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Applied Cartography and Introduction to GIS GEOG 2017 EL Lecture-1 Chapters 1 and 2

Applied Cartography and Introduction to GIS

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Page 1: Applied Cartography and Introduction to GIS

Applied Cartography and Introduction to GIS

GEOG 2017 EL

Lecture-1Chapters 1 and 2

Page 2: Applied Cartography and Introduction to GIS

What is GIS?

A Geographic Information System (GIS) is a computer system for capturing, storing, querying, analyzing and displaying geospatial data.

Page 3: Applied Cartography and Introduction to GIS

GIS Components

• Computer hardware• Software• People• Infrastructure

Page 4: Applied Cartography and Introduction to GIS

GIS Operations

• Spatial data input• Attribute data management• Data display• Data exploration• Data analysis• GIS modeling

Page 5: Applied Cartography and Introduction to GIS

What is Geospatial Data?

Geospatial data are the data describing both the locations and characteristics of spatial features, such as roads, land parcels, and vegetation stands on the Earth’s surface.

Page 6: Applied Cartography and Introduction to GIS

Geographically Referenced Data

The street network is based on a plane coordinate system. The box on the right lists the x- and y-coordinates of the end points and other attributes of a street segment.

Page 7: Applied Cartography and Introduction to GIS

Coordinate System

• Geospatial data are geographically referenced.

• Two spatial reference systems used in GIS are the geographic coordinate system and the projected coordinate system.

• Projection connects the two spatial reference systems.

Page 8: Applied Cartography and Introduction to GIS

Vector and Raster Data ModelsThe vector data model uses x-, y-coordinates to represent point features (a), and the raster data model uses cells in a grid to represent point features (b).

Page 9: Applied Cartography and Introduction to GIS

Vector-Based Overlay

A vector-based overlay operation combines spatial data and attribute data from different layers to create the output.

Page 10: Applied Cartography and Introduction to GIS

Raster-Based Overlay

• A raster data operation with multiple rasters can take advantage of the fixed cell locations.

Page 11: Applied Cartography and Introduction to GIS

Layers and Coordinate System

Two map layers are not going to merge spatially unless they are based on the same coordinate system.

Page 12: Applied Cartography and Introduction to GIS

Layers and Coordinate System

The top map shows the interstate highways in Idaho and Montana based on different coordinate systems. The bottom map shows the connected interstate networks based on the same coordinate system.

Page 13: Applied Cartography and Introduction to GIS

Geographic Coordinate System• The geographic coordinate system is the location reference

system for spatial features on the Earth’s surface. • The geographic coordinate system is defined by longitude

and latitude.

Page 14: Applied Cartography and Introduction to GIS

Longitude and Latitude

A longitude reading is represented by a on the left, and a latitude reading is represented by b on the right. Both longitude and latitude readings are angular measures.

Page 15: Applied Cartography and Introduction to GIS

Approximation of Earth’s Shape

• The simplest model is a sphere, which is typically used in discussing map projections.

• But the Earth is not a perfect sphere: the Earth is wider along the equator than between the poles. Therefore a better approximation to the shape of the Earth is a spheroid, also called ellipsoid, an ellipse rotated about its minor axis.

Page 16: Applied Cartography and Introduction to GIS

Earth FlatteningThe flattening is based on the difference between the semi-major axis a and the semi-minor axis b.

Page 17: Applied Cartography and Introduction to GIS

Datum

• A datum is a mathematical model of the Earth, which serves as the reference or base for calculating the geographic coordinates of a location.

• A shift of the datum will result in the shift of positions of points.

Page 18: Applied Cartography and Introduction to GIS

Map Projection

• A map projection is a systematic arrangement of parallels and meridians on a plane surface.

• Cartographers group map projections by the preserved property into conformal, equal area or equivalent, equidistant, and azimuthal or true direction.

• Cartographers also use a geometric object (a cylinder, cone, or plane) and a globe (i.e., a sphere) to illustrate how to construct a map projection.

Page 19: Applied Cartography and Introduction to GIS

Different Map Projections

Page 20: Applied Cartography and Introduction to GIS

Aspect and Projection

Page 21: Applied Cartography and Introduction to GIS

Map Projections

NENW

SESW

Page 22: Applied Cartography and Introduction to GIS

Common Map Projections

• Transverse Mercator

• Lambert conformal conic

• Albers equal-area conic

• Equidistant conic

• Web Mercator

Page 23: Applied Cartography and Introduction to GIS

Projected Coordinate Systems

• The Universal Transverse Mercator (UTM) grid system

• The Universal Polar Stereographic (UPS) grid system

• The State Plane Coordinate (SPC) System

• The Public Land Survey System (PLSS)

Page 24: Applied Cartography and Introduction to GIS

UTM ZonesUTM zones range from zone 10N to 19N in the conterminous United States.

Page 25: Applied Cartography and Introduction to GIS

UTM Zone

A UTM zone represents a secant case transverse Mercator projection. CM is the central meridian, and AB and DE are the standard meridians. The standard meridians are placed 180 kilometers west and east of the central meridian. Each UTM zone covers 6° of longitude and extends from 84°N to 80°S.