Workshop 2 (February 5th 2000)
The North Atlantic Oscillation and Climate Variability
Sample Questions you can use related to this topic for student
investigations:
By Dr. Michael Passow
Here are some examples of questions that correlate with NY standards. You
might find these types of questions in future Regents Exams.
The chart below
presents a comparison of selected atmospheric and oceanic conditions in the
western Pacific and Eastern Pacific during the “long-term-average” and an
“El Nino” event.
Use this chart and your knowledge of science to answer the questions
below.
|
Variable
|
Long-term-average
W.
Pacific
|
El
Nino event
W.
Pacific
|
Long-term
average
E.
Pacific
|
El
Nino event
E.
Pacific
|
Atmospheric
|
|
|
|
|
|
Rainfall
|
high
|
lower
|
low
|
higher
|
|
Surface
air pressure
|
low
|
higher
|
high
|
lower
|
|
Trade
winds
|
weak
east-to-west
|
variable
|
strong
east-to-west
|
strong
east-to-west
|
|
|
|
|
|
|
Oceanic
|
|
|
|
|
|
Surface
currents
|
east-to-west
|
west-to-east
|
east-to-west
|
west-to-east
|
|
Sea
surface temp.
|
high
|
lower
|
low
|
higher
|
|
Sea
surface height
|
high
|
lower
|
low
|
higher
|
|
Thermocline
depth
|
deep
|
shallower
|
shallow
|
deeper
|
Multiple-choice:
_____Compared with
the “long-term-average” in the eastern Pacific, surface air pressure during
an “El Nino” event
1.
decreases and rainfall decreases
2.
decreases and rainfall increases
3.
increases and rainfall decreases
4.
increases and rainfall increases
_____During an
“El Nino” event, the warm water layer near the surface in the western
Pacific
1.
becomes shallower as cold water upwells from below
2.
becomes thicker as winds blow warm water from east-to-west
3.
remains the same thickness as during “long-term average” conditions
4.
varies with longitude
Constructed
response:
Explain the affect
warmer water in the eastern Pacific during an “El Nino” event would have on
the area’s surface air pressure and rainfall patterns.
Describe two changes in oceanic conditions in the
western Pacific during and “El Nino” event compared with
“long-term-average” conditions.
Explain why
using “sea surface temperature anomaly” patterns are more useful to
oceanographers than using actual sea surface temperatures.
The chart below shows the pattern of
sea level pressure differences between two selected locations.
This is called the “North Atlantic Oscillation (NAO) Index.”
[Source: J.
Hurrell, from http://www.ldeo.columbia.edu/programs/index.html]
Impacts
that have been associated with a positive
NAO value include: warmer winter temperatures and fewer snow days in
northeastern North America; longer growing seasons in Scandinavia, and greater
rainfall and river runoff in the Central US.
Impacts associated with a negative NAO value include: warmer sear surface
temperatures, more and stronger hurricanes in the tropical Atlantic and Gulf
Coast; greater scallop harvests in eastern Long Island; and increased grade and
olive harvests in Spain and Portugal.
Explain whether
these data support the theory of Northern Hemisphere warming during the last fifty
years.
[Use the “NAO Index” chart above for the following
multiple-choice questions.]
_____During most of the past fifteen years, the NAO has
helped create in Europe and the northeastern U.S. winters that were
1.
colder than normal
2.
milder than normal
3.
near the average
_____Very severe
winters in Europe associated with a strongly negative NAO occurred in
1.
1870, 1925, 1970
2.
1892, 1904, 1955
3.
1904, 1982, 1987
4.
1916, 1936, 1969
|