Wednesday, September 29, 2010

Data Sources and Management

1) Digital spatial data is common, inexpensive, and easy to use, but sometimes a digital raster graphic can show more information more neatly.

2) DOQs are digital ortho quadrangles, which are corrected and georeferenced photographic maps.  The corrections are to minimize distortion from camera tilt and terrain displacement.

3) The National Wetlands Inventory consists of wetland maps produced by the Fish and Wildlife Service.  Topographically Integrated Geographic Encoding and Referencing (TIGER) consists of demographic maps produced by the Census Bureau.  Land Use Land Cover (LULC) Data consists of land use/cover maps produced by the US Geological Survey (USGS) from aerial photography, while National Land Cover Data (NLCD) consists of land cover maps produced by the US Geological Service from satellite maps.

4) DEMs (Digital Elevation Models) are elevation data in raster format, created from ground and aerial surveys of original elevation measurements.  National Elevation Datasets (NEDs) are seamless rasters created by the USGS from merging the best DEMs.

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2a) The feature datasets are Basemap and Hydrology.

2b) The feature classes in the Hydrology dataset are NHDFlowline, NHDPoint, NHDWaterbody, and Watersheds.

2c) NHDFlowline is a line layer, NHDPoint is a point layer, and NHDWaterbody and Watersheds are polygon layers.

3a) Topoq24.shp is a vector data layer.

3b) Topoq24 is a shapefile.

3c) There is metadata associated with Topoq24.shp

3b) NHDFlowline is a geodatabase.

3c) There is metadata associated with NHDFlowline.

3d) Three keywords used to describe NHDFlowline are Hydrography, Stream/River, and Lake/Pond.

3c) The USGS Earth Science Information Center is the author of NHDFlowline.

4a) There is still metadata associated with the layer.

6b) The Canoga Park USGS_QD_ID is 34118_B5.

7) The DOQQ is black and white.

12a) The lacounty_lu01.shp no longer appears, because its original data source no longer exists.


Sunday, September 26, 2010

Coordinate Systems & Map Projections in ArcGIS








Map Projection Overview

I made six different world maps showing Washington, DC and Baghdad, Iraq, using six different map projections.  I chose to use six different cylindrical projections, two of which are conformal, two of which are equal area, and two of which are equal distance.  The two conformal map projections are the Mercator and Miller Cylindrical Projections.  The two equal area projections are the Equal Area Cylindrical and Behrmann Projections.  The two equal distance projections are the Equal Distance Cylindrical and Plate Carree Projections.  All six map projections exhibit considerable distortion in various ways.
            The Mercator and Miller Cylindrical Projections are conformal map projections because they preserve the correct angles of map objects.  It is thus easily possible to draw rhumb lines (lines that cross meridians), greatly helping with sea navigation, the original purpose of the Mercator Projection. The Mercator Projection does have considerable land area distortion, especially with increasing distance from the Equator.  For example, Alaska, Canada, Greenland, and Russia appear much larger than they really are, and Antarctica is enormous, because the distance between parallels increases as the distance from the equator increases.  The Miller Cylindrical Projection is an attempt to improve the Mercator Projection, by scaling the parallels of latitude by 2/5, and then multiplying them by 5/4 at the Equator to minimize distortion.  Thus, the Miller Cylindrical Projection is not truly conformal, because the angles change slightly, but it is descended from the conformal Mercator Projection, and is very similar.  Thus, the Miller Cylindrical Projection also exhibits many of the same distortions.  The distance between parallels still increases as distance from the equator increases.  Alaska, Canada, Greenland, and Russia are still larger than they really are, although not as large as in the Mercator Projection; the Miller Cylindrical Projection also shows more of the northern extremes of Earth.  However, Antarctica is truly monstrous; it was already too big in the Mercator Projection, and it looks twice as large in the Miller Cylindrical Projection.  For both projections, long range distance distortion is also a problem; Baghdad is essentially the same distance away from Washington, DC on both projections (8,415 miles and 8,413 miles, respectively), when Baghdad is actually 6,208 miles away from Washington, according to travelmath.com (which measures air miles and uses the great circle formula).  Thus, there is plenty of distortion on cylindrical conformal projections.  Yet the cylindrical equal area projections did not demonstrate to be any better.
            The Equal Area Cylindrical and Behrmann Projections are equal area projections because they preserve the actual area of the countries depicted, so the countries remain correct in size.  The distance between parallels decreases as distance from the equator increases, so Alaska, Canada, Greenland, Russia, and Antarctica seem compacted against the top and bottom edges of the projections.  Still, on both projections, Alaska, Canada, Greenland, and Russia appear to be the correct size, while Antarctica is still too big, though not as big as on the conformal projections.  Long range distance distortion is still a problem for both projections; Baghdad is 8,407 miles away from Washington on the Equal Area Cylindrical Projection, and 7,288 miles away on the Behrmann Projection.  The Behrmann Projection shows the most improvement in reducing distortion in general.
            Finally, the Equal Distance Cylindrical and Plate Carree Projections are equal distance projections because they maintain a consistent distance between all parallels and meridians.  Thus, there seems to be less distortion in terms of geographic coordinates, even though there is extensive distortion in other areas.  Far northern landmasses are larger than they should be, like with the conformal cylindrical projections, and Antarctica is still very large, like with the conformal and equal area cylindrical projections.  Long range distance distortion is significant, like with the conformal projections.  For instance, on the Plate Carree Projection, Baghdad is 8,415 miles away from Washington, which is basically the same distance measured on the Mercator, Miller Cylindrical, and Equal Area Cylindrical Projections.  Notably, on the Equal Distance Cylindrical Projection, Baghdad is only 4,218 miles away from Washington, or about half the distance measured on the other projections, and well short of the actual 6,208 air miles between Washington and Baghdad.  The Equal Distance Cylindrical Projection seems compacted horizontally, or taller and thinner than most maps, because there appears to be a relatively small distance between meridians, and a relatively large distance between parallels.  Conversely, the Plate Carree Projection maintains the same distance between parallels as between meridians, so that the latitude-longitude grid consists of squares, rather than rectangles.  The result is generally more balance to the shapes of and distances between landforms.
            I chose to create six world maps with cylindrical projections because I think their rectangular shapes look nice on rectangular websites and sheets of paper.  Yet all the cylindrical projections show distortions in terms of size, shape, and distance, some worse than others.  Overall, the Behrmann Projection shows the least distortion of any of the cylindrical projections I examined.  Because it is an equal area projection, all the countries and landmasses except for Antarctica have the correct size.  Shape is also mostly correct, except for Antarctica, while the northern areas do look somewhat compacted.  There is also less long range distance distortion on the Behrmann Projection, compared to all the other cylindrical projections; Baghdad is 7,288 miles away from Washington on the Behrmann world map, and 6,208 miles away on a globe. 

1) An ellipsoid is an irregular, imperfect sphere.  It is a mathematical surface defined by revolving an ellipse around its minor (polar) axis.  It approximates the surface of the Earth without topographic undulations.  On a two dimensional service, Earth is an ellipsoid.

2) Earth's imaginary network of intersecting lines of latitude and longitude is the graticule, and is a representation of a coordinate system.

3)  Magnetic North is where a compass points, while the North Pole is one of the poles of Earth's axis of rotation.

4) A datum is a three dimensional frame of reference (model of the earth) used to determine surface locations, defining the origin and orientation of latitude and longitude.  A datum consists of a specified ellipsoid and a set of surveyed coordinate locations specifying horizontal positions for a horizontal datum or vertical positions for a vertical datum on the surface of the Earth.  Cartographers develop datums through surveys and monument points.

5) A map projection is a transformation of coordinate locations from the curved surface of the Earth onto flat maps.

6) A developable surface is a surface without distortion when flattened on a plane.

7)  Lines of longitude run north-south on the graticule, converge on the poles, and mark angular distance east and west of the prime meridian.

8) The GRS80 ellipsoid is the best model of the Earth for North America, especially as the foundation for the North American Datum of 1983.

9) The Universal Transverse Mercator global coordinate system would be appropriate to use for developing and analyzing spatial data when mapping countries or larger areas, because there is minimal distortion within its mapped segments, which all have an equal width of 60 degrees of longitude .

10) Great circle distance is the shortest distance between any two points on the surface of a sphere.

Monday, September 13, 2010

Data Formats & Models

1) A data model is a set of rules/constructs used to describe and represent aspects of the real world in a computer.  The two types of data models are vectors and rasters.  Vectors use coordinate data to represent spatial information through points, lines, and polygons, while rasters represent spatial information through grids, where each grid cell has a value, and all grid cells together form an image. 

2) Topology is the study of geometric properties that do not change when the forms are bent, stretched or undergo similar geometric transformations.  Topology is important because it is necessary to represent vector data neatly and accurately, even though its forms usually are warped in some way.  Topological vector models also effectively represent adjacency, connectivity, containment, area definition, and contiguity.

3) A vector data model would be best for representing hillside slope, through a topographical map.  The vector data model effectively shows many contour lines, which is the best way to show elevation and slope.

4) In a raster data model, as cell dimension (the real-world area represented) increases, the level of detail decreases.

5) Four types of attribute data are nominal, ordinal, interval, and ratio data.  Nominal data is descriptive/categorical data, and can be image, such as of a building.  Ordinal data is ranked/ordered data, such as a bar graph ranking states by economic growth.  Interval data is ordered data, with absolute differences in magnitude and absolute zero, such as on a scale, where numbers are different based on their position on a scale.  The scale of a map is an example of interval data.

6) Two types of vector data file formats are shapefiles and coverages.

7) Two types of raster data file formats are grids and images.

8) It is not possible to select features in ArcCatalog.

9) The world.mdb dataset does not contain a feature dataset; it contains feature classes.
10) The feature classes are cities, countries, disapp_area, and world30.

11) Flight_path.lyr is a shapefile.

12) It is possible to add data to an ArcMap document by selecting Add Data from the File menu, or by dragging the data from an ArcCatalog window.

13) There are 699 features in the disapp_area feature class, according to the table window of the preview menu in ArcCatalog.

Tuesday, September 7, 2010

ArcGIS & Arc Map

 1) ArcGIS comes with ArcCatalog, ArcGlobe, ArcMap, ArcReader, and ArcScene.  We will mostly be using ArcMap and ArcCatalog.

2) It would be better to perform most data analysis and layer symbolization in data view because data view is more detailed.  Layout view is an overview; data view contains more information, and displays it more clearly.

3) Ways to obtain help for ArcGIS desktop include searching the ArcGIS Desktop Help datatabase and/or clicking the "What's This?" icon.

4) Attributes are linked to geographic features in the attribute tables for each map layer.

5) The file extension for an ArcMap document is .mxd.

6) One way to zoom in/out is to click on Zoom Data under View.  Another way to zoom in/out is to click on the zoom in/out buttons on the toolbar.

7) Three operations available in the context menu include Copy, Remove, and Open Attribute Table.

8)  If a check box next to a layer in the table of contents is gray, then that layer is scale-dependent.  It is necessary to zoom in to see the layer.

9) A large-scale map represents a small area, because it has a relatively large map-distance to actual-distance ratio.  A city map would be a large-scale map.  A small-scale map represents a large area, because it has a relatively large map distance to actual-distance ratio.  A world map would be a small-scale map.

10) A feature is a geographic object (such as a city) displayed in a layer.  A surface us a single, continuous expanse (such as an ocean) in a layer.

11) It is not possible to create project criteria using a GIS.

12) The minimum elevation of a city Earhart visited was 0 feet, or sea level (in New Orleans).  The maximum elevation was 1,045 feet (in Tucson).  I determined these values by examining the attribute table of the "Cities Earhart Visited" layer.

13) The approximate distance from Dakar to Assab is 6,901 miles.  To figure out the approximate distance, connect the points using the measure tool, or add the relevant distances in the attribute table.

14) It is possible to figure out the names of the cities on the map by hovering over them with the mouse arrow, or by clicking on them with the identification tool.


Wednesday, September 1, 2010

3 Definitions and Uses of GIS, and 3 Similarities and Differences with Regular Maps

3 Definitions of GIS

Definition #1

"Geographic Information Systems (GIS) is a system of hardware and software used for storage, retrieval, mapping, and analysis of geographic data." 

http://www.nwgis.com/gisdefn.htm

Definition #2

"Like the field of geography, the term Geographic Information System (GIS) is hard to define. It represents the integration of many subject areas. Accordingly there us no absolutely agreed upon definition of a GIS (deMers, 1997). A broadly accepted definition of GIS is the one provided by the National Centre of Geographic Information and Analysis:


a GIS is a system of hardware, software and procedures to facilitate the management, manipulation, analysis, modelling, representation and display of georeferenced data to solve complex problems regarding planning and management of resources (NCGIA, 1990)."

http://www.geom.unimelb.edu.au/gisweb/GISModule/GISTheory.htm

Definition #3

"(Geographic Information System) An information system that deals with spatial information. Often called "mapping software," it links attributes and characteristics of an area to its geographic location. It is used in a variety of applications, including exploration, demographics, dispatching, tracking and map making. Using satellites and aerial photography, the U.S. Geological Survey and other organizations have developed digital maps of most of the world. Unlike paper maps, digital maps can be combined with layers of information."

http://www.yourdictionary.com/computer/gis



3 Examples of GIS Use

Example #1

The US Department of Housing and Urban Development uses GIS as part of an online program to help Internet users locate Empowerment Zones and Renewal Communities.  Users simply type their address, zip code, and state, and the program will display the nearest EZs and RCs.

http://gis.cancer.gov/examples/federal.html

http://egis.hud.gov/egis/

Example #2

The US National Library of Medicine uses GIS as part of an online map called TOXMAP to help Internet users locate Toxic Release Inventory facilities Superfund National Priority sights.  The data comes from the Environmental Protection Agency.  TOXMAP displays all the sights at once, and users simply explore the map.

 http://gis.cancer.gov/examples/federal.html

http://toxmap.nlm.nih.gov/toxmap/main/index.jsp

Example #3

The US National Institute of Justice uses a GIS program called Mapping and Analysis for Public Safety (MAPS).  The NIJ uses this program to develop crime maps, which can show crime trends, allowing users of these maps to find high-crime areas, and adjust resources and policies accordingly.  The NIJ publishes various maps and reports, available online. 

http://gis.cancer.gov/examples/federal.html

http://www.ojp.usdoj.gov/nij/maps/welcome.htm



Similarities between Maps and GIS

-Both maps and GIS represent data spatially.

-Both maps and GIS allow users to see considerable data all at once in an easy-to-understand format.

-Both maps and GIS allow users to analyze the data they contain to make decisions.



Differences between Maps and GIS

-Maps are simply spatial representations of data.  GIS produce maps, yet also stores data in map form as part of the software that produced the map in the first place.

-Not all maps are part of a GIS.  For example, some people can create maps using their own data, without GIS software, though this is becoming less common.

-GIS uses layers of data, which the user can display or hide, creating a custom map.  The GIS user can also zoom in or out of a GIS map.  Regular maps, on the other hand, are not customizable; they are a finished product that do not allow users to display or hide layers or change zoom levels.