Transcript Weather slides

Weather
Understanding
& Predicting
Weather Conditions
Understanding and
predicting weather
conditions
Four Elements of Weather
This ELEMENT measures
heat in the air
This ELEMENT measures
water vapor in the air
This ELEMENT measures
the force of air pressing down
This ELEMENT measures
the speed of air moving
Weather Tools
Thermometer
Anemometer
A thermometer measures the
amount of heat in the air in
degrees
A barometer
measures the weight of the air
Rain Gauge
An anemometer measures the
velocity or speed of air
movement in miles or
kilometers
A rain gauge measures the
levels or amount of
precipitation in inches or cm.
Barometer
• Wind is caused by the
uneven heating of the air.
• Air moves from places of
high pressure to one of
low pressure.
• Wind is measured by an
anemometer. It is
measured in miles per
hour.
• Wind direction is
determined using weather
vane.
• Temperature is a measure of
the amount of heat in the air.
• Determined by how fast the
molecules in the air are
moving. The faster the
molecules move, the warmer
the temperature is.
• Temperature is measured
using a thermometer. It is
measured in degrees.
Air Pressure
• Refers to the weight of
the air pushing down on
the surface below.
• LOW PRESSURE signals
stormy weather.
• HIIGH PRESSURE
signals clear conditions.
Humidity is the measure
of water vapor in the air.
Water vapor is water
that has evaporated
after being heated
Warmer climates have
higher
humidity.
Why do you think this
happens?
Chances of precipitation
Increase as the humidity does. Why do
you think this happens?
Hygrometer
Water Cycle
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The only way that Earth can be
continually supplied with fresh
water. The heat from the sun
is the most important part of
the water cycle.
This heat soaks up water from
the oceans, lakes, rivers, trees
and plants in a process called
evaporation.
As the water mixes with the air
it forms water vapor. As the
air cools, the water vapor
forms clouds. This is called
condensation.
Most of the water is
immediately returned to the
seas by rain. The rest of the
water vapor is carried inside
clouds by wind over land
where it rains or snows.
Rain and melted snow is
brought back to the oceans by
rivers, streams, and run-off
from glaciers and water
underground. This is the
process of collection.
NOW IT STARTS AGAIN
• Evaporation: Evaporation is when the sun heats up
water in rivers or lakes or the ocean and turns it into
vapor or steam. The water vapor or steam leaves the
river, lake or ocean and goes into the air.
• Do plants sweat?
• Well, sort of.... people perspire (sweat) and plants
transpire. Transpiration is the process by which plants
lose water out of their leaves. Transpiration gives
evaporation a bit of a hand in getting the water vapor
back up into the air.
•Condensation: Water vapor in the air
•gets cold and changes back into liquid.
•This is called condensation.
•Precipitation: Precipitation occurs when so much water has
condensed that the air cannot hold it anymore. The clouds get
heavy and water falls back to the earth in the form of rain, hail,
sleet or snow.
• Collection: When water falls back to earth as
precipitation, it may fall back in the oceans,
lakes or rivers or it may end up on land. When it
ends up on land, it will either soak into the earth
and become part of the “ground water” that
plants and animals use to drink or it may run
over the soil and collect in the oceans, lakes or
rivers where the cycle starts
all over again.
Precipitation Forms
When snow falls it is below freezing in
the upper and lower levels of the
atmosphere as well as on the
ground
When sleet falls it is warm in the upper
atmosphere, but dips below
freezing near the ground forming
icy pellets
When rain falls warms up as the icy
crystals fall from the clouds
(melting them), and stays warm all
the way to the ground
When hail falls, it is warm at the upper
levels and then turns colder.
Updrafts cause water droplets to
be lifted and cooled, forming
chunks of ice. This can happen in
a thunderstorm.
or sleet
CLOUDS
Cloud Chart
Cloud Group
Cloud Height
Cloud Types
High Clouds = Cirrus
Above 18,000 feet
Cirrus
Cirrostratus
Cirrocumulus
Middle Clouds = Alto
6,500 feet to 18,000
feet
Altostratus
Altocumulus
Up to 6,500 feet
Stratus
Stratocumulus
Nimbostratus
Low Clouds = Stratus
Clouds with Vertical Growth
Cumulus
Cumulonimbus
Special Clouds
Mammatus
Lenticular
Fog
Contrails
•Most common high cloud.
•Thin, feathery clouds
•Associated with fair weather
•Indicate rain or snow in the
hours ahead
•Uniform, smooth grayish low clouds
•Cover entire sky, blocking direct sunlight
•resemble fog that doesn't reach the ground
Thick blankets of cloud which produce light rainfall.
•Fluffy and white
•Flat bottom
•Form from warm, moist air rising rapidly
through a cooler layer
•Usually predict FAIR WEATHER until…..
they get larger and darker in the bottom
Nimbocumulus Clouds
Could hold as much as
110,000 tons of water!
•THUNDERCLOUDS
•Largest of all clouds
•Dark, threatening clouds
•Often produce thunder and lightning
Can reach heights of
11 miles!
FIRST
NEXT
LAST
THIRD
FRONTS and changing weather
Boundary between two air
masses of different
temperature and humidity.
•storm with lightning and thunder.
•produced by a cumulonimbus cloud,
•usually gusty winds,
•heavy rain and
•sometimes hail.
Needs moisture,
unstable air and lift.
moisture to form clouds
and rain,
unstable warm air
that can rise rapidly.
Finally… lift.
from fronts,
sea breezes
or mountains.
Violently rotating column of air that descends from a thunderstorm.
No other weather phenomenon can match the fury and destructive power of tornadoes.
They can destroy large buildings and lift 20-ton railroad cars from their tracks.
•Weather forecasting involves the
observers and meteorologists and
the work of machines.
•Computers make forecasts more
accurate, and weather satellites
orbiting the earth take photographs
of clouds from space.
•Forecasters use these observations
from ground and space, along with
formulas and rules based on
experience of what has happened in
the past, and then make their
forecast.