Celebrate Earth Day with Your Library - Possible Slides

Celebrate Earth Day with
Your Library
Possible Presentation Slides

Note to Presenter
Feel free to pick and choose the slides you
would like to use for your presentation.
There are many great online resources and
hands on activities which you can use to
enhance your program at
http://www.starnetlibraries.org/earth-day/.

Get the App
GLOBE Observer
Make observations that complement
NASA satellite observations to help
scientists studying Earth and the global
environment.
Take photographs of clouds and record
sky observations and compare them with
NASA satellite images.

Get the App
Enter your email and Earth Day
referral code: earth2017 (case
sensitive) to create account.
Note: GLOBE Observer app Team will
send an approval email with a
password to Login.
Now you are ready to go!
Issues:
globeobserverhelp@lists.nasa.gov

Referral Code
It is important that you use the referral code
“earth2017” when first setting up your login so
NASA can make a map of all the contributions
from the STAR_Net community.

Science Behind Clouds
Share what you already now about clouds.

Clouds and Satellite Comparison
“We seek to remind people that clouds are
expressions of the atmosphere’s moods, and
can be read like those of a person’s
countenance.”
-Manifesto of the Cloud Appreciation Society

Observing Clouds
• any observation is a good observation and tells
us something about the environment and
science around us
• no clouds: clear sky, means energy is easily
entering and leaving our system
• clouds: normal process
• Obscuration: means we understand what might
affect local conditions or that something might
be happening that is out of your view

The Atmosphere
The Earth's atmosphere is an extremely thin
sheet of air extending from the surface of the
Earth to the edge of space. The Earth is a
sphere with a roughly 13,000 km diameter;
the thickness of the atmosphere is about 100
km.
In this picture, taken from a spacecraft
orbiting at 300 km above the surface, we can
see the atmosphere as the thin blue band
between the surface and the blackness of
space. If the Earth were the size of a
basketball, the thickness of the
atmosphere could be modeled by a thin
sheet of plastic wrapped around the ball!

Where Do Clouds Come From?
Water in the atmosphere exists in three
main phases (solid, liquid, and gas). It
changes phase depending on temperature
and pressure. Like most other gases that
make up the atmosphere, water vapor is
invisible to the human eye.
Unlike most other gases in our
atmosphere, under the right conditions
water vapor can change from a gas into
solid particles or liquid drops. Though we cannot see it,
there is still water (vapor)
present in a clear blue sky.

How do Clouds Form?
If temperatures are above freezing,
water vapor will condense onto small
particles (dust, smoke, salt, etc.) in our
atmosphere, as water droplets. The
small particles are known cloud
condensation nuclei (CNN). Without
them clouds would not form above -
40°C.
If temperatures are below freezing, as
they are at high altitudes, tiny ice
crystals will mostly form instead.

What are Clouds?
When a large number of
water drops or ice crystals
are present, and they
scatter enough light for us
to see them, they form
visible clouds.
At any given time, over half
of Earth’s surface is
covered by clouds.

Why Collect Cloud Data?
One of the most interesting features of Earth, as seen from space, is the ever-
changing distribution of clouds. They are as natural as anything we encounter
in our daily lives. As they float above us, we hardly give their presence a
second thought. And yet, clouds have an enormous influence on Earth’s
energy balance, climate, and weather.
Even small changes in the abundance, location, or cloud type can impact
Earth’s climate and weather. This is why collecting data on clouds is important.

Clouds and Weather
Clouds can help us predict weather.
Clouds can also tell us something about air
temperature, water, and wind up in the sky.
During the day a cloudy sky will make the
temperature warmer.
At night a clear sky will make temperatures
cooler. Clouds also bring us rain.
Dry air aloft
Moist air aloft, wind
perpendicular to contrail

Role of Clouds in the Water Cycle
The water on Earth is always on
the move, changing from liquid to
vapor and back to liquid and snow
and ice near the poles and
mountains. The process is called
the water cycle, or hydrologic
cycle.
Clouds are a key element of our
Earth’s hydrologic cycle, bringing
water from the air to the ground
and from one region of the globe
to another.

Clouds and Earth’s Energy Budget
Clouds also affect how much sunlight is reaching the ground and
how much heat is escaping back to space. Understanding the
clouds helps us better understand climate.
Clouds are the key regulator of the planet’s average temperature.
Some clouds contribute to cooling because they reflect some of the
Sun’s energy – called solar energy or shortwave radiation – back to
space. Other clouds contribute to warming because they trap some
of the energy emitted by Earth’s surface and lower atmosphere –
called thermal energy or longwave radiation.

Importance of Contrail Data
Contrails, or condensation
trails, are the linear clouds
formed when a jet aircraft
passes through a portion of
the atmosphere having the
right moisture and
temperature conditions. The
relationship is between
contrails and clouds is a
current investigation area
for scientists.

Your Measurements Can
Help Scientists
1) Understand how cloud climatology
may be changing
– Human observers can identify
qualitative aspects (e.g. cloud type
clues) that automated sensors cannot.
2) Provide ground-based data on
contrails
– Human observers can see small
features (e.g. short-lived contrails) that
are not visible from satellite.

Your Measurements Can
Help Scientists
3) Verification and improvement of
automated remote sensing
From the bottom: Blue sky provides great
contrast
4) Improve interpretation of
satellite observations of
Earth’s energy balance
From the top: Varied surface confounds
detection
Hint: Observations timed to coincide with satellite imagery provide
useful comparisons, for scientists, and for you!

How to Observe: Sky Color
Sky color is an indication of the amount of aerosols in the atmosphere. Aerosols tend
to scatter all wavelengths of light, making the sky look more white. Deep blue suggests
very few aerosols. A milky sky suggests there are lots of aerosols.
Goal: to observe the bluest part of the sky.
Note: Sky color can only be observed from a clear
section of sky, with no clouds in view.
Tips:
• Turn your back to the Sun
• Look at the sky halfway between the horizon and
straight up (45°)
• Pick the shade that most closely matches your
sky
• You want to match the color of the sky, not the
clouds, so if it’s too cloudy you may not to be
able to observe sky color

How to Observe: Sky Visibility
Sky visibility is an indication of the amount of the aerosols close to the surface
of the ground. The more aerosols there are, the more hazy will appear.
Look at a landmark in the distance
Try to use the same landmark every time
Tip:
It can be helpful to take a picture of your
sky day-to-day to notice the difference
between visibility observations. In
addition, the clearest sky for your area will
be seen just after a front or a storm moves
through your area.

How to Observe: Cloud Details
at Each Height
At each level (high, mid, and low)
observers will identify the following:
• Cloud Type(s)
• Cloud Cover
• Cloud Visual Opacity
• Contrails are reported in the high cloud
section.

How to Observe: Cloud Type
Clouds can be defined by:
• Their shape
• The cloud base altitude
• Weather they are
producing precipitation
The Cloud Triangle is a
useful memory device.

How to Observe: Cloud Type by Shape
3 main cloud shapes are:
Cumulus (Puffy): Made
of water, cumulus clouds
can be associated with
fair weather. They are
usually not very tall and
they are separated from
each other with lots of
blue sky in between.
Stratus (Layered):
Made of water. These
clouds can be found
from Earth’s surface to
2,000 m high. When
you see the Sun’s disk
through them, the
edges look sharp.
Cirrus (Wispy): Made of
ice crystals and are
considered “high clouds”,
forming above 5,000m.
They generally indicate fair
to pleasant weather. The
reason for the long tail is
primarily due to high speed
winds at high altitudes.

How to Observe: Cloud Cover
You will estimate the total cloud cover of the whole sky and at each level (high, mid,
and low levels).
It may be helpful to divide the sky in 4 quadrants (North, South, East, and West) and
estimate cloud cover in each, then take the average to get the whole sky value.
Tip:
Observe the sky overhead, excluding the horizon. This can be done by:
observing above 14°,
or holding your arms out in a “V”, hands even with the height of the top of your head,
and observing between your hands,
or hold your fist out at arm’s length, even with the horizon; put your second fist on top
of the other; observe the sky from above the top of your second fist.

How to Observe: Visual Opacity
Tip:
If your shadow is well defined, a lot of sunlight is getting through the cloud above you, so the
cloud’s visual opacity would be transparent. As your shadow becomes more fuzzy, the cloud
would be considered more opaque.
Transparent: Thin clouds through which light
passes easily, and through which you can even
see blue sky. Note the milky bluish-whitish
appearance.
Translucent: Medium-thickness clouds that let
some sunlight through. There may be some
milky bluish-white near the edges, and a very
little bit of gray; but these clouds are mostly a
bright white.
Opaque: Thick clouds which do not allow light
to pass directly, although light can diffuse
through them. Clouds look gray. When these
clouds are in from of the sun, it is impossible to
tell where the sun is.
Transparent
Translucent
Opaque

How to Observe: High Level Clouds
High Clouds are those whose base is 5,000m to 13,000 m. Types
include cirrus, cirrocumulus, and cirrostratus. The clouds can be
either ice or water droplets, but are more often ice crystals. Water
clouds tend to have definite edges, while ice clouds are more
wispy. Persistent contrails (airplane trails of moisture that don’t just
disappear as the airplane passes) are high clouds as well.
NEVER look directly at the Sun!
With Halo
Cirrostratus Cirrus Cirrocumulu
s

How to Observe: Contrails
Count the number of each type; remember to report 0 if no
clouds are present
Short-Lived:
Contrails that form
short line segments
that fade out as the
distance from the
airplane that created
them increases.
Persistent Non-
Spreading: Remain long
after the airplane has left
the area. They form long,
generally straight lines of
constant width across the
sky. These contrails are no
wider than your index
finger, held at arm’s length.
Persistent Spreading:
Remain long after the
airplane has left the area.
They form long streaks that
have widened with time since
the plane passed. These
contrails are wider than your
index finger held at arm’s
length.

How to Observe: Mid-Level Clouds
These are generally clouds whose base is between 2,000 and 7,000m
altitude. Cloud types are altostratus or altocumulus, and are generally but
not always water clouds, depending on the atmosphere’s temperature and
other conditions at the cloud altitude.
Altostratus Altocumulus

How to Observe: Low Level Clouds
These are generally clouds made of water droplets whose base is
below 2,000m altitude. Low cloud types include stratocumulus,
cumulus, stratus, cumulonimbus, and nimbostratus. Fog can also be
put in this class because it is a ground-level stratus cloud. The tops
of cumulonimbus clouds can be high enough to form ice crystals.
Stratus Stratocumulus Cumulus

How to Observe: Low Level
Precipitating Clouds
Clouds that precipitate have names with nimbo prefix/suffix. Precipitation
can be in any form such as rain, snow, hail, etc. Cumulonimbus clouds
are known as thunderstorm clouds and are sometimes called anvil clouds
because of their shape. Nimbostratus clouds often bring steady, ongoing
precipitation.
Nimbostratus
Cumulonimbus
From afar From below

How to Observe: Determining Level of
Cumulus Clouds
Tip: for Cumulus (puffy) clouds, use fist/thumb/pinky finger strategy to
estimate cloud height.
High clouds (cirrocumulus)
appear comparable in size
to pinky finger held at
arm’s length.
Mid-level clouds
(altocumulus) appear
comparable in size to
thumb held at arm’s
length.
Low clouds
(cumulus) appear
comparable in size
to fist held at arm’s
length.

How to Observe: Determining Level
Stratus Clouds
Tip:
For stratus (layered) clouds, look for clues near the Sun.
NEVER look directly at the Sun!
Cirrostratus is the only cloud
type which can produce a
halo around the sun or
moon. The halo will have all
the rainbow colors in it.
Altostratus will produce a
thinly veiled Sun or moon,
and will often be darker in
appearance, a medium gray
color. The sun looks dimly lit
behind these clouds.
Stratus will usually
be very gray and
often very low to the
ground. They tend to
cover a lot of the sky.

How to Observe: Surface Conditions and
Measurements
Surface Conditions (Required): Define the surface
conditions of your observation site.
Tips:
A pond would be an example of standing water.
Leaves on tress refers to the majority of the deciduous trees
around your observation site.
Surface Measurements (Optional):
• Air Temperature
• Barometric Pressure
• Relative Humidity

Understand Data:
Context from Satellite
From above, satellite
imagery provides information
about clouds and
characteristics on mid and
high levels that may be
obscured from the ground.
With satellite imagery, you
can see where your local
weather fits into global
patterns and phenomena.
The NASA Worldview site provides contextual information on cloud cover from the MODIS
instrument on the Terra and Aqua satellites. Satellite imagery for March, 6th 2015.

NASA Resources
• NASA Earth Observatory feature article on
clouds
• NASA Fact Sheet: The Importance of
Understanding Clouds
• Imagery from Space: Explore NASA
Worldview or Visible Earth, great resources
for interpreting satellite imagery.

Let’s go identify some clouds!
When you first open the app, you will need to
create a login by entering an email address
and an optional referral code, and the system
will email you a password. It is important that
you use the referral code earth2017 when first
setting up your login so NASA can make a
map of all the contributions from the
STAR_Net community.

Celebrate Earth Day with Your Library - Possible Slides

More Related Content

What's hot (8)

Similar to Celebrate Earth Day with Your Library - Possible Slides (20)

More from NCIL - STAR_Net (20)

Recently uploaded (20)

Celebrate Earth Day with Your Library - Possible Slides

Editor's Notes