GIS exam Flashcards
(77 cards)
What is terrain
An area of land ground
A particular geographic area
Terrian impacts on the direction of the flow of water, the clarity of the signal received by mobile phones or equipment, the attractiveness of scenery
what are some common uses of DEMs?
Storage of elevation data for digital topographic maps in national databases
Creation of digital and analog orthophoto maps
Cut and full problems in road design and other civil or military engineering projects
3D displays of landforms for military purposes and for landscape design and planning
Analysis of cross-country visibility
Planning routes of roads, utilities, location of damns
Stat analysis and comparison of different kinds of terrain
Source data for derived maps, such as: aspect, profile curvature, shaded relief insolation, and hydrological and ecological modeling
Background for displaying thematic information or for combing relief data with thematic data such as soils, land use and vegetation
Providing data for simulation models of landscapes and landscape processes
what are digital elevation models (AKA DEMS)
A digital model of height (elevation or altitude) represented as regulatory or irregular spaced points/lines height values (VECTOR) –> Triangulated irregular Network (TIN) is how it is represented
A model of a physical surface the utilize cells of a grid as elevation through an arbitrary datum (RASTER) –> Elevation Lattice or Altitude matrices are used to represent
It is a representation of the bare earth
what are TINS (DEM)
-vector way of representing DEMs
-Developed by puecker et all to avoid data redundancy and create a more efficient system for computing slope from contour lines
-Vector polygon structure
-It is built by joining known point values into a series of triangles based on Delauney triangulation
what are some Methods of representing DEMs
Line data can represent contours and profiles, and critical features such as streams, ridges, shorelines, and breaks in slope
Altitude matrices are regular grid cells which represent elevation above a datum (above sea level) –> RASTER
Triangulated irregular Networks (TINs): connected triangular facets based on Delauney triangulation of irregularly spaced nodes or observation points –> VECTOR
what are altitude matrices (DEM) and some disadvan and advantages
raster way of representing DEM
Derived from remote sensing or interpolation from a grid of data points that are regularly or irregularly spaced
advantanges
-Good for calculating contours
-Excellent for generating derivative maps
-Easy to use and most available
-Provide fine spatial resolution
ASTER (advanced spaceborne thermal emission and reflection radiometer) global digital elevation model=30m interval
National and local DEMs = <5m resolution
Disadvantages
-Large amount of data redundancy in areas of uniform terrain
-Inability to adapt to areas of differing relief complexity without changing grid size
-Exaggerated emphasis along the axes of the grid for certain kinds of computations such as line-of-sight calculations
what are the three sets of record in Delauney triangulation
- The node list
-consists of records identifying each node and containing its coordinates, the # of neighbouring nodes, and the start location of the identifiers of these neighbouring nodes in the pointer list - The pointer list
-contain all the essential altitude information and linkages, so they are sufficient for many applications such as slope mapping and hill shading.
(node list does this too) - The triangle list
-For associating other attributes with the triangles, it is necessary to be able to
reference the triangles directly. Using a triangle list to associate each directed edge with the triangle to its right establishes this.
What does the Delauney triangulation allow (Diagram?)
A variable density and distribution of points to be used which reflects the changes in attribute values within an area
The structure model regards the nodes of the network as the primary units
The topological relations are built into the database by constructing pointers for each node to each of its neighboring nodes
The Neighbour list is sorted clockwise around each node, starting at north
A dummy node on the “reverse side” of the topological sphere onto with the TIN is projected represents the world outside the area modelled by the TIN
This dummy node assists with the describing of topology of the border points and simplify their processing
what information can you get from DEM models/what are DEM derivatives
Slope (landslide susceptibility)
Aspect (solar insolation, vegetation)
Catchment or dispersal area (Runoff volume, soil drainage)
Flow path (distance of water flow to point)
Profiles
Viewshed (visibility)
What are the slope and aspect in DEM
Defined as a plane tangent to the surface modelled by the DEM at any given point, and comprises of two components
Gradient/slope: the max change of altitude, measured in degrees; measure of gradient magnitude and influences ex flow velocity
Aspect; the compass direction of this maximum rate of change, measured in compass bearing (N, S); direction of flow, gradient direction
What are convexity and concavity in DEM
Convexity: rate of change of a slope expressed as a plan convexity and profile convexity
Concavity: negative convexity
what curvatures in DEM and what are the types
Profile curvature: indicated accelerated flow (convex) and areas with decreasing flow (concave); accelerated/slow flow
Tangential curvature: represents the area of convergent (concave) and divergent (convex) flow; convergent/divergent flow
Using directional filters to estimate slope and aspect
Derivate from the hypsometric curve are usually computed locally for each cell on an altitude matrix form data within a 3x3 cell kernel or “window” that is successfully moved over the map
Simplest finite difference estimates of gradient in the x direction at a point i,j is the maximum downward gradient
what is the DEM Zevenbergen and thrones method for calculating slope
Shows how these attributes and the concave and convexity are computed from a 6-parameter quadratic equation fitted to the data in the kernel
what is the DEM Horns method for calulcating slope in DEM
Uses all eight outer points of the window to determine optimal number of factors ?
what is view shed
everywhere that is visible from a specific point
what is - aspect: and trace one path
aspect- direction of the steepest downhill slope
trace one path: Follow aspect from cell to cell
how can you encode direction in DEM
use a DIRECTION GRID
Each cell in the direction grid contains information that indicated to which of the eight neighbours the poath goes next. This information is coded according to the followjing diagram
what is D8 algoritum for determining flow direction in DEM
Flow direction (FD): “steepest” neighbouring cell recieves flow
Only 8 possible directions
Cells connected together into local drain direction (LDD) netowkrs
Long linear flow lines
basically looks to neighbours and gives the steepest one the flow
what is upstream accumulation in DEM when calculating flow direction
Each cell is linked to a downstream neighbour in the LDD network
Follow all paths, accumulate cell count downstream
Result: number of cells upstream of the current cell that discharge through cells
What are the issues with DMS
- PITS !!
All neighbouring cells are higher
No outflow
Interpolation errors
Disrupt drainage topology
:cut through”: expand search and connect across pit
“fill up”: raise pit elevation until level with surroundings
-like a literal pit in a line where stuff gets suck in
What are some misc featues of DEM
Stream channels: cells with more than N upstream elements
Ridges: cells with only 1 upstream element (itself)
Catchments: all the cells that are upstream contributing elements for a particular output point
Divided by ridge lines
what is the wetness index in DEM and some difficulties with it
uses upstream accumulation and slope
-made by beven and kirkby
difficulties:
Slope, aspect depend on cell size
Streams are one cell wide
Accumulation done by simple gravity, no inertia
Dispersion, diffusion not modeled well
What are sources of geospatial data
portals that hold historical data (current to historical)
- Global Geospatial data repositories
- Federal geospatial data repositories
- Provincial geospatial data repositories
- Open-source geospatial data repositories
- Municipal (local) geospatial data repositories
6.Commercial geospatial data repositories - Themes geospatial data repositories
- Remote sensing data repositories
what are some GIS hardware considerations
In order to conduct and perform high end geospatial analyses you must consider more than just the tools a software offers or how to answer a question using those tools
1.Type of computer (personal, workstation, mainframe)
- CPU (speed, overlay procedures, input/output)
- memory (RAM vs ROM)
- Operating system (single person vs server based)
- Display (raster/vector)
- Input device (digitizing tablet vs screen digitizing)
- Output device (printers, scanners)
- Network environment (LANs)
- Storage (flash drives, clouds etc)