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Grade
Level: Elementary
| Time:
Introduction
- 30 min, Group Activity - 45 min, Wrap Up - 20 min
| Content Standard NSES Physical Science, properties of objects and
materials | Ocean Literacy Principle 1f:
The ocean is an integral part of the water cycle and is connected
to all of the earth's water reservoirs via evaporation and
precipitation.
Big
Idea
Water
can change states among liquid, vapor (gas), and
ice (solid)
at various stages of the water cycle. Temperature
affects the
change of water from one state to another. When water vapor
gets cold it changes to a liquid. This is called
condensation.
When heat is applied to water, it changes from a liquid to
a gas. This is called evaporation. This
activity will focus
specifically on two aspects of the water cycle: evaporation
and condensation.
Key
Concepts
-
Evaporation
occurs when a liquid is changed into a gas.
- Evaporation
occurs when the temperature of a liquid
is increased.
- Condensation
occurs when a gas is changed into a
liquid.
- Condensation
occurs when the temperature of the vapor
decreases.
- When
the sun heats up water in rivers, lakes
or the ocean,
it turns into vapor or steam. The water vapor or
steam leaves the body of water and goes into the
air.
Essential
Questions
- How
does water change?
- How
does water move?
- How
does life depend on water?
- Where
does the water that forms on the outside of your
drinking glass come from?
- Where
does the water go when it is
evaporated?
Knowledge
and Skills
- Observe
the relationship between temperature and
condensation
and temperature and evaporation.
- Water
vapor in the air gets cold and changes back into
liquid water.
- When
water is heated it changes into a
gas.
- Use
a model to simulate the water cycle.
Prior
Knowledge
- Basic
familiarity with the water cycle as a diagram and
introduction to the terms used to
describe the various
stages water goes through in a cycle.
- Some
events in nature have a repeating pattern - such
as daily weather patterns or changes in
temperature
and the appearance of rain and snow at different
times of the year.
- Water
can be a liquid, solid, or gas and can
go back and
forth from one form to another.
- Water left in an open container disappears, but water in a closed
container does not disappear. (Might be helpful
to complete Evaporation Investigation before this
activity.)
Common
Preconceptions
- The water
in a drinking glass
seeps through the wall of the
glass, or
evaporates from the inside and condenses
on the outside.
- Students
have a difficult time
accepting the idea of invisible
particles of water in the
air.
- Students
understand the concept
of boiling and freezing
before understanding
evaporation and condensation.
- The water
cycle involves freezing
and melting of water.
- Condensation
occurs because the
"coldness changed the water,"
or "cold caused oxygen
and hydrogen to change to
water."
- When water
evaporates, it just
disappears and ceases to exist.
- When
water evaporates, it
immediately goes up to the
clouds or into the sun.
Concept
Map
A concept map can be a helpful evaluation tool for an
activity such as this, see Assessment
Activities for further
ideas. The map provided here relates to the
branch "Hydrologic
Cycle " from the comprehensive Aquarius
Concept Map
- Water and its patterns on Earth's surface.

Background
From
the US Geological Survey
-
The
Water Cycle
The
water cycle has no starting point. But we'll begin
in the oceans, since that is where most of
the Earth's
water exists. The sun, which drives the
water cycle,
heats water in the oceans. Some of it evaporates as
vapor into the air. Ice and snow can
sublimate directly
into water vapor. Rising air currents
take the vapor
up into the atmosphere, along with water
from evapotranspiration,
which is water transpired from plants and
evaporated
from the soil. The vapor rises into the air where
cooler temperatures causes it to condese
into clouds.
Air currents move clouds around the globe,
cloud particles
collide, grow, and fall out of the sky as
precipitation.
Some precipitation falls as snow and can
accumulate
as ice caps and glaciers, which can store frozen
water for thousands of years. Snowpacks in
warmer climates
often thaw and melt when spring arrives, and the
melted water flows overland as snowmelt.
Most precipitation
falls back into the oceans or onto land,
where, due
to gravity, the precipitation flows over
the ground
as surface runoff. A portion of runoff
enters rivers
in valleys in the landscape, with
streamflow moving
water towards the oceans. Runoff, and groundwater
seepage, accumulate and are stored as freshwater in
lakes. Not all runoff flows into rivers,
though. Much
of it soaks into the ground as
infiltration.
Evaporation
drives the water cycle. Evaporation
from the oceans
is the primary mechanism supporting the
surface-to-atmosphere
portion of the water cycle. After
all, the large
surface area of the oceans (over 70% of
the Earth's
surface is covered by the oceans) provides the
opportunity for such large-scale evporation to
occur. On a global scale, the amount of
water evaporating is about the same as
the amount
of water delivered to the Earth as
precipitation.
This does vary geographically, though.
Evaporation
is more prevalent over the oceans than
precipitation,
while over the land, precipitation
routinely exceeds
evaporation. Most of the water that evaporates
from the oceans falls back into the
oceans as precipitation.
Only about 10% of the water evaporated from the
oceans is transported over land and
falls as precipitation.
Once evaporated, a water molecule spends about
10 days in the air. The process of evaporation
is so great that without precipitation, runoff,
and discharge from aquifers, oceans
would become
nearly empty over time.
Condensation
is the process by which water vapor in the air is
changed into liquid water. Condensation
is crucial
to the water cycle because it is responsible for
the formation of clouds. These clouds may produce
precipitation, which is the primary
route for water
to return to the Earth's surface within the water
cycle. Condensation is the opposite of
evaporation.
You don't have to look at something as
far away as
a cloud to notice condensation.
Condensation is responsible
for ground-level fog, for your glasses fogging up
when you go from outside on a cold winter day and
to inside a warm room, for the water
that drips off
the outside of your glass of iced tea,
and for the
water on the inside of the windows in
your home on
a cold day.
Materials:
artists clay or plastic mountain
model; plastic
(transparent) shoebox with cover or a small
glass aquarium
and plastic wrap for a cover; Petri dish; lamp; water;
ice; data sheet
Preparation:
If
you have a large aquarium, you can do this activity as
a demonstration, allowing the students to study
and observe
the phenomena and develop their own ideas and
conclusions
for class discussion. With sufficient
materials, you can
do it as a group project, with teams of three
to five students
responsible for setting up the model and
drawing conclusions
from their own work. The activity is described below as
if it were a demonstration. As always,
it's important not to overly explain what is
"supposed" to
happen, but rather let them discover the
model cycle for
themselves.
Activity
Adapted from
University Corporation for Atmospheric Research
LEARN
- Using a white or chalk board to
record student thoughts
and discussion points, engage the class in a discussion
of the water cycle. Integrate the K-W-L
strategy through
the discussion - what I know, what I
want to know,
and what I learned. Revisit this
discussion in the
assessment piece.
- Using
the clay, have each group shape a mountain. Place the
mountain on one side of the shoebox with the
sloped side
facing the interior of the box where the
"ocean" will
be.
- Pour
water into the "ocean" basin until
about one-fourth of
the mountain slope is covered. Replace the lid of the
shoebox.
- Place
a Petri dish on top of the shoebox over the mountain
(as shown). Place crushed ice into the Petri
dish.
- Position
the lamp over the ocean. Turn on the lamp.
CAUTION: THE
LAMP WILL GET HOT. DO NOT TOUCH THE BULB OR
SHADE.
- Have
students observe the container carefully and note any
changes that they see. It might help to add a little
smoke to the aquarium to help them see the
circulation.
(A few matches or incense sticks lit by the teacher,
then blown out and quickly dropped into the box will
work.)
-
Set
up should look like this image.
Assessment
/ Questions
- Using
the data
sheet provided,
have students answer the questions as prompted by their
observations. (See teacher answer sheet for
guidance with answers.)
- Challenge
the students to use their understanding of the water
cycle to explain a related phenomenon.
Example: Put 1/2
inch or so of sand or gravel in a resealable plastic
bag. Add 1/4 cup of water (color the water
blue for easier
visibility). Put the bag in a sunny window or under a
bright light. The students should be able to observe
evaporation, condensation, precipitation, and
infiltration
take place. They should identify that
transpiration is
not a part of the system.
- Ask
students to share examples of where they've
seen water
condensing and evaporating.
- In
the case of condensation, they should be able to
identify examples such as: water droplets forming
on the mirror and walls in a bathroom
where someone
has just taken a shower or bath. Ask the students
what the mirror and walls have in common
that would
allow the water droplets to form. (Water
droplets will form on objects that are
colder than
the vapor created by the shower or
bath.) Ask students why
water droplets won't form on the person or a heat
source, such as a radiator in the
bathroom. (These
objects are warmer than the water
vapor.) Other examples
include, eyeglasses that fog up on a
cold day when
you walk inside a heated room.
- In
the case of evaporation, they should be
able to provide
examples such as: a puddle that
disappears over time
on a warm, sunny day; or wet towels that dry out
in the sun.
- Review
the water cycle with students and the K-W-L
discussion
from the introduction. Fill in the
"L" portion of the
discussion.
- Have
the students diagram the water cycle or ask
them to construct
a concept map of the water cycle. The students should be
able to define the various stages. It is
recommended that
these activities be completed in pairs or
individually to
get a more accurate evaluation of student understanding.
Wrap
Up :
Re-engage the essential questions in a class discussion.
Students should now be able to answer these
questions in terms
of how water moves through the water cycle.
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