Chapter 9: External energy fuels weather and climate

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Last updated 11:53 PM on 3/15/26
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69 Terms

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weather is a _ process

Short-term

  • Thunderstorms, tornadoes, hurricanes, floods

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Climate is a _ process

Long-term

  • Glacial advance/retreat droughts, ocean circulation changes

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_ powers geological disasters

energy from Earth’s interior

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Example of Earth’s energy powering geological disasters

Solar radiation

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Some energy comes from

Earth, Moon, Sun tides

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The Sun’s electromagnetic radiation

  • Radio waves through visible, X-rays to gamma rays

  • Visible light: 434% of light at surface

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Solar radiation: reflected/absorbed amounts vary with

Latitude

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What is the average latitude ration

30/70

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Net heating on the

Equitorial belt

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Net cooling at

Polar regions

  • Heat transfer form equator to poles

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Circulation patterns determine

Weather and climate

  • Orbit, energy transfer to poles

  • Rotation and gravity

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_ raises Earth’s surface temperature

Greenhouse effect

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Solar radiation has _ wavelength

Short

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Excess heat re-radiated has _ wavelength and is absorbe dby

Long

  • Absorbed by greenhouse gases

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Albedo is the direct reflection of

Solar radiation

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_ increases albedo and why

Ice cover, keeps poles cold

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_ decreases albedo and why

Liquid water, accelerates melting

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The Hydrologic cycle steps

  1. Water evaporates from oceans plant transpiration

  2. Vapour condenses

  3. Gravity returns water to the oceans

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Vapour condenses: falls as

Precipitation

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Gravity returns water to oceans: continuously operating as a

Distillation and filter system

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¼ solar energy drives

water evaporation

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Water has the _ of all solids and liquids except ammonia

Heat capacity

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Water has the _ of all liquids at Earth’s surface temperatures

Heat conduction

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Water has the highest _ (liquid/gas)

Latent heat of vaporization

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Water has the second highest _ (liquid/solid)

Latent heat of fusion

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Water has the highest dielectric constant of all liquids meaning it keeps

Ions apart, maintains solutions

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By volume the atmosphere is 0 to 4% what

Water vapour

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humidity is

Amount of water vapour in the air

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Saturation humidity is the

Maximum vapour content

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Relative humidity is the

ratio of humidity and saturation humidity

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If temperature of air is lowered without changing humidity it will reach 100%

Relative humidity

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When relative humidity reaches 100%, excess water vapour condenses to liquid water and reaches a

Dew point

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Heat index is the

Temperature felt depending on relative humidity

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Stored or released energy is

Latent heat

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Low heat capacity of rock means it

Heats up and cools down quickly

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During the Winter

  • Land cools quickly

  • cool air sinks toward the ground

  • High pressure region

  • Ocean retains warmth

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During the summer

  • Land heats up quickly

  • Low pressure

  • Ocean warms slowly

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Atmosphere converts solar energy into

Wind

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_ moves heat around Earth

Atmospheric circulation

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Pressure decreased with altitude results in

Upward flow of air

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Convection: added heat increases

Upward flow

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Atmosphere is layered by

Temperature

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Lowest layer of the atmosphere is the

Troposphere

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Troposphere (temp and altitude)

temp decreases with altitude

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Tropopause

Temp decrease pauses

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Stratosphrere

Temp increases with altitude

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Stratopause

Temp increases pauses

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Mesosphere

Temp decreases with altitude

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Air pressure differences result in

Pressure differentials

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Pressure gradiant

Force air flows from high to low pressure

  • Equalize pressure differentials

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Isobar

Map line connecting point of equal pressure

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Wind

Horizontal air flow

  • Across isobars perpendicularly from high to low

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Closely spaces isobars indicates greater

Wind speed

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Coriolis effect

Force due to Earth’s rotation

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Northern hem: moving objects pushed

Starboard

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Southern hem: moving objects pushed

Portside

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Friction

Surface (ground,trees) resists flow

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Gradient, Coriolis, and friction determine

Wind direction

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Anticyclone

Circular isobars, middle isobar highest

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Anticlone: northern hem has _ winds

clockwise

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Anticlone: southern hem has _ winds

Counterclockwise

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Cyclone

Circular isobars, middle isobar lowest

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Cyclone: northern hem _ winds

Counter clockwise

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Cyclone: southern hem _ surface winds

clockwise

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Anticlone: air aloft_ and_ out at ground

sinks and flows

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Cyclone: ground air _and_ aloft

flows and rises

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Solar radiation at equator powers circulation of

Hadley cells

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Warm, moist air rises at

Intertropical Convergence Zone (ITCZ)

  • cools and rains in tropics

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Dry air picks up moisture along surface therefore

Many great deserts in this region

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