then create a graph.” How many times have math teachers assigned that assignment and expected that students knew how to survey? Today I received firsthand knowledge of how a survey takes place.

Marine scientist scanning for wildlife

Up on the flying bridge (about 5.5 meters from the surface of the ocean) scientists are surveying birds and marine mammals. There is a protocol that each follows. Here, the protocol is basically a list of agreed upon rules on how to count the marine life seen on the ocean. One researcher inputs the data into a waterproof laptop…imagine chilling at the pool and being able to surf the web! There are other researchers sitting alongside and calling out the types of birds and marine mammals they see. The researchers surveying the birds and mammals use not only their eyes but also binoculars.

Krill collected by the Trucker Trawl

After the researcher spots and identifies the birds or mammals, they call out their findings to the recording scientist in a code like fashion, doing this allows for the data to be inputted faster. The team can travel miles without Krill collected by the Trucker Trawl Researcher recording observations on the flying bridge Pacific White Sided dolphins bow riding seeing any organisms or there may be so many that the scientist at the laptop has a tough time keeping up. In this case the surveying scientist may have to write down their findings and report them when there is a break in the action.

Imagine that you are driving down the highway with your family. You have been asked to count the number humans, cows, horses, goats, dogs, cats, cars or trash on your trip. How would you make sure that your family members didn’t double count and still record all that you see? This is where protocols (instruction/rules) come in. So, let us say that you are behind the driver, and your brother or sister is in the backseat next to the window. There is also a family member in the passenger seat up front (yeah they called ‘shot gun’ before you did.) This is much like the seating arrangement on the flying bridge of the R/V Fulmar.

Researcher recording observations on the flying bridge

So how could you split up the road and area around the road so that you do not count something twice? You could split the area that you see into two parts. Take your left arm and stick it straight out the window. Have your sister/brother stick their right arm out their side window. If we drew an arc from your arm to your sibling’s arm it would be 180 degrees. Of the 180 degree arc, you are responsible for counting everything from your arm to the middle of the windshield. So, you are responsible for 90 degrees and your sibling has the other 90 degrees from the middle of the windshield to their arm.

Pacific White Sided dolphins bow riding

Once you start counting you need to record the data you are collecting. Can you write and count at the same time? Not very well, so we need someone to record the data. There are actually a lot of points of data that you need to enter.

You need to tell the recorder…
• Cue: How did you see the item you are counting?
• Method: Were you searching by eye or using a pair of binoculars?
• Bearing: The angle that the item is from the car as related to the front of the car.
• Reticle: How far the item was from your car when you first observed it (you would use your binoculars for this measurement).
• Which side of the car are you on and who is dong the observing?
• Behavior: What was the organism doing when you spotted it? Was it traveling, feeding or milling (just hanging out)?

Deploying the CTD

You also have to determine the age and sex of the organism. You need to record the species of the organism and how many you observed.
Now that is all for the species above the ground… what would you do for the animals below the road surface? On the R/V Fulmar they collect species from below the surface of the ocean and data about the water. They do this several different ways…

Bringing in the Hoop Net

1. CTD: Conductivity, Temperature, and Depth. This is a tool that records the physical properties of the ocean. It records…

a. Salinity (amount of salt in the water)
b. Temperature (how hot or cold the water is)
c. Depth (how far the instrument travels below the surface)
d. How much chlorophyll is in the water
e. Turbidity (how murky or clear the water is)
f. How much oxygen is in the water

Deploying the Tucker Trawl

2. Hoop Net: Looks like a very heavy hula hoop. Except this hoop has a cone shaped cylinder made of fine mesh attached to it. At the apex of the cone, a small PVC container, called a cod end, is attached. Zooplankton (tiny swimming animals) and some phytoplankton (tiny marine plants) are funneled into the cod end of the net as it is towed behind the boat. When the net comes back to the boat, the researchers take off the cod end and use this sample of organisms.

Collecting data from the CTD

3. Tucker Trawl: Is like three hoop nets attached together. The cool thing about this big net is that the scientists can close each net at different depths. As Map of the transect lines Retrieving the Hoop Net Phytoplankton Net the net is towed behind the boat they “close” each net to capture zooplankton at different depths. The tucker trawl is used primarily to collect krill

Map of the transect lines

Transects
Have you ever lost something in your room? Perhaps it was your homework? The bus is coming and you have to find your binder. So you start tearing your room apart. By the time the bus is five minutes away… you room looks like a disaster and you can’t remember where exactly you have looked and yet, still no binder.
Imagine a group of scientists 30 miles offshore, doing that same type of “looking” for organisms, with the captain piloting (driving) the boat any which way. Just like your binder that was missed when you were looking for it, number and location of organisms in parts of the ocean would be missing from the data set.

Retrieving the Hoop Net

So if you wanted a systematic way to look for your homework that is lost in your room, you would imagine a grid. You would have lines running from one wall to another. These lines would be parallel to each other. You would walk along the line looking for you binder. When you came to the end of the line (at your wall) you would then start on another line. By walking back and forth in your room in this systematic way, you will not miss any part of your room.

Phytoplankton Net

You have just traveled along a transect line. A transect is a path you travel and as you do you are counting and recording data. On the R/V Fulmar, scientists are counting birds, marine mammals, and collecting krill. By counting how many and what kinds of organisms are along the transect line, scientists will be able to calculate the density of organisms in a given area. There are several different types on lines that we survey. There are the near shore transects…which extend 12 kilometers from the shore (that is as long as running back a forth a football field 131 times). Offshore lines are 50 to 60 kilometers from the coast. Imagine how many football fields that would be!

Bow of R/V Fulmar

Density… Take your right hand and put it in your right front pocket of your pants and pull out all the coins you have in your pocket. Looking down at your hand you count 10 dimes. Now do the same for your left hand. You found you have two dimes. The “area” those coins were located is equal… meaning your pockets are the same size. The density of coins in your pockets is greater in your right pocket because there are more coins per square inch than in your left pocket.

Humpback Whale

The researchers on the ACCESS cruise use the data they have collected out in the field (in this case the field is the three central California National Marine Sanctuaries) to calculate the density of the organisms they are researching. They are counting and recording the number of organisms and their location so they can create graphs and maps that show the distribution of those organisms in the waters off the coast.

Taking a surface water sample

Why do they need this information? The data starts to paint a picture of the health of the ecosystem in this part of the world. With that information, they can make suggestions as to how resources are used and how to protect the waters off the California coast. By using data that has been collected over many years, suggestions can be made on how the ocean can still be utilized (used) today while insuring that future generations of humans, marine mammals, birds and krill have the same opportunities.

whale breach
whale breach
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David Altizio, May 22 – 23, 2010

NOAA Teacher at Sea
David Altizio
Onboard NOAA Ship Fairweather
May 17 – May 27, 2010

NOAA ship Fairweather
Mission: Hydrographic survey
Geographical Area of Cruise: SE Alaska,
from Petersburg, AK to Seattle, WA
Dates: Saturday, May 22 and Sunday, May 23

Me standing on the rocks, making tidal observations.

Weather Data from the Bridge

Position: Customhouse Cove                  Position: Customhouse Cove
Time: 0800 on 5/22                                   Time: 0800 on 5/23
Latitude: 550 56.01’ N                              Latitude: 55006.5’N
Longitude: 1310 13.75’ W                       Longitude: 131013.7’W
Clouds: Mostly Cloudy                               Clouds: Mostly Cloudy
Visibility: 10 miles                                      Visibility: 10 miles
Winds: 6 knots from the NW                     Winds: 6 knots from the SE
Waves: Less than one foot                         Waves: Less than one foot
Dry Bulb Temperature: 12.20C         Dry Bulb Temperature: 11.00C
Wet Bulb Temperature: 10.20C        Wet Bulb Temperature: 9.80C
Barometric Pressure: 1015.0 mb     Barometric Pressure: 1010.0 mb
Tides (in feet):                                             Tides (in feet):
Low @ 0224 of 2.8                                         Low @ 0335 of 1.5
High @ 0828 of 12.2                                      High @ 0943 of 12.4
Low @ 1436 of 1.6                                          Low @ 1537 of 2.0
High @ 2105 of 14.6                                      High @ 2159 of 15.4
Sunrise: 0424                                               Sunrise: 0423
Sunset: 2100                                                 Sunset: 2101

Science and Technology Log

On Saturday morning I went out and made observations at a tide gauge in Customhouse Cove. We took measurements over a three hour period every six minutes for a one minute interval. We used a pair of binoculars to read the tide staff, which was about 20 feet away, to the nearest millimeter. The purpose of taking this reading over a period of one minute is because the water is constantly moving both toward the shoreline and away from it. This interval ensures that you can get the most accurate reading as possible.

Tide staff, used for measuring rising and falling tides

On Sunday, I again went out on a small launch boat. This time we needed to complete a few more holidays using the multi‐beam sonar, then we went to two small islands, Smeaton and South Twin, to recover the GPS (global positioning systems) base stations.

Computer screen,showing live acquisition of multi-beam SONAR data from one of the holidays.

The GPS base station data is recorded daily, while the survey project is underway. The data is then uploaded during the processing phase and used to correct the precise position of the Fairweather and its launches to within a few centimeters of accuracy. This allows the survey technicians to know the exact horizontal position when all of the data was collected by the multi‐bean sonar. Sunday was the last day that data was collected on this project, and that is why we recovered both of the GPS bases stations.

Me,in the process of removing one of the GPS base

When the tide gauge was established for measurements, during April of 2010, a three hour period of observations was made, similar to what I did on Saturday morning. In the time since April, observations are to be made each week for at least 1‐2 hours. Due to the remote nature of some of the tide gauge locations this is not always possible. The purpose of the observations of the rising and falling tide is to establish the vertical location of the tide gauge sensor, which is submerged below the surface, in relation to the tide staff. These observations help in correlating the height observed on the tide staff, with benchmarks that were previously installed by the Fairweather crew along the beach.

Maritime activities throughout the world depend on accurate tidal and current information for safe operation. NOAA’s National Ocean Service collects studies and provides access to thousands of historical and real‐time observations as well as predictions of water levels, coastal currents and other data.
Ocean tides move in response to gravitational forces exerted by the moon and sun. Since the moon is much closer to the Earth it is the dominant force that affects Earth’s tides. Whichever side of the Earth is facing the moon experiences a greater gravitational attraction, and the oceans get pulled towards it causing a bulge.

Me, holding the rod for leveling measurements (with the Fair weather in the background).

When the highest part or crest of the wave reaches a particular location, high
tide occurs; low tide corresponds to the lowest part of the wave, or its trough. The difference in height between the high tide and the low tide is called the tidal range. Here, in SE Alaska there is almost a 15 feet difference between high and low tide.

Me,reading the level off of the leveling rod(again with the Fairweather in the background).

Most coastal areas, experience two high tides and two low tides every lunar day. Almost everyone is familiar with the concept of a 24‐hour solar day. A lunar day is the time it takes for a specific site on the Earth to rotate from an exact point under the moon to the same point under the moon the next day.

One of the benchmarks on the beach.

On Saturday afternoon, we went back to the tide gauge to take elevation levels of five benchmarks on the beach. The purpose of these measurements is to establish a vertical height of the tide gauge with five existing benchmarks. When the gauge was started in April 2010, the same measurements were made. We verified that the opening and closing measurements were within an acceptable range. After taking height measurements, I helped take out one of the prototype tide gauges since the data was not needed anymore. The regular gauge was later removed on Sunday.

Part of the tide gauge instruments, solarpanel, GPS transmitter.

I was able to help out with these height measurements by holding a rod on top of the benchmarks, while another member of the crew looked through a scope and read the levels off of the rod. We also documented the entire site by taking photographs.

A humpback whale tale.

Personal Log

The weather on Saturday was probably the best I have had in SE Alaska so far. It was sunny and in the low 60’s. I learned a few days ago, that when you are out at sea and it is sunny you need sunscreen and a baseball hat in order to not get sunburn. As I told you, on Saturday morning I was dropped off by a small boat to observe the level of the tide. Nothing too exciting, but the weather made it just fine. Since we were very close to the ship, I was able to come back on and have “hot” lunch rather than sandwiches and stuff. In the afternoon, we went back to the same tide gauge and I helped out with elevation studies is the easiest way to say it. This was better than the morning for me.

In the morning one other guy and I were literally dropped off on a barely exposed rock just offshore from the tide gauge. When we started there was water between the two of us, but we knew the tide was dropping so we were fine. However, we were sort of stranded there until the small boat picked us up for lunch. We had to take levels of the water every six minutes. Sounds boring but it went by rather quickly. As the tide dropped small tidal pools were exposed and I was able to explore. There was tons of sea life. It reminded me of Point Loma near San Diego, where I vacationed once. While we were there, of course there were bald eagles and even a few seals.

In the afternoon we actually went onto the beach and I got to explore a little. First time on land since Ketchikan; which we are still very close to. I was in my full on geologist mode, breaking and smacking rocks to see what they looked like on the inside. I saw some cool stuff, possibly some small flakes of gold, garnet crystals, and maybe some silver flakes. The captain (CO) also came along with us, which was pretty cool.

Dinner was good. Baked potato bar, some interesting tofu dish (most people ate prime rib, very rare, uncle Jerry style), salad, and coconut lemon cake for dessert. I am getting spoiled from all this good food. I watched another amazing sunset from Customhouse Cove on Saturday (that makes 3 from the same anchor spot).

Sunset on Saturday 5/22

Sunday, the weather was not as nice as Saturday; at least it did not rain. However I really did enjoy the day. The crew that I was with was great. We all got along very well. I was able to get onto land three times and explore and climb around on the rocks. Also we saw two humpback whales, a bunch of seals, more Dall’s porpoises, and yes more bald eagles.

Being able to go onshore was really special for me. I was not sure this was something I would be able to do. From here we will start making our course to Seattle. We were just told that we WILL be going through the “inside passage” which is supposed to be absolutely spectacular. I can’t wait.

For now the project is almost complete. There is only a small amount of data and bottom samples that need to be collected. I am enjoying my time onboard the Fairweather. Everyone has been very nice. I have developed a routine. I get up at 0640, breakfast begins at 0700, there is a safety meeting on the bow of the ship at 0800, then if you are on a launch you leave and come back in the late afternoon. Dinner is served at 1700, then after dinner we have a debriefing meeting to discuss the day’s work and any problems that may have been encountered.

As I said I have a little routine. Even the breakfast steward (cook) knows me by now. I come into the mess hall (dining area) and ask for my usual. Three scrambled eggs with scallions and cheese. I also have one piece of toast, three strips of bacon, some hash browns and fresh fruit, some coffee and orange juice. Not too bad. If you are doing survey work from the ship there is hot lunch at 1200, otherwise on the launches it is a bag/picnic style lunch. Yes I know I am getting spoiled with all of this good food.

Me enjoying my time on shore.
Sunset on Sunday 5/23
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Justin Czarka, August 14, 2009

NOAA Teacher at Sea
Justin Czarka
Onboard NOAA Ship McArthur II (tracker)
August 10 – 19, 2009 

Mission: Hydrographic and Plankton Survey
Geographical area of cruise: North Pacific Ocean from San Francisco, CA to Seattle, WA
Date: August 14, 2009

Weather Data from the Bridge 

Sunrise: 6:29 a.m.
Sunset: 2033 (8:33 p.m.)
Weather: patchy mist
Sky: partly to mostly cloudy
Wind direction and speed: Northwest 10-15 knots (kt)
Visibility: unrestricted, reduced to 1-3 nautical miles (nm) in mist
Waves: northwest 3-6 feet
Air Temperature: 17.50°C
Water Temperature: 17.63°C

Science and Technology Log 

Today I rotated to a new job assignment. I have been working with the CTD water samples, storing nutrient samples, and preparing chlorophyll samples.  Now I work with Jay Peterson, researcher from Oregon State University, Hatfield Marine Science Center, Newport, Oregon, deploying, retrieving, and preparing live samples from the vertical net and bongo net on a cable.

The vertical net gets rinsed off after the tow.
The vertical net gets rinsed off after the tow.

The nets collect all types of plankton, both plants and animals.  As with all the sample collections occurring aboard the McArthur II, communication is the backbone of the operations, or “ops.” For the vertical net and bongo net, two people manually place the nets over the ship’s starboard side, while a winch operator deploys and retrieves the nets from the ocean, and the bridge navigates the ship. For vertical nets, the goal is to take the net to 100 meters (m) depth and then hauled up vertically. The purpose is to catch organisms from the entire water column up to the surface.  It is the same depth for the bongo net, but the goal is to have the cable at a 45° angle with the ship moving at a steady 2 knots (kt). Both nets have flowmeters to determine the volume of water that goes through the net. Once back on the deck, the nets are rinsed from the top to the bottom so that everything in the net can be analyzed. The samples are placed in jars or buckets to observe under microscope.  We find euphausiids (krill), copepods, Tomopteris, Chaetognatha (arrow worms), fish larvae, Phronima, and even bird feathers!  You have to check out these animals online, as they all have fascinating features. More importantly, while small in size, they are an essential part of the food web. Without them, many species would struggle to find food.

Personal Log 

Today we a day of plenty in terms of sighting marine mammals and other species as well!  The day started out near shore at Newport, Oregon and the Yaquina Head Lighthouse.  The McArthur II travels roughly in a zigzag approach near shore to off shore and back for this mission.  Getting ready for the day watch, I saw some whales off the port (left side facing forward on a ship). That was just the beginning. As we headed due west on the Newport transect line (44 39.1′ N latitude) we spotted brownish and reddish jelly fish, albatross following along the starboard side during bongo tows, sea lions skirting by the stern, and a shark fiddling with driftwood presumably looking for small fish that were utilizing the log as a habitat. Later in the day, we navigated near breaching humpback whales on the starboard side. Towards evening, a group of 5-6 pacific white-sided dolphins followed along for 10 minutes or so.

A Doliolid, which feeds on plankton, was caught in the vertical net before being released into the ocean. Note the pinkish lines, the muscle bands, and blimp-like shape.
A Doliolid, which feeds on plankton, was caught in the vertical net before being released into the ocean. Note the pinkish lines, the muscle bands, and blimp-like shape.

Being out here witnessing the wildlife in their environment is fascinating.  You start to internalize the ocean planet as more than a vast emptiness.  There exists a tremendous amount of species diversity living above and below the surface. Yet sadly, since few of us spend regular time away from our land habitats, we tend to neglect the essential nature of the ocean.  The ocean truly sustains us, whether providing the majority of our freshwater (through evaporation and, consequently, rain), supporting our nutritional diets, and driving the weather we experience daily.  Teacher at Sea really reinforces this revelation since I get to spend an extended amount of time away from my terrestrial existence learning to appreciate the ocean’s influence on our lives.  May we gain enough understanding to ensure the sustainability of the ocean ecosystem.

Animals Seen 

Humpback whales
Shark
Jellyfish
Doliolid
Albatross
Albacore tuna
Sea lion
Pacific white-sided dolphin

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Ruth Meadows, July 11, 2009

NOAA Teacher at Sea
Ruth S. Meadows
Onboard NOAA Ship Henry B. Bigelow 
June 12 – July 18, 2009 

Mission: Census of Marine Life (MAR-Eco)
Geographical Area: Mid- Atlantic Ridge; Charlie- Gibbs Fracture Zone
Date: July 11, 2009

Waiting to see what animals we can spot off the bow
Waiting to see what animals we can spot off the bow

Weather Data from the Bridge 
Temperature 18o C
Humidity 61%
Wind speed 4.2 knots

Science and Technology Log 

Today is our last day at sea and the weather is certainly cooperating with us. We have beautiful blue skies, warm temperatures and calm waters.  It is a perfect day for observing marine life.  Several of us spent most of the day on the bow of the ship looking for any type of marine life.  Throughout the day, we spotted three Mola mola fish, which is a very large ocean sunfish that can be found in temperate oceans.

A humpback whale breaches the water off the bow of the Bigelow.
A humpback whale breaches off the bow.

One went right by the ship so we were able to see the entire body of this fish through the water.  Another one was just lying on its side but we were too far away to see it very well. Finally it was suppertime and we all went to the galley eat, somewhat disappointed that we had not seen more sea life. During supper, the call we had all been hoping to hear came, “Humpback whale off the bow.”  We all left the galley and quickly ran up to the deck afraid we would miss seeing this majestic creature.  We were in for a treat.  It was as if the whale knew we were watching and performed for us.  For over 40 minutes, the humpback whale slapped its pectoral fins, slapped its tail and even breached out of the water twice.  It was an amazing sight.

The fluke of the humpback
The fluke of the humpback

As the whale slowly swam around, the ship carefully followed at a safe distance giving us an amazing opportunity to observe this massive mammal in its natural habitat. At one point, the whale was floating on its back and slapping both of its pectoral fins in the water at the same time.  We were close enough to actually hear the sound of the fins hitting the water.  Many members of the ship’s crew came to the bow to watch also. While we were watching, the chief engineer standing next to me looked down at the water next to the ship in time to point out a Mako shark swimming just below the surface moving slowly toward the rear of the ship. The afternoon turned into an amazing good bye present to the entire crew of the Bigelow. After the humpback whale made its final dive deep into the ocean, many of us stayed outside to enjoy our last sunset over the Atlantic Ocean.

Personal Log 

The past four weeks on board the NOAA ship, Henry B. Bigelow, have been an amazing experience for me.  We traveled over 5,000 nautical miles to search for rare and unusual animals that live in the deep ocean along the Charlie-Gibbs Fracture Zone in the Mid-Atlantic Ridge.  I was truly fortunate to have been selected for this particular scientific cruise.  The scientific crew, NOAA corps and crew were second to none. Everyone worked around the clock to make sure the goals of the cruise were accomplished.  In addition to the professionalism of all the members of this cruise, everyone seemed to truly enjoy working together to complete all parts of the mission. Everyone, from the captain of the ship, the engineers, the deck hands, the cooks and the scientific crew, made me feel welcome and included in all the activities on board. I will take many things with me from this opportunity I was lucky enough to be selected for.

A beautiful sunset on the Atlantic
A beautiful sunset on the Atlantic

I knew I would learn a lot about the ocean and the organisms that live there.  What I didn’t know before I left was how much I would enjoy getting to know the people that were a part of the MAR-ECO cruise. Thank you for allowing me to be a small part of this wonderful experience.

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Susan Smith, June 7, 2009

NOAA Teacher at Sea
Susan Smith
Onboard NOAA Ship Rainier
June 1-12, 2009 

Mission: Hydrographic survey
Geographical area of cruise: Trocadero Bay, Alaska; 55°20.990’ N, 33°00.677’ W
Date: June 7, 2009

Sending the CTD to the bottom
Sending the CTD to the bottom

Weather Data from the Bridge 
Temperature: Dry Bulb 12.8° C (55°F)
Wet Bulb 11.7°C (53°F)
Cloudcover: Overcast 8/8
Visibility: 4 nautical miles
Wind: VRB, light speed
Sea Wave Height: 0-1
Sea water temperature: 9.4°C (49°F)

Science and Technology Log 

Today we left Craig to finish our grids in Trocadero Bay, Alaska. It was a time to clean up or capture data from isolated locations which had either been missed or not completely surveyed. For the first few hours we spent our time surveying areas very close to the shoreline and areas very difficult in which to maneuver.

Bringing the CTD back up
Bringing the CTD back up

We did our first cast with the CTD (Conductivity, Temperature, Depth) equipment and I finally asked if I could run it. Ian, the survey technician, happily obliged. The CTD calculates speed of sound through water. I have finally gotten the gist of sonar settings. The following information will help you understand why it is all necessary for getting accurate data to the surveyor and coxswain. 

Range- How long it takes for the sonar beam to go to the bottom and return, or in layman’s terms, tells the sonar when to ping and listen.

Pulse length– Pulse length sets how long the sonar transmits, thus allowing more power to be put out bythe sonar, but it results in decreased resolution. The longer the length of the pulse the lower the resolution, so shorter is optimal. For instance, when going through kelp it should be set at low so the kelp isn’t all being picked up by the sonar beam.

I really enjoyed driving the launch today.
I really enjoyed driving the launch today.

Sonar Beams- There are 512 beams at high frequency (400khz). Low frequency (200 khz) equals 256 beams.  There are two yellow gates on the screen which  surveyors utilize. One is positioned above the shallow water, one is positioned beneath the deepest water measurement. When in shallow water most surveyors disable them. When in deep water, if the top gate is positioned too low, you lose valuable data on the outer limits. If the lower gate is positioned too low it records too much noise. However, if it is set too high the outer beams are missing and no data is recorded. Surveyors must constantly watch this screen when these gates are active to ensure all data they want is being captured.

The airplane indicates the launch position and the color is the area which has been logged.
The airplane indicates the launch position and the color is the area which has been logged.

The surveyor must ensure the data is placed in appropriate folders, enter data in spreadsheets, and basically keep things running smoothly for the entire time data is being logged. So, in essence the surveyor must watch the sonar screen, set the polygons on the screen for him/herself and the coxswain, continually check the settings, remember to log on for data retrieval  and log off when the swath is completed, set the CTD for casts every four hours, and monitor as many as ten folders at one time.

The rule of safety: Never shall safety for life or property be compromised for data acquisition.
The rule of safety: Never shall safety for life or property be compromised for data acquisition.

The coxswain’s job is to drive the launch into areas to be charted, based on the POD, the Plan of the Day, grids. When data is being recorded he/she drives approximately four to eight knots, depending on the wave action. High swells require slower forward progress. The coxswain has two computer screens-one showing the grid being logged or charted, and another displays depth of water in feet, meters, and fathoms and several other pertinent pieces of data. He or she is ultimately responsible for making decisions about when to enter dicey locations and determining when to stay out of a risky situation.

Seals swimming in kelp
Seals swimming in kelp

When traveling in either extremely shallow water or water full of kelp and known rocky locations, a bow watch will stand on the bow and give visuals for the coxswain to avoid. Obviously, this person must wear a safety jacket and hold a rope around an arm or wrist, due to the precarious position he or she is in. High swells could cause serious accidents in a second.

Did you know when backing up a launch, sonar cannot penetrate the bubbles formed when the water is getting stirred? The readings inside the launch show the color red, or dangerous zones, because the sonar thinks the boat is at the bottom. As the surveyors and coxswains say, “No worries! We know where we are.”

Question of the day: What is a patch test and why is it run?

Humpback whale photo courtesy of Ian Colvert
Humpback whale photo courtesy of Ian Colvert

Personal Log

Now that I felt much more comfortable with understanding the sonar I was able to relax more on the launch today. Perfect timing, as this was such a great day for biological observations. Five different humpback whales were sighted in the bay with us; in one location two were in position as forward observers on either side of our launch. The last whale we spotted surfaced fairly close to our launch so we had to stop, mainly because the regulations state you must stay 100 yards from humpback whales. This whale went under the launch and surfaced about 50 meters from us. Off and on during the day they would surface in the areas we were surveying so we had to just wait until they moved along.

I also observed at least eight bald eagles either sitting in trees, flying over the water, or harassing the whales. One eagle flew down close to the water and looked as though it was taunting the whale! Then it quickly flew back up to a tree top and perched on a branch. Several eagles would fly off together, separate, then come back together before landing on a tree. Early in the morning we ran into a group of seals swimming around in kelp. They poked their heads out and just stared at us as we drove by. Luckily we saw them in time to slow down, so as to not disturb them anymore than necessary.