Geo3100 - Study Guide Chapter 9
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Dec 6, 2023
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Exam 3 Study Guide: Part 2
Chapter 9: Atmospheric Processes and Severe Weather
Instructions:
Use the chapter 9 reading and lecture materials to answer the following
questions.
Some questions have multiple parts so
carefully read the questions
and provide
detailed and specific responses.
Generally, the difference between a good grade and a
poor grade on an assignment is based on whether or not the questions were answered
completely.
The purpose of this assignment is to test your understanding of course
materials covered from Chapter 9. Additionally, this assignment doubles as Part 2 of the
Exam 3 study guide.
1.
Describe the three types of heat transfer and how they differ from one another. (1
pt)
1.
Radiation: wavelike energy that is emitted by any substance that posses heat.
2.
Conduction: the transfer of heat through a substance by means of atomic or
molecular interactions.
3.
Convection: the transfer of heat by the mass movement of a fluid.
2.
Describe Earth’s energy balance. (1 pt)
1.
Earth’s Energy Balance: a general equilibrium between incoming and
outcoming energy. The energy that earth receives from the sun affects the
atmosphere, oceans, land, and living things before being radiated back into
space.
3.
How is color related to energy absorption? (1 pt)
1.
Dark colors have low albedo (like the forests and oceans). Bright colors like
Ice have high albedo.
4.
Describe the characteristics of the troposphere. (1 pt)
1.
1. The Troposphere contains air, with high nitrogen and high water vapor
content. Temperature and pressure decrease with elevation.
5.
Describe basic atmospheric circulation. (1 pt)
1.
The Earth’s atmosphere circulates as air is heated and cooled. The density of
the air and atmospheric pressure help drive this as cold air is more dense
than hot air and sinks while hot air rises to replace its space. The hot air is
then cooled becomes wetter and denser as the change in pressure assists this
transformation. The once hot air is now cold and falls to continue the cycle.
6.
What is the Coriolis affect and how does it influence storm rotation in the northern
and southern hemispheres? (1 pt)
1.
Earth's rotation causes deflection or spin in the atmosphere. Low pressure
systems in the northern Hemisphere spin counterclockwise. The vector of
rotation is perpendicular at the equator and thus it has no effect. The
opposite will be seen in the southern hemisphere. This means that storms
forming at the equator stay there and that storms forming at the subtropics
move over Open Ocean and when conditions are correct they form tropical
storms and possibly hurricanes.
7.
Describe the polar jet stream and subtropical jet stream. (1 pt)
1.
The polar jet stream and subtropical jet stream both belong to the northern
hemisphere. The polar jet stream occurs at a lower altitude while the
subtropical is at a higher altitude. Both jet streams move from west to east
and have different strengths with the polar stream being stronger.
8.
Describe the three stages of thunderstorm development and conditions necessary
for both to form. (1 pt)
1.
Cumulus Stage: a cloud forms from water vapor being condensed as it rises.
This stage requires a continuous amount of head and condensation which will
drive the expansion and rise the cloud.
2.
Mature Stage: updrafts and downdrafts are both active. In this stage
precipitation leaves the clouds once the updrafts of air can longer support
them. The falling precipitation and downdrafts leave the cloud base and
storms begin to produce heavy rain, lightning, thunder, and depending on the
precipitation cycle hail.
9.
Describe the stages of tornado development. Where are tornados likely to occur
within the United States and why? (1 pt)
1.
Organizational stage: when vertical wind shear starts causes rotation of winds
within a storm. In this stage a funnel begins to descend towards the ground
but does not yet make contact.
2.
Mature stage: includes the visible development of a condensation funnel form
rotating winds extends to the ground. Depending on the strength of the
tornado smaller whirling bodies called suction vortices may form.
3.
Shrinking stage begins as the tornado runs out of the moist/warm air and
cause the funnel to thin. During this stage the tornado is more dangerous
because wind speeds being to increase as the diameter decreases.
4.
Decaying stage (rope stage): downdrafts of air cause the tornado to move in
an erratic pattern and eventually disappear.
10.
How can severe weather hazards be minimized? (1 pt)
1.
As with all hazards our ability to react to hazards appropriately is very
important. With severe weather hazards the use of forecasting and predicting
technology to accurately predict occurrence allows to mitigate hazards. By
implementing watches and warning for severe weather appropriate
preparation and eventual actions is available to persons in at risk areas.
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