Revolution Rotation Declination (Tilt of Earth’s Axis) Seasons Time Zones Insolation and its...
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Transcript of Revolution Rotation Declination (Tilt of Earth’s Axis) Seasons Time Zones Insolation and its...
• Revolution
• Rotation
• Declination (Tilt of Earth’s
Axis)
• Seasons
• Time Zones
• Insolation and its variation Sunrise over the Earth. Source: http://ajorbahman.blogspot.com/2011/02/third-of-russians-think-sun-spins-round.html
Unit 4: Sun-Earth Relationships
OBJECTIVES• Examine the Earth’s motions relative to
the Sun• Demonstrate the consequences of the
Earth’s axis tilt for the annual march of the seasons• Introduce the time and spatial
variations in solar radiation received at surface locations
Revolution of the Earth around the Sun
• Perihelion-closest to Sun Jan. 3rd
• Aphelion-farthest from Sun July 4th
• Distance differences from Sun do not influence amount of solar
energy received significantly
Earth revolves around the Sun in an elliptical path. Earth and Sun are not drawn to scale, and the orbit’s elongation is highly exaggerated for clarity.
Declination of the Earth’s Axis• Constant tilt of 23.5 degrees• Provides seasons
Video shows misconceptions about the cause of the seasons. http://www.youtube.com/watch?v=iMEfYLvxioc
Solar altitude-Sun’s height above the horizon
• Vertical (90o) Sun is at the equator on equinoxes
• Vertical Sun is at the Tropic of Cancer on summer solstice
• Vertical Sun is at the Tropic of Capricorn on winter solstice
World’s Time Zones
Why are the boundaries not straight lines?Why are the Prime Meridian, International Dateline significant?
Source: http://www.colourbox.com/vector/clocks-in-people-head-vector-invitation-card-vector-3095601
Intensity of Sunlight
Reception of solar radiation at different latitudes showing direct, indirect rays
Source: http://nsidc.org/cryosphere/frozenground/what_affects_fg.html
Relationship between solar noon altitude and daylight hours
Daylength (left axis) and noon solar altitude (right axis) at 45° north latitude. These factors work together in producing pronounced seasonality at middle and high latitudes. Notice also how the pace of change in both is much greater near the equinoxes than near the depths of summer and winter.
Spatial distribution of insolation at top of the atmosphere as percentage of global average
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Seasonal and spatial variation in solar radiation reaching the top of the atmosphere as a percentage of the global average. The latitude axis is scaled to acount for shrinking area at higher latitudes. Compare with patterns of the previous figures to see how solar position modulates the effect of daylength.