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World Natural Environments
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Introductory concepts
Earth-sun relationships Geographic grid Map use
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Earth-sun relationship
Significance: seasonal distribution of solar radiation general circulation of atmosphere & oceans Spatial distribution of climate regions & vegetation types
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Plane of the ecliptic
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Axial Inclination
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Axial Parallelism
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2. Geographic grid Significance: Provides system for locating features
Longitude provides basis for time zones
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Meridians of Longitude
Measures angular distance east or west Reference point is the prime meridian through Greenwich, England Values range from 0 – 180o Longitude is the x in an (x,y) coordinate pair
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Parallels of Latitude Measures angular distance north or south
Reference point is the equator Values range from 0 – 90o Latitude is the y in an (x,y) coordinate pair
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Latitude / Longitude Usually measured in degrees, minutes, seconds (e.g. 90o 30’ 36”) 60 seconds / minute 60 minutes / degree so, 3600 seconds / degree May be expressed in decimal degrees 90o 30’ 36” = 90.51o
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(-x, y) (x, y) (-x, -y) (x, -y) Where x = longitude and y = latitude
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3. Map use Uses of maps: Aids to location, navigation
Portray spatially distributed information
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Thematic maps Isopleth maps Choropleth maps:
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Isopleth maps Constructed from point data
Extrapolated to lines or areas Displays continuous data
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Choropleth maps Constructed from area-based data
Boundaries of areas may be natural or man-made (defined) Displays discrete data
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Exercise 1
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