Rotates on its axis Revolves around the Sun Changing Sun ...

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1 Earth motions Rotates on its axis Revolves around the Sun Seasons—Result of constant axial tilt Changing Sun angle Changing Sun angle Changing length of daylight

Transcript of Rotates on its axis Revolves around the Sun Changing Sun ...

Page 1: Rotates on its axis Revolves around the Sun Changing Sun ...

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Earth motions

•Rotates on its axis•Revolves around the Sun

Seasons—Result of constant axial tilt

Changing Sun angle •Changing Sun angle •Changing length of daylight

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Special days Solstice—Sun's vertical rays are located at the Tropic

(23½º latitude) • June 21-22 • December 21-22

Equinox Sun’s vertical rays located at the Equator Equinox—Sun s vertical rays located at the Equator (0o latitude)• March 21-22• September 21-22

Figure 16.17Figure 16.16

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Heat is always transferred from warmer to cooler objects

Mechanisms of heat transfer • Conduction• Convection

R di ti ( l t g ti di ti ) • Radiation (electromagnetic radiation)

Figure 16.21

Figure 16.19 Figure 16.3

Air is a mixture of gases

Major components of clean, dry air • Nitrogen (N) – 78%• Oxygen (O2) – 21%• Argon and other gases • Argon and other gases • Carbon dioxide (CO2) – 0.036% – absorbs heat

energy from Earth

Water vapor Aerosols Ozone Ozone

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Atmospheric pressure variation

Figure 16.5

with altitude

Figure 16.7

TroposphereSt t hStratosphere

Mesosphere Thermosphere

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Daily maximum and minimum are measuredOther values calculated from these

• Daily temperature range• Daily mean temperature • Monthly mean temperatureMonthly mean temperature• Annual mean temperature• Annual temperature range

Line of equal temperature Divides map into areas

warmer than that temperature and areas cooler than that temperatureM ith i th t t diff f Maps with isotherms use constant difference from one isotherm to the next

Often colored for ease of understanding