5. Lab 5
Weather and Climate Change
Weather and Climate Change
Concepts to Explore
• Atmosphere
• Weather
• The Water Cycle
• Climate
6. Introduction
The Earth’s atmosphere is composed of 21% oxygen (O2), 78%
Nitrogen (N2) and approximately 1% other
gases (including water vapor, argon, carbon dioxide, hydrogen,
and helium). Oxygen is essential for life and is
used by most organisms for cellular respiration while carbon
dioxide is used by plants and certain bacteria for
photosynthesis.
Figure 1: Clouds are visible accumulation of water droplets that
accumulate in the Earth’s lowest
layer of the atmosphere, the troposphere.
Our atmosphere is composed of five layers:
1. Troposphere - Nearest to the Earth’s surface; layer in which
weather occurs (rising and falling air);
comprises one half of total atmosphere; air pressure is
decreased to 10% of that at sea level.
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Weather and Climate Change
2. Stratosphere - Contains the ozone layer (important for UV
7. ray absorption).
3. Mesosphere - Layer which meteors burn up in upon entering
the Earth’s atmosphere.
4. Ionosphere/Thermosphere - Locations of auroras (e.g., aurora
borealis); layer in which the space shut-
tle orbits.
5. Exosphere - Upper limit of the Earth’s atmosphere; layer
where Earth’s atmosphere merges with outer
space.
Weather is the state of the atmosphere at a given time and place
and includes temperature, pressure, the
type and amount of precipitation, wind, clouds, etc. Weather
conditions can change hour to hour, day to day,
and season to season. Our weather is caused by uneven heating
of the Earth from the sun. The resulting
temperature differentials generate wind that forces warm air to
flow to regions of cooler air. This flow can oc-
cur both horizontally across the surface of the Earth (i.e., from
tropical to polar regions) and vertically, causing
clouds, rain, and storms to develop as warm, moist air cools and
condenses as it rises. In addition to driving
our weather, the sun’s energy also is responsible for regulating
how water moves on, above, and below the
Earth’s surface through the water cycle.
Figure 2: The water cycle - can you name the steps? Refer to
Lab 2 for help!
8. The water cycle describes how the amount of water on Earth
remains constant over time. Water exists in
three different states (in solid form as ice, as liquid water, and
in a gas as water vapor) and cycles continuous-
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Weather and Climate Change
ly through these states. The temperature and pressure determine
which state water is in. The water cycle
consists of the following processes:
• Evaporation of liquid water to a gas (water vapor)
• Condensation of water vapor to liquid water
• Sublimation of solid water (ice) to water vapor (think dry ice)
• Precipitation occurs when water vapor condenses to
clouds/rain
• Transpiration occurs when liquid water moves through plants
9. from roots to leaves, changes to water
vapor and is released to the atmosphere through holes (stoma)
in the leaves
• Surface Run-off occurs when water moves from high to low
ground
• Infiltration occurs when water fills porous spaces in the soil
• Percolation occurs when ground water moves in a saturated
zone below Earth’s surface
Figure 3: Clouds.
Clouds form at many different altitudes in the troposphere when
water vapor in warm air rises and cools. The
water vapor condenses on microscopic dust particles in the
atmosphere and transforms into either a liquid or
solid and is visible as clouds. Warm air can hold more water
vapor than cool air so clouds often form over the
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Weather and Climate Change
10. tops of mountains and over large bodies of water since the air
over these formations is typically cooler than
the surrounding air.
Climate is defined as the long-term average pattern of weather
in a given region. Our climate is influenced by
five components: the atmosphere, the hydrosphere (mass of
liquid water), the cryosphere (mass of solid wa-
ter; ice), the land surface, and the biosphere (life on Earth).
Climate change refers to the observed accelerat-
ed increase in the Earth’s temperature over the past 100 years
and its predicted continued increase. The
Earth’s average temperature has increased approximately 1 - 1.5
degrees F since 1900 (see figure below)
and is projected to rise an additional approximately 3 - 10
degrees F over the next 100 years.
Figure 4: Global Temperature Anomalies. Source:
www.nasa.gov
Changes in the Earth’s atmosphere have contributed to global
11. warming. Global warming is due to the accu-
mulation of “greenhouse gases”: carbon dioxide (CO2) from
burning fossil fuels (oil, gas, and coal); methane
(CH4) from agriculture, landfills, mining operations and gas
pipelines; chlorofluorocarbons (CFCs) from refrig-
erants and aerosols; and nitrous oxide from fertilizers and other
chemicals. Increased temperature results in
increased evaporation, accelerated polar ice melting, increased
number of extreme temperature days, heavier
rains/floods, and more intense storms. These changes will have
important implications across public health,
infrastructure, energy, economic, and political arenas.
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http://www.nasa.gov/
Weather and Climate Change
Experiment 1: Modeling the Water Cycle
In this lab, you will construct a model of the Earth’s
surface/atmosphere to explore how energy drives
weather. Follow the procedure below to complete
Demonstration 1 on modeling of the water cycle.
Materials
12. 100 mL Graduated cylinder
Canning jar
Petri dish
Thermometer
*Hot water
*Water
*Ice cubes
*You must provide
Procedure
1. Using a graduated cylinder, carefully pour 20 mL of warm
water (60 °C) into canning jar and secure the
lid.
2. Fill the petri dish with ice and place on top of the canning
jar’s lid.
3. After 30 minutes, remove the petri dish, carefully remove the
13. lid, and look at the underside. Then, answer
the Post-Lab Questions on the Week 5 Lab Reporting Form.
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Weather and Climate Change
Experiment 2: Assessing Infiltration
Water movement among phases and sources is based on a
number of environmental climatic factors. In this
experiment you will test how water moves between land and the
atmosphere based on differences in weather
conditions. Follow the procedure below to complete Experiment
1 on water movement.
Materials
(2) 9 x 12 in. Bags
250 mL Beaker
200 mL Sand
14. *Water
*A sunny location (window sill, outside porch, etc.)
*A shady location
*You must provide
Procedure:
1. Read through the Experiment 1 procedure and then record
your hypothesis on the effects of sunlight on
evaporation on the Week 5 Lab Reporting Form.
2. Add 200 mL of sand to two separate plastic re-sealable bags.
3. Add 200 mL of room temperature water to each bag.
4. Seal each bag, leaving a bit of air in each.
5. Place 1 bag in a sunny location and 1 bag in a shady location
(complete this in the day when the sun is
15. out).
6. Observe the bags immediately after sealing and again after 3
hours. Answer the Post-Lab Questions on
the Week 5 Lab Reporting Form based on your observations.
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Appendix
Good Lab Techniques
Good Lab Techniques
Good Laboratory Techniques
Science labs, whether at universities or in your home, are places
of adventure and discovery. One of the first
things scientists learn is how exciting experiments can be.
However, they must also realize science can be
dangerous without some instruction on good laboratory
16. practices.
• Read the protocol thoroughly before starting any new
experiment.
You should be familiar with the action required every step of
the
way.
• Keep all work spaces free from clutter and dirty dishes.
• Read the labels on all chemicals, and note the chemical safety
rating
on each container. Read all Material Safety Data Sheets
(provided
on www.eScienceLabs.com).
• Thoroughly rinse lab ware (test tubes, beakers, etc.) between
experi-
ments. To do so, wash with a soap and hot water solution using
a
bottle brush to scrub. Rinse completely at least four times. Let
air
dry
• Use a new pipet for each chemical dispensed.
• Wipe up any chemical spills immediately. Check MSDSs for
special
handling instructions (provided on www.eScienceLabs.com).
17. • Use test tube caps or stoppers to cover test tubes when shaking
or
mixing – not your finger!
A B C
Figure 1: A underpad will
prevent any spilled liquids
from contaminating the sur-
face you work on.
Figure 2: Special measuring tools in make experimentation
easier and more accu- rate in
the lab. A shows a beaker, B graduated cylinders, and C test
tubes in a test tube rack.
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Good Lab Techniques
• When preparing a solution, refer to a protocol for any specific
instructions on preparation. Weigh out the desired amount of
chemicals, and transfer to a beaker or graduated cylinder.
18. Add LESS than the required amount of water. Swirl or stir to
dissolve the chemical (you can also pour the solution back
and forth between two test tubes), and once dissolved, trans-
fer to a graduated cylinder and add the required amount of
liquid to achieve the final volume.
• A molar solution is one in which one liter (1L) of solution
con-
tains the number of grams equal to its molecular weight.
For example:
1M = 110 g CaCl x 110 g CaCl/mol CaCl
(The formula weight of CaCl is 110 g/mol)
Figure 3: Disposable pipettes aid in ac-
curate measuring of small volumes of
liquids. It is important to use a new pi-
pette for each chemical to avoid con-
tamination.
• A percent solution can be prepared by percentage of weight of
chemical to 100ml of solvent (w/v) , or
volume of chemical in 100ml of solvent (v/v).
For example:
20 g NaCl + 80 mL H2O = 20% w/v NaCl solution
19. • Concentrated solutions, such as 10X, or ten times the normal
strength, are diluted such that the final
concentration of the solution is 1X.
For example:
To make a 100 mL solution of 1X TBE from a 10X solution:
10 mL 10X TBE + 90 mL water = 100ml 1X TBE
• Always read the MSDS before disposing of a chemical to
insure it does not require extra measures.
(provided on www.eScienceLabs.com)
• Avoid prolonged exposure of chemicals to direct sunlight and
extreme temperatures. Immediately se-
cure the lid of a chemical after use.
• Prepare a dilution using the following equation:
c1v1 = c2v2
Where c1 is the concentration of the original solution, v1 is the
volume of the original solution, and
c2 and v2 are the corresponding concentration and volume of
the final solution. Since you know c1,
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20. Good Lab Techniques
c2, and v2, you solve for v1 to figure out how much of the
original solution is needed to make a cer-
tain volume of a diluted concentration.
• If you are ever required to smell a chemical, always waft a gas
toward you, as shown in the figure
below.. This means to wave your hand over the chemical
towards you. Never directly smell a
chemical. Never smell a gas that is toxic or otherwise
dangerous.
• Use only the chemicals needed for the activity.
• Keep lids closed when a chemical is not being used.
• When diluting an acid, always slowly pour the acid into the
water. Never pour water into an acid,
as this could cause both splashing and/or an explosion.
• Never return excess chemical back to the original bottle. This
can contaminate the chemical sup-
22. Lab 5 - Demonstration 1: Modeling the Water Cycle
POST LAB QUESTIONS
1. Which water cycle processes are represented in this model
and by what components?
Answer =
2. Which processes are not represented? How could the model
be altered to include these processes?
Answer =
3. How would the “weather” be affected if the water was at a
decreased temperature? What about at an increased
temperature?
Answer =
Experiment 1: Water Movement
POST LAB QUESTIONS
1. Develop a hypothesis predicting the effect of sunlight on
evaporation?
Hypothesis =
2. Based on the results of your experiment, would you reject or
accept the hypothesis that you produced in question 1? Explain
how you determined this.
Accept/reject =
3. What parts of the water cycle are represented in this
experiment?
Answer =
4. How would increasing the proportion of land (sand) to water
affect the amount of water vapor released?
Answer =
5. How would drought conditions impact infiltration and
evaporation from the ground?
Answer =
References