Daily Logs
Week 6
Tuesday, October 9, 2001
Wednesday, October 10, 2001
Thursday, October 11, 2001
Friday, October 12, 2001
Saturday, October 13, 2001
Date: Tuesday, October 9, 2001
Photos: Bruce
Cowden, the Chief Bosun
Latitude: 1o S
Longitude: 92o W
Temperature: 84o F
Seas: Calm in port
Science Log: There is a flurry of activity getting ready
for departure. The crew is very focused checking that everything
(and I mean everything!) is strapped down tightly. Then the authorities
come on board to check passports and do an inspection. If all
is in order we will be on our way shortly.
Photos: Any job that requires moving things around on
the deck is overseen by Bruce Cowden, the Chief Bosun. In the
first photo you can see Bruce hoisting the gangway, and in the
second he is leaning overboard to watch the lifting of the anchor.
Travel Log: We are now underway! The gangplank has been
raised, the anchor (all 270 meters of it) is lifted and the ship
is moving out to sea. Most everyone is standing on the decks outside
taking their last photos of these fabulous islands. Goodbye Galapagos!
Goodbye to Lonesome George (a huge turtle that is the last of
his kind) and all the other gentle giants. Goodbye to all the
beautiful herons, frigates, and blue-footed boobies! And finally,
goodbye to all the friendly inhabitants of these islands that
are working to preserve them for the future.
Keep in touch,
Jane
Date:Wednesday, October 10, 2001
Photos: Buoy
repair
Latitude: 1o S
Longitude: 95o W
Air Temp: 22.5 o C
Sea Temp: 19o C
Sea Wave: 0 - 1 ft.
Swell Wave: 3 - 4 ft.
Visibility: 8 miles
Cloud cover: 6/8
Science Log: Everyone was working in full swing today.
Weather balloons being released, water samples being collected,
data from every possible source was being analyzed. The big event
of the day though, was coming upon the first buoy. A buoy is relatively
small, about the size of a small monkey bar set - just big enough
for one or two people to climb onto. It has a long rope with an
anchor attached at the bottom so it is supposed to stay put. But
many times the currents and winds are too strong and it drifts
a bit, making it hard to find in the big ocean. Fortunately, it
has a sensor on it that helps the ship locate it. This buoy was
placed out here last year. It is full of sensors that store information
like temperature and salinity (how much salt is in the water)
and winds. Using that information, scientists can chart even the
smallest changes over long periods of time. Unfortunately this
buoy was damaged a while ago and stopped transmitting. Perhaps
a ship ran into it or maybe a shark took a bite out it. Today
2 scientists went out in a small boat (see
photos) and climbed aboard the buoy and repaired it. Lucky
for them, the seas were very calm, but even so, it is very dangerous
work. They found the buoy quite damaged probably from a collision
with a ship. The buoy was fixed and is now transmitting again.
Travel Log: Repairing the buoy took about 2 hours. During
that time some of the crew enjoyed fishing off the back of the
boat. As Jennifer mentioned in her logs, the bottom of the buoy
and the rope that leads down to the anchor act as a special habitat
for sea life. Barnacles and mussels attach themselves to the rope
and then small fish come to feed on them, The food chain grows
quite large so that in a year's time many big fish, including
sharks, can often be seen by a buoy. Today one of the crew caught
a 25 pound mahi which was deliciously grilled up for dinner.
Today we also had our first emergency drills. Each person on
board is responsible for knowing what to do, where to go, and
what to bring for each of the three types of emergencies. The
first is your basic fire drill. But since you can't get off the
ship easily, you have to know where to go to be safe. The second
one is the "abandon ship" drill. This one is tough because
each person must get to her room, put on a life vest, and carry
a large orange duffle bag with your "gumby" suit in
it down to a lifeboat. A gumby suit is a big bulky rubbery suit
that will keep you warm and dry if you have to go into the water.
You put it on right over your clothes and it's really tough to
do. I was told that it will be even be harder to do in the middle
of a dark and cold night! The last drill is the "man overboard"
alarm. What do you do if you were to see someone fall off the
ship? Three things: keep your eye on him, throw something in the
water that will float like a life ring, and yell for help. Safety
is a big concern when you are on a ship.
Question of the Day: How does the ship get fresh water
for its passengers?
Keep in touch,
Jane
Date: Thursday, October 11, 2001
Photos: Dr.
Uttal and the ETL Lab
Latitude: 4o S
Longitude: 95o W
Air Temp: 21.0 o C
Sea Temp: 19.0o C
Sea Wave: 1 - 2 ft.
Swell Wave: 3 - 4 ft.
Visibility: 10 miles
Cloud cover: 8/8
Science Log: Clouds
Today I met with meteorologist Dr, Taneil Uttal from ETL (Environmental
Technology Lab) in Boulder, Colorado. She is head of a group that
has done cloud studies in the Arctic. On this trip one of the
things Dr. Uttal wants to determine is how similar marine clouds
are to Artic clouds. To do this she and her associate Duane Hazen
use radiometers and radar which are all packed into a trailer.
The whole trailer is on the deck of the Ron Brown. Think of the
trailer as a big package of instruments. Duayne's job is to keep
the machinery running. In the photo you can see the radar antennae
on top of the trailer. It is there to measure the lectromagnetic
radiation at a certain frequency.
Here is how Dr. Uttal explains what's going on:
What is a cloud?
________________
A cloud is gazillions of tiny water droplets or ice crystals
floating
together up in the sky. Some clouds make rain and snow. Some clouds
do not. In EPIC we are looking at both kinds of clouds.
What is a Radiometer?
_____________________
Think of a pokemon which has a special power that no other pokemon
has. There are many things in the world around us that are just
like
that. For instance tiny droplets of water floating in the air
are
beaming certain energies that only water droplets have. If we
know
what the water droplet energy is like (and we do!), we can measure
it
and find out how much water there is in a cloud. A radiometer
is a
special instrument that we have here on the Ron Brown for measuring
the
special energy of a water droplet so we always know how much water
is
in the clouds over the ship. The energy of a water droplet can
be
named by how fast it is. A water droplet has three energies, 20
GHz,
32 GHz and 90 GHz. A GHz is 1,000,000,000 cycles per second.
What is a radar?
_________________
A radar is different from a radiometer because instead of looking
for
natural energy from something like a water droplet, it beams out
it's
own energy, bounces it off of things in the sky (like water droplets
in
a cloud), and measures the reflected energy. By looking at the
reflected energy, the radar can tell you things about a cloud
that are
different then what the radiometer tells you. It can tell you
about
how high a cloud is, how big the droplets are, and how fast the
droplets
are falling. The radar energy is 35 GHz.
What do you get when you look up with a radar and a radiometer?
_______________________________________________________________
When you put the data from a radar and radiometer together, you
can
figure out even more things, like how many cloud droplets there
are,
where the water is located in the cloud, and get an even better
guess of how
big the droplets are.
What does all this information tell you?
________________________________________
Right now people do not know very much about how clouds reflect
sunlight from the sun, reflect warmth that is coming up from the
earth, and change things like the temperature on the surface where
we live. These things will change depending all the cloud height,
how much water it has, how big the droplets are, and how fast
they are falling. In EPIC, we want to know which kinds of clouds
might make the ocean warmer, and which might make the ocean colder.
This can have a big effect on where fish and other ocean animals
might want to live and what kind of weather happens over the ocean.
Dr. Uttal is a scientist on board but she is also a mother and
wife back in Colorado. Taniel and her husband Rusty, have 2 children
- Kalvin, 6th grader at Baseline Middle School and Miranda, a
4th grader at Flatirons Elementary School.
Travel Log: Today I spent time on "the bridge"
of the ship. This is the area that controls all the functions
of the ship. The captain and his officers are responsible for
all that goes on, much like the principal of the school is in
charge. The best view can be had from the bridge and there are
video cameras that look out over all the decks. The highlight
was seeing a pod of porpoises swimming nearby. So graceful! I'm
going to keep my eye out for whales.
Question of the Day: What is the fastest creature living
in the sea?
Keep in touch,
Jane
Date: Friday, October 12, 2001
Photos: ARGO
float and Dr. Weller
Latitude: 7o S
Longitude: 95o W
Air Temp: 21.2 o C
Sea Temp: 21.1o C
Sea Wave: 3 -4 ft.
Swell Wave: 3 - 5 ft.
Visibility: 8 miles
Cloud cover: 8/8
Science Log: ARGO
An ARGO Float is a small (about 3 feet in length) black tubular
shaped instrument that measures temperature and salinity in the
water. It's interesting particularly because it is so simple.
The middle part of the instrument, called a bladder, is made of
a thick rubber material that can inflated like a balloon. It has
a pump inside that inflates or deflates the bladder which changes
its volume while keeping the mass the same. A deflated state has
an increased density which makes the ARGO sink to a depth of 900
meters below the surface. There it drifts for 10 days collecting
data. Then the bladder is inflated so the ARGO rises to the surface
and transmits its data to a satellite. When the transmission is
complete, it deflates again and begins the whole process anew.
This will go on for four years! As part of an international project
Dr. Weller, our Chief Scientist, and a group of scientists hope
to have 3000 of these in the water all over the world collecting
data. We will be deploying a total of 6 at the points marked on
the photo. The one you see in the photo was deployed at 2.5 o
S.
Travel Log: Pilot Whales - My first sighting of whales.
So beautiful and graceful. Not good for picture taking though
because they blend in so well with the ocean. The weather is fine
with a high cloud cover and light winds and no rain.
The crew says this is the calmest water they've been in all year!
Lucky me!
Question of the day: What would happen to an ordinary
styrofoam cup at at depth of 900 m.?
Keep in touch,
Jane
Date: Saturday, October 13, 2001
Photos: SPMR,
CTD, and Sea Bird
Latitude: 11o S
Longitude: 91o W
Air Temp: 19.7 o C
Sea Temp: 19.9o C
Sea Wave: 3-4 ft.
Swell Wave: 3 - 4 ft.
Visibility: 8 - 10 miles
Cloud cover: 3/8
Science Log: Energy from the Sun
The sun is the source of all energy on the Earth. The sun gives
us this energy in the form of light and heat. Where does all that
energy go? Why? How can it be measured? These are some of the
questions many of the scientists on board are asking.
Toby Westberry and Olga Polyakov are scientists that have 2 instruments
to help them understand how solar energy behaves in the ocean.
The first is the SPMR which is a tool used to measure how much
light penetrates the water. The more light = the more heat. You
can see in the photo that it is a small black device attached
to a long cord. Toby and Olga lower the SPMR over the side and
let it sink to 300 meters. Then they reel it back in just like
a fishing pole. It tells them the "color" (wavelength)
of the light at different depths. They do this over and over again
in different locations in the ocean. Why? We know that the ocean
water is not the same temperature in all places on the planet.
Can you think of why this might be?
Well Toby and Olga know that there are tiny living organisms
in the ocean that play a role in how warm or cool the temperature
is. They are called phytoplankton. It seems that the more phytoplankton
there is near the surface of the water, the more heat is trapped
there.
Here's an excellent explanation from Mrs. Richards of what's
happening that might help you to understand the process:
Imagine a nice clear swimming pool. The sun's heat energy can
penetrate all the way to the bottom of the pool because the water
is so clear. Whatever heat energy hits the pool will be dispersed
throughout the water somewhat evenly. Makes sense, right?
Now imagine that the pool has a layer of scum and algae at the
top. Face it, you just haven't done a very good job at cleaning
the pool, and your allowance just isn't big enough to make the
job worthwhile. Now, the sun's heat energy can't pass all the
way to the bottom of the pool because the scum is blocking the
light. The very top of the pool water is going to capture almost
all of the sun's heat energy, and the bottom layers of water will
be darker and colder. Imagine how the temperature of the water
will be affected by the amount of scum in the water.
Knowing how much phytoplankton is hanging around would certainly
help understand how the sun's energy is being used. For this experiment
they use a CTD. (Boy they sure use a lot of abbreviations for
things!) This instrument is really big and needs a big machine
called a winch to lift it in and out of the water. It has 12 tubes
that fill up with water, each at a different depth. When the CTD
is back on the ship, Toby and Olga fill labeled plastic bottles
with the water. Then their work begins. First they run all the
water samples through a filter to figure out how much phytoplankton
was in the sample. Remember each tube on the CTD took in water
at a different depth. So each bottle will tell a different story.
They use this information to create a data graph which is used
with other information to tell how the sun is heating the ocean.
Travel Log: Sea birds! I don't know how they do it or
where they came from but all of a sudden 5 "boobies"
showed up over the ship. What was amazing is that they hardly
ever flap their wings, yet they fly as fast a the ship. The ship
is moving forward at about 10 miles an hour and has big engines
to push it. These birds just seem to glide along over us. Beautiful!
Question of the day: What is an updraft and what causes
it?
Keep in touch,
Jane
Note for educators: Although Jennifer and Jane's reseearch cruise ended, the EPIC research continues. Please use this web site, Jennifer and Jane's lesson plans, daily logs, the videos, and the photos to educate your students about climate, El Niño, and scientific research in general. Consider this web site, as well as the TAO web site, a resource for teaching your students. Many organizations and countries are involved in funding the EPIC Experiment. Primary U. S. funding is provided by The National Science Foundation and The National Oceanic and Atmospheric Administration. This website is maintained and frequently updated by
NOAA's Office of Global Programs
ogpwebmaster@noaa.gov.
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