NOAA Teacher at Sea
Brett Hoyt
Onboard NOAA Ship Ronald H. Brown October 8 – 28, 2006
Mission: Recovery and maintenance of buoy moorings Geographical Area: Southeast Pacific, off the coast of Chile Date: October 22, 2006
Jeff Lord using an acoustic transmitter to talk to the acoustic release. This machine also tells the scientists the range to the release that helps them in finding it.
Data from Bridge
Visibility: 12nm (nautical miles)
Wind direction: 130º
Wind speed: 19 knots
Sea wave height: 4-6ft
Swell wave height: 5-7 ft
Sea level pressure: 1019.7 millibars
Sea temperature: 17.3ºC or 63ºF
Air temperature: 18.0ºC or 64ºF
Cloud type: cumulus, stratocumulus, and stratus
Note:
All day on the 21st was spent traveling to the Chilean tsunami buoy approximately 300 miles off the coast of Chile. During this time, the Woods Hole group was busy retrieving data from their instruments from Stratus 6. Many of the instruments collect data all year long and store it on flash memory cards. When recovered one year later, this data is then downloaded onto computers for later analysis. We arrived late in the day on October 22 at the tsunami site and immediately started the process of recovering the old buoy. As you can see, scientists work day and night to get the job done. I really have never seen a group of harder working people.
Jorge Araya and Alvaro Vera, members of the Chilean Navy, looking for the yellow glass balls which were released over an hour ago and take that long to reach the surface. Work vests were required but not hard hats for this part of the operation. Both have over 12 years with the Chilean Navy.
The Machine
The glass balls are attached to the Bottom Pressure Recorder, or BPR, and float to the surface leaving the anchor on the bottom of the ocean.
Jorge Gaete, a civilian contractor for the Chilean Navy for the past 2 years, helps with the deployment of the tsunami buoy.Capturing the yellow flotation balls that have brought the BPR to the surface for recovery.
The second part of the tsunami warning system is the recovery of the buoy. This buoy receives the signal from the BPR and quickly transmits the warning via satellite to the Chilean authorities who in turn warn the public. This recovery was done at night. Without the vast array of sensors found on the Stratus 7 buoy, this recovery progressed quickly and was completed within 30 minutes.
Hooking lines to the tsunami buoy for a quick recovery.
The Experiment
There is no experiment today; however, I will try to explain how the system works. When a tsunami is triggered by an underwater earthquake the BPR detects the increase in pressure on the bottom of the ocean due to the increase in the height of the water column above the sensor. When I asked Alvaro how this worked when sea swell was 6-7 ft at times and waves could reach a height of 45ft he explained that the pressure is sharp and abrupt. This is indicated by a very short wave (period) of energy passing through the open ocean. In open ocean the height of a huge tsunami wave is so short a ship would hardly know one has passed by. It is only when this wave heads into shallow water that the wave becomes deadly.
The BPR immediately after recovery, without its anchor that remains on the bottom of the ocean.
Classroom Activities
Please share with your students the DART tsunami warning system.
My next log will cover the deployment of a new warning system.
NOAA Teacher at Sea
Brett Hoyt
Onboard NOAA Ship Ronald H. Brown October 8 – 28, 2006
Mission: Recovery and maintenance of buoy moorings Geographical Area: Southeast Pacific, off the coast of Chile Date: October 19, 2006
Dan Wolfe, senior scientist at NOAA, at his workstation on board
Weather from Bridge
Visibility: 12nm(nautical miles)
Wind direction: 130º
Wind speed: 20 knots
Sea wave height: 5-7ft
Swell wave height: 3-4 ft
Sea level pressure: 1020.4 millibars
Sea temperature: 19.4ºC or 66 ºF
Air temperature: 19.2ºC or 66ºF
Cloud type: cumulus, stratocumulus
The Scientists
Today we will be interviewing Dan Wolfe, a senior meteorologist for the National Oceanic and Atmospheric Administration—NOAA for short. Standing an imposing 6’3”, it seemed only fitting that our next scientist should be studying the heavens. Mr. Wolfe is a 30-year veteran of NOAA and has been a scientist for the past 31 years. Mr. Wolfe entered the Coast Guard in 1969 immediately after graduating high school. He was initially assigned to the Coast Guard icebreaker “Glacier” transferring to the oceanographic unit where he staged scientific experiments. He traveled to the Arctic and it was there that he discovered his soon to be life long passion for the atmosphere and all that is in it. Mr. Wolfe was a trained scuba diver while stationed on the Glacier. After leaving the Coast Guard he attended Metropolitan State College where he earned his degree in meteorology. He has the distinction of being the first student to graduate in meteorology at this college. It was while at Metropolitan College that Mr. Wolfe became a coop student working for NOAA. After earning his degree he went to work for NOAA as a meteorologist where for the next 30 years he has become one if its leading atmospheric scientists. After seven years on the job he decided that he wanted to know more and enrolled at Colorado State University where he earned his masters degree.
This is a radiosonde, which measures relative humidity, temperature, barometric pressure, and winds as it passes through the atmosphere and radios its data back
Mr. Wolfe is one of the few individuals who has worked in BOTH the Arctic (North) and the Antarctic (South) (not just Antarctica but actually at the South Pole). His work has taken him to the depths of the Grand Canyon and to the Arctic more times than he cares to remember.
One of his more exciting job assignments with NOAA is managing a 1,000-ft research tower just off of I25 north of Denver Co. When I asked Mr. Wolfe what message he would like to give to upcoming scientists he replied, “Kids should seek out paid/or unpaid internships while in high school. Look for internships within your community in careers that you think you might like. This gives you the opportunity to try a job before investing money and time in college in a future you may not enjoy. If you try a job and discover you don’t like it, try something else until you find something you do like. Be sure to give the job a chance though.”
NOAA Teacher at Sea, Mr. Hoyt, releasing a radiosonde
The Machine
One important scientific instrument used by a meteorologist is the radiosonde (pronounced radio sond). This device measures relative humidity, temperature, barometric pressure, and winds by utilizing the global positioning satellite system. The radiosonde is battery activated then secured to a large helium balloon. It is then released where it begins its ascent into the upper atmosphere, measuring humidity, temperature, and pressure sending these data back to the scientist via a digital radio frequency. Depending on the balloon used, these radiosondes can obtain heights in excess of 6 miles. The atmospheric data collected on this cruise will be shared with other scientists to help improve global weather computer models.
The Experiment
There is no experiment as these data are transmitted via satellite link immediately after the flight is finished to the National Center for Environmental Prediction to be fed into their continuously running forecast models.
Classroom Activities
Elememtary K-6:
Ask the students, “What is weather?” “Why is it important to predict the weather?” Have the students take a piece of drawing paper and divide it into four equal parts. In each part have the students draw and color four different types of weather common to where they live. Example could be sunny, rainy, partly cloudy, and snow.
Middle School:
Why do we use calibrated thermometers to measure air temperature? Ask students to answer on paper whether the classroom is hot, warm, cool, or cold and to estimate the actual temperature of the room. Then compare the students’ answers to the actual temperature. Then discuss the importance of a “standard.” Without this “standard” scientists around the world would have no way of communicating what the atmosphere is doing.
Please examine the High School for more activities
High School:
Everyday we hear on the radio, television, or newspaper that it will be sunny, partly cloudy, partly sunny, etc. How do meteorologist arrive at this? Today we will learn how.
Divide the sky into eight parts. Examine each part and count how many squares have clouds. There is no hard and fast rule on what to do with partially filled boxes
No squares having clouds-Clear or Sunny
One to two squares having clouds-Mostly Clear or Mostly Sunny
Three or four squares having clouds-Partly Cloudy or Partly Sunny
Five, Six, or Seven squares having clouds-Mostly Cloudy
Eight squares having clouds-Overcast or Cloudy Take the sky photo below and print it out. Draw a grid like the one above on top of the sky photo. Have the students write down what they think the day is. Then compare the student’s answers. Is this an exact science?
Have your teacher take photos of the weather in your area and do your own.
NOAA Teacher at Sea
Brett Hoyt
Onboard NOAA Ship Ronald H. Brown October 8 – 28, 2006
Mission: Recovery and maintenance of buoy moorings Geographical Area: Southeast Pacific, off the coast of Chile Date: October 18, 2006
Weather Data from Bridge October 18
Visibility: 12nm(nautical miles)
Wind direction: 120º
True Wind speed: 10 knots
Sea wave height: 2-4ft
Swell wave height: 3-5 ft
Sea level pressure: 1021.6 millibars
Sea temperature: 19.3ºC or 67ºF
Air temperature: 22.5ºC or 72ºF
Cloud type: cumulus, stratocumulus
We are going to use a different format for today because it is recovery day!
On October 16th we deployed the Stratus 7 buoy. The second part of this cruise is the recovery of the Stratus 6 buoy that was deployed approximately one year ago. To ensure a continuous record, a new buoy is installed at the same time the old one is recovered. Today, October 18th, is the recovery of the Stratus 6 buoy. Please compare and contrast the photos of October 16th (Deployment) with that of October 18th (Recovery).
The Stratus 6 Buoy one year after it was deployed. The nearest Land is 600 miles to the east. These birds are feeding off the marine life this buoy collects in the waters around the mooring.Recovering of the Stratus 6. Can you spot the Scotsman? Hint: He’s the one in the cowboy hard hat.Instruments waiting deployment for Stratus 7.Stratus 6 instruments one year after deployment covered in barnacles. What would two years of deployment look like?Gooseneck barnacles from the Stratus 6 buoy.Damage to a current meter caused by fisherman’s gear. Of the 8 meters, 6 were fouled. Here we have entanglement of the current metering fans by fishermen’s lights. They use these lights on their lines to attract fish to their hooks at night. Once the entanglement occurs data cannot continue to be gathered.NOAA Teacher at Sea, Mr. Hoyt, scraping barnacles off one of the sensors from Stratus 6. “ I’ve got to talk to my travel agent.”Remember the glass balls from Stratus 7? Here are the glass balls from Stratus 6. It took them over one hour to reach the surface after the acoustic release was activated. They are not in the nice neat line as we had in deployment.Anyone like puzzles?The acoustic release, one year after being sent 13,000 ft to the bottom of the ocean. Scientists sent a signal to this release to let go of one side of the chain. Should one release fail, they could trigger the other release.Dr. Weller, leading by example, cleaning the equipment free of barnacles. Remember in an earlier posting when he stated he was a “hands on scientist”?
NOAA Teacher at Sea
Brett Hoyt
Onboard NOAA Ship Ronald H. Brown October 8 – 28, 2006
Mission: Recovery and maintenance of buoy moorings Geographical Area: Southeast Pacific, off the coast of Chile Date: October 16, 2006
Weather Data from Bridge
Visibility: 12nm (nautical miles)
Wind direction: 060º
Wind speed: 10 knots
Sea wave height: 3-4ft
Swell wave height: 5-6 ft
Sea level pressure: 1020.8 millibars
Sea temperature: 19.3ºC or 66ºF
Air temperature: 19.1ºC or 66ºF
Cloud type: cumulus, stratocumulus
We are going to use a different format for today because it is Deployment Day! Today was deployment day for the entire crew and the best way to tell this story is in pictures. So let’s begin.
Before scientists deploy a buoy they must measure how deep the ocean is. This is the actual bathymetric (bottom measure) read out of the target site for Stratus 7.This is the map of the bottom of the ocean. Please note the scale in meters on the left as well as + marks the spot. Can you see the pattern the boat is making?With over 4,400 m (13,000 ft) of cable it takes a full crew to stage the cable.Jeff Lord making final preparations for the dozens of instruments to be deployed beneath the buoy. What an amazing man. “What would we do without you?”Lifting the Stratus 7 Buoy off the ship. This process takes the cooperation of about a dozen individuals to do.Stratus 7 off the side ready to have the instruments deployed under it.Jeff attaching a current meter (Invented and patented by Dr. Weller) to the bottom of the buoy. It weights about 160lb and there are eight of them. Please note the safety equipment Jeff is wearing. SAFETY FIRST!Dr. Weller operating the winch (it has over 2.5 miles of cable on it!) and supervising the deployment operation.Attaching glass balls (they are located inside the yellow plastic housings which protect them from chipping), which are at the very end of the 13,000 feet of cable just above the acoustic release, which in turn attaches to the anchor. These hollow glass balls can withstand pressures in excess of 5,300 lb/sqin.This is the acoustic release (actually two) that attaches the buoy mooring line to the anchor. One year from now an acoustic signal will be sent down 13,000ft to trigger the chain to be released. The reason they use two is that if one fails the release will still take place and the mooring line will begin its ascent to the surface with the help of the glass balls.Everything is just moments before release. This anchor weighs 9,000lbs and will take over 45 minutes to fall to the bottom of the ocean. All the instruments are attached, glass balls secured, and the acoustic release in place. Drum roll please…………………. The anchor is deployed!Stratus 7 on station in the South Pacific Ocean helping scientist understand this big blue planet we call home.
NOAA Teacher at Sea
Brett Hoyt
Onboard NOAA Ship Ronald H. Brown October 8 – 28, 2006
Mission: Recovery and maintenance of buoy moorings Geographical Area: Southeast Pacific, off the coast of Chile Date: October 15, 2006
Dr. Robert Weller sitting on the aft deck
Weather Data from Bridge
Visibility: 12nm(nautical miles)
Wind direction: 110º
Wind speed: 11 knots
Sea wave height: 2-3 ft
Swell wave height: 3-5 ft
Sea level pressure: 1016.8 millibars
Sea temperature: 18.6ºC or 65 ºF
Air temperature: 18.2ºC or 64ºF
Cloud type: cumulus, stratocumulus
The Scientists
Today we will visit with Dr. Robert (Bob) Weller. Dr. Weller is the lead scientist for this scientific cruise and upon whose shoulders the success or failure of this expedition rests. Dr. Weller is an easy going, soft-spoken, easy to approach, modest, and very intense man with a passion for understanding the climate of the earth and all the processes within it. Many times scientist possess a great mind for academic excellence yet they fail at relating to people. Dr. Weller is the exception, possessing a brilliant mind, keen insight and intuition, and superb people management skills. It is exactly these qualities that have enabled him to lead such important and ground breaking research on climate and climate studies He understands that the success of a cruise depends on getting people (sometimes of various nationalities, on our cruise five) to work together to accomplish great things.
The Stratus 7 Buoy on station in the South Pacific just after being deployed
Dr. Weller began at an early age to feel the pull of science. He entered college initially to be a biochemist but something happened. In the middle of college he accepted a job with an oceanographer and from that time on he knew that a new career was in order. He graduated in 1972 with a degree in engineering and applied physics. He continued on and five years later in 1978 earned his doctoral degree in oceanography.
Upon earning his doctoral degree he accepted a position working at the prestigious Woods Hole Oceanographic Institution. He has been there ever since. How many people do you know who have stayed at the same job for 28 years! Dr. Weller finds himself at sea 2-3 months out of the year. He is a self-described scientist who likes to do things “hand on” (he’s not afraid to get dirty–please see the photo of him on deck and in his hard hat). When I asked him how long he has been a lead scientist he modestly replied” I don’t know if I’m there yet.” When I asked him what one message he would like to send to you future scientists he stated “ Kids and future scientists should be less concerned about outer space and more concerned about the planet we currently live on”. He wants kids to think about the things you can do about the temperature of the oceans and the role they play in the wellbeing of our planet we call home.
The anchor for the buoy
The Machine
Today we will examine the reason we all went to sea, the Stratus 7 Buoy. This buoy sends real time data from a fixed location off the coast of Chile. The buoy system maintained by the Woods Hole Oceanographic Institution (WHOI) out of Woods Hole Massachusetts plays an extremely critical role in understanding weather patterns that have worldwide implications. These buoys are highly sophisticated weather and climate data-gathering stations. The data collected from these stations is used to check the accuracy of powerful computer simulations that are used to predict climate change.
The Stratus 7 buoy replaces the aging Stratus 6 buoy that has been on station for over a year. There has been a Stratus buoy in this location since 2000. Dr. Weller stated that in years past buoys would not be on station for years at a time but rather for days at a time. Most did not exceed 40 days. Through trial and error, research and innovation, the life at sea for a buoy has been extended into the years. Concerned about waste and pollution in the oceans, most buoys are serviced, refitted, and given a new life year after year. Some might wonder about the cost, sometimes in excess of $1million dollars, of the buoy programs. The economic payoff is immense. It is buoys like these and the data that they collect that help scientists predict the absence or presence of El Nino. This has a huge and direct agricultural impact upon coastal states and to a lesser degree states far removed from the oceans. Do you have droughts or floods out of the norm in your area? The cause could be ocean related.
Hundreds of pounds of chain!
The Stratus Buoy can make the following measurements: -precipitation -wind speed and direction -air temperature -relative humidity -barometric air pressure -long wave radiation (radiation given off by a hot body) -short wave radiation (incoming energy from the sun) -sea surface temperature. The buoy not only transmits this data real time but also stores much more detailed information on flash cards. These cards are collected and taken back to the laboratory for further study. In addition to all the above surface instrumentation there is over 5,000 lbs of sub surface measuring instruments. These include current velocity, salinity, and temperature. These instruments are located at various depths down to 2,500ft. For example there will be 8 current velocity-measuring instruments at 8 different depths.
Cool facts
-You probably wonder how this million-dollar instrument is powered. Wind, solar, high powered lithium batteries, nope none of the above. It is powered by 1,650 D cell alkaline batteries. Exactly the ones you would use in a flashlight in your house.
-The mooring line (the line connected to the anchor) will be over 12,000 feet long
-The anchor is a cast iron weight that weighs over 9,000 pounds. -This anchor will take over 45 minutes to make it’s journey to the bottom of the ocean
-The buoy will have over 5,000lbs of instruments hanging from the bottom of it
The Experiment
There is no direct experiment with the stratus buoy. The data collected by it is used by scientists world wide to generate new ideas, hypothesis, and conclusions. As stated earlier this data is used to help climatologists improve computer models and check them for accuracy.
Dozens of instruments to be deployed directly beneath the buoy 800 meters worth that’s over 2,400 feet of instruments!
Classroom Activities
Elememtary K-6: Items needed- Styrofoam cup or similar floating device, small piece of string and a metal washer some rubber cement or other flexible glue, some round toothpicks and a large tub of water. Have the students decorate their cup using markers, plastic straws, aluminum foil, or anything else that the kids might think would make their buoy look scientific. Put the string through the bottom of the cup making as small as hole as possible (the point of a compass or the toothpicks work well) tie the string to a toothpick on the inside of the cup and let the toothpick rest on the bottom inside the cup. Place a small dab of glue on both the inside and outside of the string to keep the water from entering the cup. With the string dangling from the bottom outside of the cup tie on the washer or other object for weight. Ask the kids what scientific information their buoy collects.
Middle School:
Items needed- volt-ohm meter, glass beaker, two small copper wires, 500ml of distilled water, and some common table salt.
Salinity of the oceans seawater is of concern to scientists and is one of the tests conducted by the Stratus 7 Buoy. The way scientists test for salinity is called a conductivity test. That is they measure the conductivity of seawater. Have the student pour 250ml of distilled water into a glass beaker. Place two small copper wires on opposite sides of the beaker and submerged in the water. Be sure that at least 1cm of wire is exposed copper and in the water. Set the voltmeter to ohms and get a reading and record it. Add .5 grams of salt and mix well. Test the conductivity again. Keep adding salt in .5-gram increments. Does the readings change? If so how? Are the numbers getting larger or smaller? If so why?
High School:
Items needed- volt-ohm meter, glass beaker, two small copper wires, 250ml of distilled water, and some common table salt, and sugar.
Salinity of the oceans seawater is of concern to scientists and is one of the testes conducted by the Stratus 7 Buoy. The way scientist test for salinity is called a conductivity test. That is they measure the conductivity of seawater. Have the student pour 250ml of distilled water into a glass beaker. Place two small copper wires on opposite sides of the beaker and submerged in the water. Set the voltmeter to ohms and get a reading and record it. Add .5 grams of salt and mix well. Test the conductivity again. Keep adding salt in .5-gram increments. Does the readings change? If so how? Are the numbers getting larger or smaller? If so why?
Now run the test with sugar. What are your results? Was there a change? Now change the temperature of the solution by heating or chilling with ice. Does this make a difference in your readings?
Lead a class discussion on what each instrument of the stratus buoy does and why it is important to scientists.
