The Current Today
Objectives
Students will be able to:
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use real time data to locate the Gulf Stream
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Materials
copies for each group of the tracking chart
Full Basin
Western Atlantic
copies for each student of the
Blank Gulf Stream Map
computers with Internet access
colored pencils
Student Worksheets Pair 1,
Pair 2,
Pair 3
optional: printable Lab Report Directions
Background
The use of satellite imagery is one of the most accurate ways to locate the Gulf
Stream. NOAA (National Oceanic and Atmospheric Administration)
operates a Polar Orbiting Satellite (POES) with an AVHRR sensor (Advanced Very
High Resolution Radiometer). This sensor measures the amount of thermal
infrared radiation given off by the surface of the ocean. The amount of
thermal infrared radiation given off by an object is related to its temperature,
so by measuring the amount of radiation given off by the ocean, scientists can
calculate the temperature of the sea surface. The satellite thermal
infrared radiation data is color coded to produce an image of the ocean. The satellite image allows people to
easy locate the warm current of
water in the Atlantic Ocean known as the Gulf Stream by comparing the color
differences to a color/temperature scale. Sea surface height (radar
altimeter data), measured by the TOPEX/Poseidon and ERS-2 satellites also is
valuable information to help track down the location of the Gulf Stream.
The Radar Altimeter on ERS-2 sends radar signals to the earth and ocean surface
and collects the return signal. That information is processed to reveal
the ocean wave height and wind speed (over oceans), the surface backscatter, and
the height of the satellite above the surface. This provides the
possibility to monitor the global ocean circulation and regional current
systems.
The satellite systems offers the advantage of daily global coverage. Other means of
measuring sea surface temperature such as buoys (drifting and moored) are used
to maintain accuracy of the satellite data, further removing sources of error.
Oceanographers use the images to visualize the Gulf Stream; the width, the
number of rings and meanders, etc. Constant monitoring is necessary
because the Gulf Stream is not a stable current, it meanders North and South.
Sometimes these meanders are small, taking the form of waves which appear to
break backwards relative to the northeasterly flow of the current. In some
instances, the meanders become so large that a pocket of warm water is pinched
off and separates from the stream into the cooler shelf water. These are called
warm core rings. The warm core rings rotate clockwise for several days,
eventually drifting west to southwest until they interact with the shelf or the
Gulf Stream. Most warm core rings are reabsorbed into the stream after
wandering for 1 to 3 months. The effects of warm core rings were observed
by early oceanographers, but the true extent was not well understood until the
availability of satellite imagery. It is also interesting to note that
just as stream meanders to the North can pinch off a warm core ring, stream
meanders to the South can also pinch off, forming a cold core ring. These rings
are often less visible in the satellite imagery because of the warmer water
lying above, but can still be seen by the trained eye. (Northern
Gulf Stream Image June 11, 1997)
Procedure
1. Create working groups of 6 students. Break each group of six into
pairs.
Pair 1
2. Obtain the most recent data from the following buoys. Record the
following
information on the Student Worksheet: Latitude and Longitude, Time and Date,
Air
Temperature (ATMP), Water Temperature (WTMP). Scroll down the page to the Previous 24
observations. Plot the location of the 6
buoys on the chart.
Pair 2
3. Obtain the most recent ship data by clicking on the
Ships in the North Atlantic link below. The symbols on the chart
represent the ships and buoys currently logging data in the Northern
Atlantic. The red symbols are buoys and the blue symbols represent ships.
Notice the series of letters and numbers under the blue ship
symbols. These are the "Ship IDs". No two sets of letters and
numbers are the same. Locate at least four ships between 30N - 50N
Latitude and 50W - 80W Longitude. Write down the exact "Ship ID" on
the Student Worksheet.
Ships in the North Atlantic
4. Now click on the Ships Observations Report link below.
Look through
the data reported by the ships selected from the North Atlantic map. Record the water temperature. Record the location of the ship(s).
Ships Database
NOTE: If the Ship ID does not show up in the current hour
observations, use the drop down Time menu and get the data for the
previous hours.
Pair 3
5. Obtain the most recent satellite image of the Gulf Stream and answer
the questions on the student worksheet.
Real Time Sea Surface Temperature Satellite Data
6. Using colored pencils, sketch the approximate current location of the
Gulf Stream on the chart. Use the appropriate colored pencil to represent
the temperature of the water and label. Use the latitude and longitude
points to guide placement of the current.
7. After each pair of students has collected their respective data and
answered their questions, have the students regroup into their group of six.
Have the students compare their data and answer the Assessemtn questions on the worksheets.
Assessment
Compare the ocean water temperature data from the satellite image with
the temperatures collected from the ships and buoys.
1.
How close do the data sources compare?
2.
With the availability of satellite imagery, why do you think scientists continue
to collect data from ships and buoys?
Analyze satellite imagery. Review the following archived satellite images and answer the questions on the
Student Worksheet.
3. Does the position of the North Wall (the Northern boundary
of the Gulf Stream) fluctuate greatly during the year? Explain.
4. Describe yearly sea surface temperature changes of the Northwest
Atlantic Ocean.
5. Study the satellite image below. Based on the information
in the image, estimate the time of year. Support your answer.
Lab Report Assessment
1. Define the following Gulf Stream terms:
North Wall
warm core eddies
cold core eddies
Gulf Stream meanders
Apply the knowledge learned working in your small group to the following
activities. Complete the activities individually and submit your question
responses and completed Gulf Stream Map in your Lab Report.
What
information besides sea surface temperature might illustrate the pathway of the Gulf
Stream?
2.
View the example real time data image to learn
how to locate the Gulf Stream, the position of the North Wall, warm-core
eddies, cold core eddies and Gulf Stream meanders.
3.
Using the AVHRR Sea Surface Temperature Data, choose
a recent 7-Day Composite Image for the Gulf Stream Region:
- Choose the current year and month (Click on choice)
- Scroll down and select the most recent 7-Day Composite Image.
If there is too much cloud interference, click back and
select the next day.
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4.
On the Blank Gulf Stream Map, sketch in the current location of the Gulf Stream
and label the following:
- The Gulf Stream Current
- North Wall
- Meanders
- Cold-core eddies
- Warm-core eddies
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5.
Using the Gulf Stream Velocities, choose the
real time data image timeframe that best matches your sea surface temperature date.
6.
On the Gulf Stream Map, draw in the arrows that represent the direction of the
water flow in the following features:
- The Gulf Stream Current
- North Wall
- Meanders
- Cold-core eddies
- Warm-core eddies
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7. Answer the following questions in your lab report:
a. What direction does the current flow around Cold-core eddies?
b. What direction does the current flow around Warm-core eddies?
c. Do Cold-core eddies or Warm-core eddies have faster current velocities?
d. Where is the location of the North Wall in respect to the Gulf Stream?
e. What is the difference between a meander and an eddy?
f. What features were easily recognized on the sea surface temperature
map?
g. What features were easily recognized on the velocities map?
h. If you had to choose one of these real time data to use while sailing
in the Gulf Stream, which would it be? Why?
i.
How is the Gulf Stream identified today?
j.
Why is it important to know where currents are today?
k.
Why is it so important to spend money on a satellite to collect this data?
l.
How are today's data collection methods different than from the ones identified
in the previous lesson? Better?
m.
Are any of the older methods still employed today? Which ones? Why?
n. In general, does the position of the Gulf Stream change drastically
during the course of one year? Provide support for your response.
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Implementation Tips
Students will need Internet access to complete the Lab Report portion of
this lesson. Please ensure that all students will have access prior to
assigning the Lab Report. An option would be to print and photocopy the
images prior to class and distribute the images to the students with limited or
no Internet access to enable them to complete the assignment.
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