17
Unit 3: Mapping the Earth’s Surface Royal Observatory at Greenwich, near London, marks the Prime Meridian, where east meets west.

Unit 3: Mapping the Earth’s Surface

  • Upload
    alaire

  • View
    60

  • Download
    0

Embed Size (px)

DESCRIPTION

Unit 3: Mapping the Earth’s Surface. Royal Observatory at Greenwich, near London, marks the Prime Meridian, where east meets west. OBJECTIVES Introduce reference systems used for locations on the Earth’s surface - PowerPoint PPT Presentation

Citation preview

Page 1: Unit 3: Mapping the Earth’s Surface

Unit 3: Mapping the Earth’s Surface

Royal Observatory at Greenwich, near London, marks the Prime Meridian, where east meets west.

Page 2: Unit 3: Mapping the Earth’s Surface

OBJECTIVES• Introduce reference systems used for

locations on the Earth’s surface• Describe the most important

characteristics of maps and the features of common classes of map projections• Interpret isoline maps.• Discuss contemporary developments in

geographic information science

Page 3: Unit 3: Mapping the Earth’s Surface

Locations on Earth• Latitude-parallels

• Longitude-meridians

• Prime Meridian

• Great Circles

Page 4: Unit 3: Mapping the Earth’s Surface

Latitude and Longitude

Page 5: Unit 3: Mapping the Earth’s Surface

Global Positioning System (GPS)Provides location (lat, long) and elevation using orbiting satellites based on a corrected geoid (the reference ellipsoid of the Earth). The correction is made due to gravity variations as shown on the maps below.

GPS monitor on a tripod can be used to measure small movements of the Earth from earthquakes, plate tectonics. Source: http://celebrating200years.noaa.gov/transformations/ht_mod/image6.htmlSource: http://en.wikipedia.org/wiki/Geoid

Page 6: Unit 3: Mapping the Earth’s Surface

In a remote area, the GPS provides accurate location and elevation from 3 satellites.

Page 7: Unit 3: Mapping the Earth’s Surface

Map Projections• Cylindrical (A)

• Mercator (A)

• Conic (B)

• Planar

• Equal-area

Page 8: Unit 3: Mapping the Earth’s Surface

The Mercator Projection-Distortion greatest near the poles-Provides true and constant compass bearing-rhumb lines

Page 9: Unit 3: Mapping the Earth’s Surface

Planar gnomic projection: meridians converge at poles and straight lines follow great-circles

Page 10: Unit 3: Mapping the Earth’s Surface

Equal-area projection preserves relative sizes of continents;Interrupted form-not continuous, thus minimizes distortions

Page 11: Unit 3: Mapping the Earth’s Surface

The Robinson map projection• Compromise between area and shape distortion

• Shows whole globe; stretches poles into lines

Source: http://gothos.info/wp-content/uploads/2011/04/robinson.png

Page 12: Unit 3: Mapping the Earth’s Surface

Isarithmic (isoline) map showing contours of equal values (rainfall)• Like topographic (height) charts, reduces 3-D volumetric data onto

2-D map.

Page 13: Unit 3: Mapping the Earth’s Surface

Topographic contour maps showing horizontal map of isolines (A) and vertical cross-section of traverse line XY (B).

Page 14: Unit 3: Mapping the Earth’s Surface

Perspective sketch of coastal landscape (A) and corresponding topographic map (B).

Page 15: Unit 3: Mapping the Earth’s Surface

Geographic Information System (GIS)

• Computer-generated overlays• Query capabilities-

can ask questions of data (ie, where will I find the combined features A-I-1?)

Page 16: Unit 3: Mapping the Earth’s Surface

Remote Sensing• Satellite based• Aircraft based

• Ground based (radar, infrared)

Landsat image of the Los Angeles area showing vegetation (red), urban areas (blue-gray) and water (black). Vegetation mostly associated with higher terrain, notably the San Gabriel Mountains to the north of the city and the Santa Monica Mountains to the west.

Page 17: Unit 3: Mapping the Earth’s Surface

Remote sensing of the environmentActive systemsPassive systems

Electromagnetic spectrum (wavelengths of energy)

Earth orbiting satellites gather data used in: weather, climate, atmospheric pollution geology, hydrology, soil science and agriculture, biology, oceanography