Module 11 Flashcards

1
Q

Terrain Analysis

A

terrain analysis is the process of using topographic data to derive terrain
attributes

is the analysis and interpretation of topographic features through geographic information systems. Such features include slope, aspect, viewshed, elevation, contour lines, flow, upslope flowlines and dowslope flowlines

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2
Q

DEM’s and Terrain Analysis

A

▪ digital elevation models emerged in
photogrammetry in the 1950s and since then, digital
point elevation data in the form of DEMs have
gradually replaced contours on topographic maps
and have become the main source of topographic
data
▪ supported by DEMs and other forms of digital
topographic data, digital terrain analysis takes the
place of manual terrain analysis – it is now one of the
most powerful tools in GIS for environmental
modeling and landscape visualization

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3
Q

__________ are the most widely used digital terrain model due to their simplicity and ease of computer implementation

A

digital elevation matrices

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4
Q

TINs

A

TINs use the vector model to represent terrain by using contiguous, nonoverlapping triangle facets that consist of planes linking the three adjacent elevation points in the network

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5
Q

Breaklines in TIN

A
▪ breaklines are line features or boundaries of
area features with or without height
measurements
▪ hard breaklines represent a discontinuity in the
slope of the surface, capturing abrupt changes in
the surface (eg road cuts, streams)
▪ soft breaklines do not change the local slope of a
terrain surface, but mark an important feature of
the terrain (eg, coastlines, study area boundaries)
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6
Q

DEM vs TIN

A

DEM=RASTER
-▪ DEMs can be readily integrated with remotely sensed environmental data – there
are well-established algorithms for digital image processing that can be used to
process DEMs
▪ however, DEMs can have erroneous sinks or depressions generated during their
production as a result of data input errors, insufficient input data, interpolation
effects, or by rounding and averaging errors

TIN=VECTOR
-▪ vector contours are simply digitized contour lines and are only used in GIS for data
capture and visualization, not for analysis
-Triangular irregular networks (TIN) have been used by the GIS community for many years and are a digital means to represent surface morphology. TINs are a form of vector-based digital geographic data and are constructed by triangulating a set of vertices (points). The vertices are connected with a series of edges to form a network of triangles.

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7
Q

DEM sink

A
▪ a sink is a cell or a set of spatially connected cells in a DEM that are surrounded by
higher elevation values
-▪ while there are real sinks in nature
(sinkholes, quarries), they tend to be
rare
-▪ sinks are particular problems for
hydrologic research, creating false
drainage patterns – a DEM that has its
sinks removed is known as a
hydrologically correct DEM
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8
Q

Removing Sinks in DEMs(2)

A

1.▪ sinks can be removed or ‘filled’ by raising the values of cells in depressions to the value of the depression’s spill point, the cell with the lowest value surrounding the
sink
▪ a smoothing filter (eg, moving average) is a common method of removing sinks on a large scale, but it may also remove real sinks, as well as raise the average
elevation of the terrain and create artificial flat areas

2.▪ an alternative approach to sink filling is
using the ‘Topo to Raster’ tool in ArcGIS,
which couples the DEM to a watershed
model, showing where the lakes and rivers
are located
▪ since rivers and lakes are natural sinks, the
algorithm knows to keep them, while DEM
sinks found far from the lakes or rivers are
assumed to be error sinks and are filled

MOST DEMs are not hydrologically correct and therefore contain spurious sinks

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9
Q

the ____ instrument onboard the Terra satellite is capable of generating DEM quality elevation data using stereo pairs of imagery
– the product has a horizontal resolution of 30m and a vertical resolution of 15m

A

ASTER

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10
Q

InSAR

A

▪ InSAR acquires multiple radar images of the terrain to extract 3-D information, with
accuracies as good as traditional photogrammetric techniques

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11
Q

LiDAR

A

LiDAR produces masspoints (an x,y location with an elevation) – the space between
points can then be interpolated to produce a continuous elevation surface

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12
Q

Terrain Data Sources(3)

A
  1. ASTER
  2. INSAR
  3. LIDAR
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13
Q

____ ____ _____(DEMs) provide a basis for extracting terrain-related attributes or features, and can be divided into primary and secondary attributes (2)

A

Digital Terrain Models

▪ primary attributes: are mainly used to describe the size, shape, and other surface attributes of hillslopes, catchment boundaries, and stream channels – ie, elevation, slope, aspect, profile and plan curvature, flow accumulation, drainage network, flow length, upslope area…

.Secondary attributes:
▪ secondary attributes are used to characterize the spatial variability of specific environmental processes occurring in the landscape
– they tend to be applied to quantify the influence of topography on the spatial distribution and abundance of
water, soil, fauna, and flora

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14
Q

for both DEMs and TINs, _____
is calculated using the normal
vector approach

A

slope

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15
Q

Aspect

A

– an important factor that controls the spatial distribution of solar irradiance (thus affecting evapotranspiration), and flora and fauna distribution and abundance

  • ▪ like slope, aspect is calculated for each DEM grid cell or every triangle facet in a TIN based on the normal vector
  • ▪ aspect is usually described as a compass direction, measured clockwise in degrees from 0 (due north) to 360 (due north), using the following rule
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16
Q

Aspect: Give me direction= N,E,S,W

0-22.5=

157-202=

247-292=

67.5-112=

A

North

South

West

East

17
Q

Terrain Profile

A

a terrain profile is a 2D diagram that depicts the landscape in vertical cross-section
-Terrain point attribute grouped with unique symbol, Terrain point attribute with graduated color ramp, and Terrain point elevation with graduated color ramp.
-▪ terrain profiles typically include a vertical
exaggeration, a scaling factor that emphasizes
vertical features which might be too small to
identify relative to the horizontal scale

18
Q

Vertical Exaggeration

A

a scaling factor that emphasizes
vertical features which might be too small to
identify relative to the horizontal scale

19
Q

in GIS, the method for producing a terrain profile based on a digital terrain model generally involves:(5)

A
  1. finding all intersections of a specified profile line with sides of the triangles in a TIN or with grid cells in a DEM
  2. calculating the horizontal position along the profile line of every intersection and its elevation through interpolation
  3. drawing the x-axis with its length equal to the horizontal distance of the profile line at the scale of the digital terrain model
  4. determining the height of the vertical axis according to the specified vertical exaggeration factor, and drawing the y-axis
  5. plotting the intersections in the diagram using their horizontal distances to the starting point of the profile line as x coordinates and their elevation x vertical exaggeration as y coordinates
20
Q

surface curvature

A

is the amount by which a surface deviates from being flat
▪ there are many measures of surface curvature – GIS typically uses plan and profile
curvature

21
Q

▪ there are many measures of surface curvature – GIS typically uses ___ and ____
curvature

A

▪ while slope influences the overall rate of movement downslope and aspect determines the direction of flow

1.plan: plan curvature has an effect on convergence
and divergence of flow
-curviture to the middle on sides like a flat paper vs paper bent at centre into a tube
—-__—-

2.profile:profile curvature affects flow acceleration and
erosion/deposition rates
-curviture to the middle from top and bottom increasing slope
—–_____

22
Q

Positive curvature indicates

Negative curvature indicates

A

the surface is upwardly convex (eg, hills and ridges)
__—__

the surface is upwardly concave (eg, depressions and
valleys)
—__—

—-a flat surface has 0 curvature

23
Q

Convex

Concave

A

hills

depressions/valleys

24
Q

Hydrological Terrain Analysis:

Flow Direction

Flow Accumulation

Flow Length

A

Flow Direction: is fundamental in hydrological analysis because in order to determine where a landscape drains, it is necessary to determine the direction of flow for each location in the landscape

flow accumulation: refers to how much water accumulates from upstream areas and contributes to overland flow – basically calculated as the number of upstream cells that flow into each cell based on their flow direction
▪ locations having high flow accumulation values are the areas of concentrated flow (usually stream channels), while locations having 0 accumulation correspond
to the pattern of ridges

Flow length: is the distance or weighted distance along a flow path, either upstream or downstream, and used to calculate the length of the longest flow path
▪ flow length is an important input to surface runoff models, primarily through the calculation of time of flow concentration within a catchment

25
Q

when multiplied by the average rainfall in each cell during a given storm, the flow accumulation value represents the amount

A

of rain that flows through each cell or the

amount of rain that fell in the upslope area of each cell (assuming that all rain becomes runoff)

26
Q

Drainage Network

A

▪ by selecting cells with a flow accumulation value greater than some threshold value, a network of high-flow cells can be generated, known as the drainage
network
▪ the threshold is important – a higher threshold value will only choose the largest flow accumulation zones, resulting in a low drainage density; a lower threshold will include smaller flow accumulation zones, resulting in a higher drainage density

27
Q

Topographic Wetness Index(TWI) is derived through the following procedure on a depressionless DEM(6)

A
  1. derive the flow direction from the DEM
  2. derive the flow accumulation (𝑓𝑎𝑐𝑐) from the flow direction
  3. calculate the upstream catchment area:
    𝐴 = 𝑓𝑎𝑐𝑐 + 1 × 𝑑^2
  4. calculate the specific catchment area as:
    𝐴𝑠 = 𝑓𝑎𝑐𝑐 + 1 × 𝑑
  5. calculate the slope (𝜃) from the DEM
  6. calculate the topographic wetness index
28
Q

Describe the Topographic Wetness Index(TWI)

A

▪ TWI serves as a physically-based index quantifying and estimating the location of zones of surface saturation
▪ in a catchment, areas having similar TWI values are considered to have a similar hydrologic response to rainfall when their other environmental conditions are
the same

29
Q

Stream Power Index(SPI)

A

is a measure of the erosive power of overland flow

▪ as the specific catchment area and slope increase, the amount of water contributed by upslope areas and the velocity of water flow increase, hence stream power index and erosion risk increase
▪ averaging (eg, focal/neighbourhood smoothing) is commonly used to reduce the
high spatial variability seen in both data sets

30
Q

Sediment Transport Index(STI)

A

accounts for the effect of topography on soil erosion

▪ STI can be used to characterize the
processes of erosion and deposition, and to
present the effect of topography on soil loss

31
Q

Visibility Analysis

A

▪ visibility analysis involves determining what is visible from a location or a set of locations along given lines of sight or across an entire area – useful in landscape planning for assessing scenic quality and the impact of new developments on the landscape
▪ “which areas can be seen from a forest fire observation station that is 20m high?”
▪ “which land areas are visible from a planned scenic road, and how often can those areas be seen from the road?”

32
Q

View Shed analysis

A

▪ viewshed analysis expands the line-of-sight analysis to cover every possible point in the study area as a target, which is useful to define the areas of the terrain
surface that are visible from a viewpoint or a set of viewpoints, thus allowing users to calculate what they can see from a given set of vantage points

▪ through viewshed analysis, it is possible to
determine what would be visible from planned developments, how visible a particular spot on the landscape is,