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Velvet Dowdy
ESP
Grade 11
Water, Oceans, and Atmosphere
Earth Science
The Hydrologic Cycle
• Evaporation
• Transpiration
• Condensation
• Precipitation
The Earth’s Water
• 97.2% Ocean
• 2.14% Ice Caps and Glaciers
• 0.61% Surface Water
• 0.005% Soil moisture
Earth’s Atmosphere
Earth has an atmosphere for 3
reasons
1.Volcanic history
2.Mass of the planet
3.Amount of radiation from
the sun
Atmosphere
• Troposphere
• Stratosphere
• Mesosphere
• Thermosphere
• Ionosphere
• 90% of our atmosphere is in
the troposphere
• 99% of the atmosphere is
below the ozone layer
Earth’s Seasons
• Any planet that is tilted on its
axis will have seasons
• As the planet orbits about the
sun, the angle at which solar
radiation hits areas of the planet
will change—hence seasons
Atmospheric Benefits
The surface of the Earth is
warmer than it would be in
the absence of an
atmosphere because it
receives energy from two
sources: the Sun and the
atmosphere.
In the absence of an
atmosphere the Earth
would average about 30
Celsius degrees (about 50
Fahrenheit degrees) lower
than it does at present. Life
(as we now know it) could
not exist.
The surface
of the Earth receives
nearly twice as much
energy from the
atmosphere as it does
from the Sun.
The atmosphere radiates
because it has a finite
temperature, not because it
received radiation. When the
atmosphere emits radiation, it
is not the same radiation as it
received from the sun.
Driving forces of Air
Motion
•Convection Currents
•The earth’s rotation
Global Circulation Patterns
Cooler, dense air from the poles
pushes warmer, moister, less
dense air from the equator
upward. This air moves toward
the poles and cools.
Ocean Currents Affected
by
• Wind
• Density
• Earth’s rotation
• Earth’s surface and under
water features
Water oceans and atmospheres (earth science)

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Water oceans and atmospheres (earth science)