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What Buoys Can (and Cannot) Tell Us
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- Many important measurements can be made at the surface of the
ocean
- Consider how "at sea" instrument data complements data
gathered by Earth-orbiting satellites
- Learn about reference time zones
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At left (<<<) is a map from the National
Data Buoy Center that shows
buoy locations off the northeast U.S. There are many buoys off U.S.
coasts. We will focus on 3 sites underlined in yellow at left (<<<):
Buoy data can tell us about these conditions at a specific place:
- Winds at sea
- Waves
- Weather or atmospheric conditions
- Water temperature
What buoys cannot do is give scientists a "bird's eye" view large
areas of the ocean. This is one reason that scientists also use data collected
by Earth-orbiting satellites. |
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At right (>>>) is an example of the Station Information available
from the National Data Buoy Center.
The location of this buoy is shown on the map above ^^^) .
- The buoy's latitude and longitude are given as 42.90 N, 68.94 W
- Note that the Station number for this buoy is #44005.
There are several instruments on this buoy. Their location on the buoy platform
is described alongside the photo.
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44005 - GULF OF MAINE 85 NM (Nautical Miles) EAST OF PORTSMOUTH,
NH
6-meter NOMAD buoy DACT payload
42.90 N 68.94 W
Site elevation:sea level
Air temp height:5 m above site elevation
Anemometer height:5 m above site elev.
Barometer elevation:sea level
Sea temp depth:1m below site elev.
Water depth:29.3 m
Watch circle radius:69 yards
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The table at right (>>>) is entitled "Conditions
at 44005 as of 2300 Z (7:00 pm EDT) on 08/05/1998." Thus these
data show conditions at the "Gulf of Maine" buoy on August 5, 1998.
Time is given in two ways:
- "2300 Z"
- This is known as "Zulu time," which is also known
as Greenwich Mean Time (GMT). Greenwich, England is globally
accepted as a reference standard for both time and longitude
(its location marks zero degrees longitude). "Zulu" time and
GMT are based on a 24-hour clock.
- "7:00 pm EDT"
- Eastern Daylight Time (EDT) is GMT minus 4 hours (Standard Time is
GMT minus 4 hours).
- Click here to
check out how other U.S. time zones compare to GMT.
You can learn more about this table n the Buoy
Data Formats section.
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Click on the graph icon in the table below to see a time
series plot of the last few days of that observation.
Conditions at 44005 as of 2300 Z ( 7:00 pm EDT) on
08/05/1998:
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Wind Speed: |
0.0 kts ( 00 m/s) |
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Wind Gust: |
1.9 kts ( 1 m/s) |
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Wave Height: |
2.3 ft (0.7 m) |
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Dominant Wave Period: |
10.0 s |
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Atmospheric Pressure: |
30.17 in (1021.7 mb) |
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Pressure Tendency: |
-0.0 mb (Steady) |
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Air Temperature: |
70.5 F ( 21.4 C) |
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Water Temperature: |
67.8 F ( 19.9 C) |
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- Understand the relationships between:
- wave period and wave energy
- wave period and wave length
- wave period, wave length and wave speed (for deep-water waves)
- Learn about one of nature's most destructive events: a tsunami
- Become familiar with a "non-linear" graph of data
- Discover how data are collected by buoys and how these data are
calibrated
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- Surface measurements from buoys are extremely important
for ocean science but are limited as far as area coverage. Look at the map
of buoy locations off the U.S. northeast coast.
- How do you think the number of buoy stations compares
with the number of weather stations on land?
- Given your answer, do you think that weather on
land is better monitored than weather at sea?
- Why do you think this is the case?
- The type of instruments found on the buoy are listed
found by clicking here. Consider the
following information:
- "Anemos" is Greek for "wind"
- "Baros" is Greek for "weight"
- Which measurements are made by the anemometer?
What does the barometer weigh?
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3. The graph at right (>>>) shows the distribution
of wave energy in Earth's oceans. The greater the area of the graph
means the higher energy level for that wave period.
Blue = wave periods less
than 1 minute
Green = wave periods between 1 minute and 1 hour
Greenish-blue = wave periods longer than 1 hour
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- What wave-causing force generates the most of the
energy possessed by ocean waves?
- Why do you think this is the case?
4. A tsunami (pronounced "tsoo-nah-mee")
is a seismic sea wave caused by sudden movements of the earth's crust. A tsunami
has a very long wave period and over deep water, they can reach speeds of
760 km per hour (470 mph).
- Tsunmais are usually caused by underwater earthquakes.
- Can you think of other events that might cause
these long-period waves?
- Click here
to see an animation (with narration) about tsunamis (2 MB).
- Click here
to see how regular wind waves compare to tsunamis.
5. On the graph above (^^^), the distance between "0.1
seconds" and "1 second" is about equal to the distance between
"30 seconds" and "5 minutes." And both of these are much
less than the distance between "12 hours" and "24 hours."
- Can you name the type of scale that is being used
to show time on this graph?
- Can you guess why this scale is called "non-linear"?
- Why was this scale chosen to show this type of
information?
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6. Now
that you know more about the relationship between wave-generating forces and
wave period, let's examine the relationship between wave-generating
forces and wave length (>>>).
- Which wave-generating force(s) cause(s) relatively
short wave length waves?
7. For DEEP-WATER WAVES,
there is a relationship between wave period, wave length, and wave speed.
- Click here to see
a graph that shows how these factors are related.
- From this graph, you'll see that a wave with a period
of 8 seconds has a wavelength of about 100 meters.
- What is the speed of such a deep-water wave?
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8. In
Step 4, you examined the wave period of tsunamis. You also learned that, over
deep water, they can reach speeds of 760 km per hour (470 mph).
- Do tsunamis have very short or very long wave lengths?
Why?
- To calculate the speed of a tsunami. you would NOT
use the graph that shows the relationship
between wave period, wave length and wave speed for DEEP-WATER WAVES (presented
in Step 5).
- Can you guess why not?
- [HINT: Deep-water waves are defined as waves
whose depth is greater than one-half their wave length.]
9. Earth-orbiting satellites
provide frequent data over very large areas. Satellite measurements -- collected
far above the ocean -- are often compared to "in-water" buoy measurements.
This is done to ensure that the satellite sensors are correctly calibrated.
To help understand calibration, consider this:
- Your favorite cookies are the "slice and bake"
type that come in a cylinder-shaped package. The recipe reads:
- "Cut dough into 1 inch thick slices"
- "Place slices onto ACME-brand cookie sheet"
- "Place slices, round side down, at least
1 inch apart"
- "Bake for 20 minutes"
- "Use oven temperature of 325°F"
- However, when you follow this recipe your cookies
are over-cooked. You bought the ACME-brand cookie sheet last week so that's
not the problem. You decide it's time to check or calibrate the "instruments"
used to bake the cookies.
- How would you confirm the following measurement
devices are working correctly?
- Your "handy 1 inch measure" (the
distance between the knuckle and tip of your thumb)
- Oven timer
- Oven temperature
- What test(s) would you perform to make sure
that you've corrected the problem?
- Let's say that your cookies turn out perfect every
time.
- Does this necessarily mean that all of your
measurement devices are working correctly?
- Can you imagine how 2 improperly working tools
can combine to give good results?
- For example, what if your "handy 1-inch
measure" is too long AND your oven temperature is too high?
Could this combination give you "perfect cookies"?
- What steps should scientists take to make sure ALL
of their instruments are properly calibrated?
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- anemometer
- barometer
- calibrate
- Greenwich Mean Time
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- longitude
- non-linear
- tsunami
- wave energy
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- wave length
- wave period
- wave length
- "Zulu" time
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