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Atmosphere Activity Sheet
130 points
As always,
I
t’s all about relationships.
As you prepare for exam-3, review the content below and formulate relationships between
atmospheric processes, the role of water vapor in the atmosphere, cloud formation and Bakersfield climate.
In many cases, don’t
memorize, but explain in your own words and develop a picture in your mind regarding atmospheric processes.
Most importantly, as
you learn the concept and relationship, be able to explain the concept using the proper terminology.
Please make sure you take a look
at the probable exam essay questions at the end of this activity sheet.
It’s recommended that you view the atmosphere lecture
in
its entirety before answering questions.
1.
Construct a diagram depicting the layers of the earth’s atmosphere and properly identify the 4 major
atmospheric terms.
a.
Relationship Questions:
1.
Using your atmosphere diagram, describe temperature changes that take place
from one layer to the next.
Troposphere : on this layer as altitude will boom , the
temperature of air decreases . - The troposphere is warmer close to the Earth 's
floor as warmth from the surface of earth warms this air . Due to the fact the
altitude will boom it outcomes in decrease in fashion of air molecules , for that
reason the common of their kinetic electricity decreases . - Stratosphere : the
altitude increases , the air temperature will boom . The Stratosphere has a layer
of ozone , referred to as the ozone layer . this layer absorbs most of the
ultraviolet radiation from sunlight hours which ends up within the stratosphere
being warmer . - Mesosphere : due to the fact the altitude will increase , the air
temperature decreases . The Mesosphere , has a decrease in temperature with
altitude as decreases within the density of the air molecules . - Thermosphere :
the altitude will increase , the air temperature will increase.
2.
What major factor influences temperature change in each atmospheric layer?
In a
few layers , temperature will increase with altitude and in others it decreases. The
temperature gradient in every layer is determined through the warmth source of
the layer . The most vital layers of the atmosphere have one-of-a-type
temperature gradients and the ability to create the thermal shape of the
surroundings.
3.
The stratosphere warms as altitude increases, but what is the maximum
temperature the stratosphere reaches?
How does this temperature relate to
where we live?
The stratosphere is the layer above the troposphere, temperature
within the stratosphere rises with growing altitude, as ozone layer absorbs the
greater a part of the solar ultraviolet radiation. - Ozone molecules in this layer
take in immoderate-strength ultraviolet (UV) mild from the solar, converting the
UV energy into warm temperature. this deposit protects human lifestyles from
direct daytime.
4.
Provide a list of characteristics that differentiate one atmospheric layer from
another.
The surroundings is cut up into layers primarily based on how the
temperature in that layer changes with altitude, the layer's temperature gradient.
5.
Using the pie diagram outlined in lecture, write and LEARN the composition or
the earth’s atmosphere.
Earth's environment is a composition of 78 % nitrogen,
21% oxygen, 0.9 % argon, and 0.1% different gases.
6.
Describe atmospheric pressure and the relationship to our atmosphere.
Atmospheric pressure and wind are each extensive controlling elements of
weather and climate on stress is the strain exerted on a unit vicinity, and
atmospheric strain is identical to the load of air above a given vicinity on the
earth's floor or inner its surroundings.
7.
What is an atmosphere?
Do other planets have atmospheres, Explain.
An
environment may be defined as a layer of fuel or we can term as layers of gases
that envelope a planet and is held in place thru the gravity of the planetary
frame . Astronomical bodies hold an surroundings on the same time as their get
away pace is drastically huge than the not unusual molecular tempo of the gases
present inside the environment. Out of these, the planets Venus, Earth, Mars,
Jupiter, Saturn, Uranus, and Neptune have massive atmospheres.
2. Ozone
a.
Relationship Questions:
1.
What is ozone, where in the atmosphere is it found
The ozone layer is a type of
compound that has those oxygens combined and is found in the stratosphere.
2.
How important is ozone -- Explain
Very important because its the reason, we are
alive because it blocks the UV sunlight from burning us into bacon.
3.
Describe how ozone reacts with UV sunlight to protect life on earth (see lecture
animation)
It absorbs the UV sunlight radiation.
4.
How much UV sun radiation is absorbed from ozone and what percentage of UV
light reaches the earth’s surface.
Think about this answer and the fact, we still
get sunburned.
Explain
97% is absorbed, 3% reaches the earths surface but still
makes it very hot.
5.
Is ozone the same as smog, Explain
The ozone is produced when sunlight reacts
with vehicle exhaust and oxygen in the air.Smog is produced when the oxygen
and vehicle fumes react in the sunlight.
3.
Sunlight
(insolation)
and or all light is identified using wavelengths which is grouped into the
electromagnetic spectrum.
Construct a diagram showing the entire electromagnetic spectrum scale
(EM scale) and label the following:
a.
Wavelength
b.
Long and short wavelength groups
c.
Wavelength types (radio, microwaves……….. Gamma rays)
d.
Visible light spectrum (within the EM scale)
b.
Relationship Questions:
1.
What is the relationship between wavelength and long wave/short wave
radiation?
Shortwave radiation (visible light) contains a lot of energy; longwave
radiation (infrared light) contains less energy than shortwave radiation
(shortwave radiation has a shorter wavelength than longwave radiation).
a.
What wavelengths are harmful and non-harmful to life on earth, Explain:
(consider wavelength and how fast light travels)
Due to Uv exposer
limites
2.
Differentiate between various types of wavelengths (radio, microwave, inferred
……………)
Radio waves have photons with the lowest energies. Microwaves
have a little more energy than radio waves. Infrared has still more, followed by
visible, ultraviolet, X-rays and gamma rays.
3.
How fast does light travel and how is the speed of light and wavelength used to
describe the term frequency?
They are all related by one important equation: Any
electromagnetic wave's frequency multiplied by its wavelength equals the speed
of light.
a.
Explain the concept of frequency and relationship to long and short wave
radiation and question 1a above.
4.
The sun delivers the entire EM scale to the earth.
Describe how the earth’s
atmosphere (layers of the atmosphere) changes insolation to long wave radiation
by the time insolation reaches the earth’s surface.
Shortwave and longwave
radiation interacts with the earth and atmosphere in different ways. Shortwave
radiation (visible light) contains a lot of energy; longwave radiation (infrared light)
contains less energy than shortwave radiation (shortwave radiation has a shorter
wavelength than longwave radation).
5.
4.
Atmospheric processes are primarily controlled by the presence of water vapor in the earth’s
atmosphere.
It is extremely important that you learn how important water vapor is in our atmosphere.
a.
Relationship Questions:
1.
What percentage range is the presence of water vapor in the earth’s atmosphere
The percentage of water vapour in the atmosphere range between 0.2 % to 4 %.
a.
Where on earth would one expect the highest levels of water vapor and
lowest levels of water vapor, Explain
water vapour concentration varries
with latitude.it's concentration maximum over tropical region ,as high as 3-
4% and if we go towards pole it's concentration is reduced significantly.
2.
Where does the water vapor come from that fills the earth’s atmosphere --- Think
evaporation
About 90% of water vapour comes from water bodies like
sea,ocean,lake,river etc and about 10 % comes from transpiration of plants.
5.
The concept of latent heat drives most atmospheric processes we feel and see (clouds, storms,
hurricanes ect… It’s important to grasp the latent heat concept.
a.
Relationship Questions:
1.
What is latent heat (describe) -
Latent heat is the extra amount of heat required
by the 1gm of substance to raise its temperature by 1 degree celcius .
2.
How does energy (from the sun) drive the concept of latent heat?
In your
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explanation use the terms evaporation, condensation, heat absorption, heat
release
The extra amount of energy which fall on the earth's surface from sun
helps in evaporation process as the heat energy absorbed by the water particle
i.econversion of liquid state(water) to gaseous state(water vapour). When
theextra amount of heat released by the water particle the evaporated
waterparticle condensate i. conversion of state from gaseous to liquid
a.
In your answer, explain what happens to energy during the process of
evaporation and condensation -
During evaporation, energetic molecules
leave the liquid phase, which overally decreases the energy of the
remaining liquid molecules. Energy is absorbed by the water molecules in
evaporation.
3.
Explain how heat energy (sun) changes the energy level of water (liquid state),
water vapor (gas state) and ice (solid state) using the concept of latent heat. -
During evaporation, energetic molecules leave the liquid phase, which overally
decreases the energy of the remaining liquid molecules. Energy is absorbed by
the water molecules in evaporation.
4.
Finally, in your own words and after thoroughly answering the above questions,
write a statement explaining latent heat in YOUR own words.
Latent heat is the
extra amount of heat required by the substance to convert from one state to
another state.
6.
The concept of relative humidity
a.
Relationship Questions
1.
Explain the difference between humidity and relative humidity (RH)
Humidity
, It
means amount of water or vapor present in air at certain temperature in the
nature or a system . Humidity depends upon air temperature , cool air have
higher humidity related to warm air.
Relative Humidity
- It have ratio between vapor present in air and actual vapor
present in air at same temperature in the system . It express in percentage.
2.
It is essential that you are able to calculate RH.
RH is always calculated in terms
of percentage.
a.
Calculate the RH if air at 25C can hold 20g of water vapor and it currently
is holding 5g.
What is the RH?
The answer is 25% ----- how did you get
this answer, Explain
- RH = Vobs/Vactual*100
- = ( 5/20 ) *100
- =5 *5=25 %
b.
Calculate the RH if air at 30C can hold 35g of water vapor and it currently
holds 15 g of water vapor.
What is the RH?
- RH = Vobs/Vactual*100
- =( 15/35)*100
- = 42.8%
3.
The concept of dew point (DP), relative humidity (RH) and condensation
a.
What is the dew point?
It is the amount of temperature at which air
became saturated and no more vapor exit in air , condense vapor change
into rain.
b.
Explain what happens to water vapor when RH is 100%
When relative
humidity became 100%, it means air became saturated and dew point
occur at which vapor condensed. c. When the temperature of an air
parcel decrease , Rh increase and became 100% which causes
saturation because air parcel can't hold any more water vapor.
c.
When the temperature of an air parcel _______________, RH humidity
_________________ and reaches 100% which causes _____________
because the air parcel can not hold any more water vapor.
d.
What is the current RH in Bakersfield? (look it up on your phone)
e.
What is the dew point for Bakersfield
(look it up on your phone)
f.
Explain when the Bakersfield atmosphere begins to condense given your
answers in d and e.
4.
Now, describe
the relationship between RH, DP, condensation, air temperature,
saturation and latent heat
7.
The greenhouse concept
a.
Relationship Questions:
1.
Listening to the lecture, describe how the greenhouse effect warms the earth’s
atmosphere
The greenhouse effect positively impacts the Earth's atmosphere's
temperature. The greenhouse effect refers to the ability of the atmosphere to
selectively absorb the electromagnetic spectrum of longer wavelengths and
remain transparent to wavelengths of shorter wavelengths. This is achieved
through the presence of greenhouse gases such as CO2, CH4, and others.
These gases absorb longer wavelength components of terrestrial radiation and
thus warm the Earth's atmosphere.
2.
What role do greenhouse gasses play regarding the warming of the atmosphere?
As mentioned, the greenhouse gases selectively absorb the longer wavelength
component of terrestrial radiation and thus warm the lower atmosphere. It is to be
remembered that the maximum concentrations of greenhouse gases are found in
the lower atmosphere and hence, the lower atmosphere is impacted at its
maximum.
3.
Is the greenhouse effect natural? Explain your answer
The greenhouse effect is a
natural phenomenon and occurs in nature through the presence of gases such
as CO2, CH4, water vapor, and others. In the absence of the greenhouse effect,
the Earth's surface temperature would have been subzero. Hence, the
Greenhouse effect of nature is critical in maintaining a sustainable temperature
on the surface of Earth.
4.
Which greenhouse gas creates stronger counter reradiation, water vapor or
carbon dioxide?
CO2 creates stronger counter radiation among water vapor and
carbon dioxide.
a.
Which greenhouse gas (water vapor or carbon dioxide) is more
concentrated in the earth’s atmosphere. Show your answer using
numbers
Water vapor is most concentrated in the Earth's atmosphere and
is also themost abundant greenhouse gas found in the Earth's
atmosphere.
b.
What do you think is a bigger contributor to global warming in terms of
greenhouse gasses (water vapor or carbon dioxide)? Explain
The biggest
contributor to the greenhouse effect is water vapor due to itshigh volume
present in the Earth's atmosphere.
c.
Do you think global warming is caused from humans or natural earth
processes --- Explain your reasoning from your answers above.
Global
warming is caused by the nature as part of its normal process . However ,
due to the anthropogenic interference with the environment , the
concentration of the greenhouse gases in the atmosphere has increased,
resulting in the rapid temperature rise within a short interval of time. This
is categorically dangerous for the existence of humans
.
8.
Adiabatic processes
a.
Relationship Questions:
1.
IMPORTANT!
Describe what is meant by adiabatic cooling and heating of the
atmosphere
2.
How does atmospheric air pressure changes promote adiabatic cooling / heating
of the atmosphere?
As a parcel of air rises, the water vapor in that parcel will
condense and heat will be released. The rising air will therefore cool more slowly
as it rises; the wet adiabatic lapse rate will in general be less negative than the
dry adiabatic lapse rate.
3.
How does air cool or heat under the Dry adiabatic rate (DAR) and the moist
adiabatic rate (MAR)--- In other words, for every 1000 m of rising air or sinking
air, how does the temperature change adiabatically under the DAR and MAR.
The moist adiabatic lapse rate is less than the dry adiabatic lapse rate because
moist air rising condenses out its water vapor (once saturation is attained).
9.
Cloud formation using adiabatic processes, dew point, RH, DP and the LCL
a.
Relationship Questions:
1.
What is a cloud?
Cloud is an aerosol consisting of a visible mass of minute liquid
droplets , frozen crystals , or other particles suspended in the atmosphere of a
planetary body or similar space.
2.
Define the following terms:
Adiabatic - The process or condition in which heat does not enter or leave
the system concerned .
b) Cloud - Cloud is an aerosol consisting of a visible mass of minute liquid
droplets , frozen crystals , or other particles suspended in the atmosphere
of a planetary body or similar space .
C ) Saturated - When a volume of air at a given temperature holds the
maximum amount of water vapour , the air is said to be saturated .
D ) Relative humidity ( RH ) - It refers to the moisture content ( i.e. , water
vapor ) of the atmosphere , expressed as a percentage of the amount of
moisture that can be retained by the atmosphere ( moisture - holding
capacity ) at a given temperature and pressure without condensation .
E ) Dew Point - The dew point is the temperature to which air must be
cooled to become saturated with water vapor .
F ) Convection - It describes the vertical transport of heat and moisture in
the atmosphere , usually from a warmer area ( the surface ) to a cooler
one ( aloft ) .
G ) Liffting condensation level - It is formally defined as the height at
which the relative humidity of an air parcel will reach 100 % with respect
to liquid water when it is cooled by dry adiabatic lifting .
H ) Condensation - Condensation is the change of the state of matter
from the gasphase into the liquid phase,.
I)Latent Heat-It is energy in the form of heat released or absorbed by a
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substanceduring a phase change of the substance. The amount of latent
heat involved withcondensation/evaporation and freezing/melting are
different under differenttemperatures and pressures.
J) Gravity- It is the force that pulls something towards the centre of the
earth.
K) Atmospheric pressure-Atmospheric pressure, also known as
barometric pressure,is the pressure within the atmosphere of Earth. The
standard atmosphere is a unit ofpressure defined as 101,325 Pa, which is
equivalent to 760 mm Hg, 29.9212 inches Hg, or 14.696 psi.
L) Precipitation- Precipitation is any product of the condensation of
atmospheric water vapor that falls under gravitational pull from clouds.
The main forms of precipitation include drizzling, rain, sleet, snow, ice
pellets, graupel and hail.
M) Evaporation- Evaporation is a type of vaporization that occurs on the
surface of aliquid as it changes into the gas phase
N) Umbrella - used for protection from rain and sun.
3.
Below is a paragraph with blanks.
Fill in the blanks with the proper terms listed
above (a-j) from your definitions .
The following terms are related with regards to
cloud formation.
Once you have put the correct terms in the blanks, learn how a
cloud forms --- not memorize.
As warm air takes in moisture due to ___
Dew Point
_______________ , air begins to rise and
________
pressure
__________
decreases causing the rising air to ____
adibatic
___________ cool.
As
cooling air takes place, ______
dew point
_____________ increases and approaches ______
relative
humidity
____________ where air is saturated to 100% creating ______
percipitation
__________ and
releasing ______
latent heat
______________.
Condensation takes place at an altitude within the
atmosphere known as the _______
LCL
__________________.
At this altitude, _____
clouds
_________
form. At this atmospheric elevation, clouds appear to have flat bottoms.
Air continues to rise beyond
the LCL where air is completely ___
saturated
___________
and condensation is producing larger and
larger water drops.
Water drops are suspended within the could due to _______
convection
currents
_____________ currents caused by ____
gravity
_________ heat release at the LCL and rising
air becomes cooler as it moves away from the LCL.
Water droplets become increasingly larger and
convection currents cannot hold them.
____
LCL
__________ takes over, clouds begin to
______
evaporation
_______and you now need to get your _______
percipation
_____________.
10.
Draw a diagram that represents your paragraph and blanks you filled in.
It is extremely
important that you can explain how a cloud forms in your own words using the proper terminology.
11.
Orographic lifting and Bakersfield climate
a.
Relationship Questions:
1.
What is meant by orographic lifting of air masses?
Orographic lifting of airmasses
refers to the forced lifting of warm and humid airmass under the trigger effect
provided by a mountain barrier standing in the way of the air mass movement.
The forced lifting of the warm and humid airmass results in its cooling and
condensation thus causing orographic precipitation along the slope of the
mountain.
2.
Watch the last slide of atmospheric presentation and observe how an air mass
originates in the Pacific Ocean and moves across California from west to east.
a.
Explain how air moving up the western side of the Coast Range and
Sierra Nevada Mountains form clouds -- HINT: See your answers in the fill
in the blank paragraph.
As the warm and humid airmass from the Pacific
Ocean encounter thewestern slopes of Coast Range mountains and
Sierra Nevada mountains,they are forced to rise upwards. During the
process, the warm and humid airmasses cool and condense around
hygroscopic nuclei thus forming clouds.
b.
How are rain shadows produced? Both in the SJV and Mojave desert
areas.
HINT: adiabatic warming on the eastern side of the mountain
ranges.
The clouds formed causes precipitation along the slope side of
the mountain facing the warm and humid airmass. This side is known as
the windward side. As the rising air reaches the summit, it is almost
devoid of humidity content. Thereafter, it begins its descent along the
opposite slope of the mountain. During the process, the air warms at an
adiabatic lapse rate. This leads to the prevalence of dry atmospheric
conditions without any chances of precipitation. This slope is called the
rainshadow region.
c.
Why is the Bakersfield area considered a semi-desert climate?
Bakersfield area is located along the Rainshadow region of the Coast
Range mountains and hence observes minimal precipitation. Thus, it
experiences a semi-arid climate.
Possible Essay Questions for EXAM 3
1.
Describe adiabatic processes and how it relates to cooling and warming air within the earth’s
atmosphere
2.
How does a cloud form?
3.
What are the layers of the atmosphere and how does temperature relate to each atmospheric layer?