GIS Mid-Term Exam Vocab

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Last updated 11:25 PM on 4/7/26
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81 Terms

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What is spatial data?

  • Many different formats

  • Includes location information

  • Any information with a location attached to it.

Why is it special?

  • Multidimensional

  • Voluminous

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3 basis of classifying problems:

  • Scale or level of geographic detail

  • Intent or purpose

  • Time scale

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3 principles of spatial variation:

  • Proximity effects are key to representing and understanding spatial variation.

  • Issues of geographic scale and level of detail are key to building appropriate representation.

  • Different measures of the world co vary

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Positive spatial auto correlation

If the features that are similar in location are also similar in attributes.

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Negative spatial autocorrelation

Features that are close together in space tend to be more dissimilar in attributes than features that are further apart. (Checkerboard pattern)

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Zero autocorrelation

When attributes are independent or no definite neighbor.

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Discrete data

Real world features with well defined boundaries

ex. river, buildings, streets, ocean.

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Continuous data

Do not have well defined boundaries.

ex. elevation, rainfall, temp.

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Vector

Distance and direction from a location.

  • Vector data model represents discrete objects on the surface of the earth.

  • ex. roads buildings

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Raster

  • Data models stores information in rows and columns

  • Attributes are represented in a cell.

Data types

  • continuous raster

  • discrete data

  • imagery

  • scanned map

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Remote sensing

Acquiring data with sensor systems that digitally record the interaction between electromagnetic energy and object.

Advantages of this:

  • consistency of the data

  • availability. of systematic global change

  • regular repeat cycles

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Metadata

Data about the data:

  • Primary collector of the data

  • Description about the content

  • Range of possible values

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Map scale

Scale of a map or data is the size of a map or data on a screen or printed paper relative to the size of it in real world.

ex. 1 cm on the map = x cm on the ground

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Geodatabase

Physical store for your GIS data.

3 types:

  • Personal geodatabase

Stored and managed in microsoft access data files and has maximum size of 2 GB. Can be read by multiple people, but only edited by one person at a time

  • File geodatabase

Stored in the file system folder, up to 1 tetrabyte. Supports multiple people editing different features classes or tables at the same time.

  • Multiuser geodatabase

Support versioning and replication, requires a data base management system. Found in larger organizations because it supports multiple viewers and editors.

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Feature classes

Thematic datasets representing geographic features, tables with a spatial field and and additional column.

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Feature datasets

Store spatially related feature classes in a common dataset for building topology.

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Mosaic dataset

Manages large collection of raster data which can be heterogenous in:

  • Format

  • Source

  • Data type

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Cartesian coordinates

  • 2 dimensional

  • expressed in ordered pairs

  • axes are perpendicular

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Datum

Coordinates without specified datum are vague.

  • How is it defined?

Using 1 of the spheroids

Using latitude and longitude

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Two most common spheroids:

  • GRS80

  • Clarke 1866

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Latitude (Parallel)

Gives you the extent a particular point lays north or south of equatorial plane.

  • Positive —> north of the equator

  • Negative —→ south of the equator

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Longitude

Gives the same east or west of prime meridian.

  • Positive —→ east of the prime meridian

  • Negative —→ west of the prime meridian

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NAD 1927

Obtained from ground based measurements. Is not geocentric center of the reference ellipsoid and center of mass of planet are no coincident.

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North American Datum 1983

3-D geometric datum

Further upgrade continuously operating reference stations NAD 83.

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3 main elements in coordinate systems:

  1. Name

  2. Units of measure

  3. Datum

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Geographic coordinate system

Spheroid (ellipsoid)

Angular units (degrees)

  • Difficulties

Units of degree cannot be used to measure distance on the ground, or the length of a line.

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Reference globe

Created by wrapping a grid of lines or graticules around a model of the earth.

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Projection

The process of converting a round globe into a flat map.

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Small and large areas:

Small areas: flat earth approximation works well.

Large areas: flat earth introduces distortion which causes errors.

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Scale factor

The amount of distortion when the surfaces of a spheroid is projected onto a plane is defined by scale factor (k).

k = distance on the projection / distance on ellipsoid

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2 types of distortions:

  1. kp = along parallel

  2. km = along meridian

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3 types of projection:

  1. Equidistant - preserving distance along meridian.

  2. Equal area - area preserved

  3. Conformal - shape preserved

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Distortion

  1. Shape *conformal

Feature outline look the same on map as they do on the earth.

  1. Area *equal area

The size of feature on a map is the same relative to its size on the earth.

  1. Distance *equidistant

Line on map has same relative distance with the line on the earth.

  1. Direction *azimuthal

Useful for navigation

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Developmental surfaces

A geometric shape that can be flattened without being distorted (cone, cylinder, plane)

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Point of tangency

A plane touches the globe at a single point.

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Secant

Line of intersection between the globe and the surface.

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Cylindrical

Touches globe along a line called a tangent, or it can pass through the globe and intersect along 2 secants

Meridians straight, meridians and parallels intersect at right angles

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Conic

Created by setting a cone over a globe and projecting light from the center of the globe onto the cone.

Contacts the globe along a single tangent.

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Standard parallel

Line of latitude in conic or cylindrical projection where projection surface touches globe.

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Central meridian

A line along which the developable surface is cut and flattened into a plane.

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Transverse mercator

Cylinder touches the sphere along a meridian. A conformal map projection good for north-south extending areas.

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State plane coordinate system

Relies on imaginary flat reference surface with cartesian axes.

Calculates easier

Has zones and is a standard map projections within U.S.

Conformal projection

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UTM coordinate system

conformal projection

divides earth into 60 zones, each zone is 6 degrees

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3 primary requirements of georeferencing are:

  1. unique - only 1 location associated with a given georeference.

  2. Shared meaning - meaning is shared among all users.

  3. persistent through time - addresses change.

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Geocoding

Matching of an address with its corresponding geospatial location.

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Baton geocoding

Multiple addresses can be plotted at the same time and mapped as a point feature class.

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Address locator

Rules for interpreting addresses list of standard street components snap shot of reference data.

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Reference data

Snapshot of geographic data with address information.

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Georeferencing

Process of registering your source imagery to a reference image or vector GIS layer. Defining location to your unknown spatial reference data using map coordinates and assign the coordinate system.

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Target data

Geoferenced raster or a vector feature class that resides in the desired map coordinate system.

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Source data

Data with unknown coordinate system.

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Polynomial transformation

Uses least square fitting algorithm order of polynomial.

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Spline

True rubber sheeting

  • Optimizes for local accuracy but not global accuracy.

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Root mean square error

The difference between where the from point ended up as opposed to the actual location that was specified to point position.

RMSE: Describes how consistent the transformation is between links.

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Attribute tables

Spatial data store more than just their spatial properties. Non-spatial information about spatial features make up the attribute table.

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Different types of attributes

  1. Nominal data

  2. Ordinal data

  3. Interval data

  4. Ratio data

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Attribute join

Linking two or more tables. Can only be preformed if 2 tables have a field in common called as key.

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One-to-one

Single record is linked to another single record.

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Many-to-one

Many records in an attribute table is joined to 1 record from another table.

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For making queries:

  • If and is used, then BOTH must be true

  • If or is used, then either may be true.

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Boolean operators

Used to evaluate pairs of conditions.

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Spatial analysis

Finding distributions and pattern of features.

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Spatial distribution

Finding spatial distribution of something.

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Overlay

Two or more layers, overlay analysis is needed.

To find locations that are suitable for particular use or are susceptible for some risk.

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Map overlay

Combines two or more layers to create a new output feature class containing information from both.

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Geoprocessing

When two or more functions are applied together to solve a specific problem.

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Types of overlay:

  1. Point-in polygon

Use to assign polygon attributes to points.

  1. Line-on polygon

Use to assign polygon attributes to lines.

  1. polygon-on polygon

New spatial data is created with features and attribute table.

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Union

Combines and keeps all features.

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Intersect

Combines and keeps common features.

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Dissolve

Eliminates all of the attributes in the table except the dissolved one.

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Buffer

Constructs polygon areas within a specified distance of features.

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Merge

Combines 2 features classes of the same type into a new combined feature class.

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Near

Calculates distance between the input features and the closest feature in another layer or feature class.

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Append

Places features from 1 feature class into a existing feature class of the same type.

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Tagged image file format (TIFF)

Geotiff tags are supported. Supports black and white + gray scale

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Joint photographic experts (JPEG)

A standard compression technique for storing full color and gray scale images.

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Portable network graphic (PNG)

Provides a well compressed lossless compression for raster files.

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Local operations

Examines raster by cell. Achieved using map algebra.

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Zonal operations

Compute results for blocks of contiguous cells that share the same value.

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Global operations

Produce results that are true of the entire layer such as mean value.

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Euclidean distance

Operation assigns to each cell its distance from the closest source cell.