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GEOG2750%20Earth%20Observation%20

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Semester 1: Earth Observation of the Physical Environment Louise Mackay ... 5 practical worksheets contributing 5% each to the final module mark ... – PowerPoint PPT presentation

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Title: GEOG2750%20Earth%20Observation%20


1
GEOG2750 Earth Observation GIS of the Physical
Environment20 Credit Level 2 Module
  • Louise Mackay Steve Carver
  • Module Information
  • See also
  • http//www.geog.leeds.ac.uk/courses/level2/geog275
    0/index.html

2
Module Outline
  • Runs Semester 1 2.
  • Semester 1 Earth Observation of the Physical
    Environment Louise Mackay
  • Semester 2 GIS of the Physical Environment
    Steve Carver
  • Two complimentary technologies for monitoring
    understanding the Earths physical environment

3
GIS Aims
  • On completion of semester 2 students should have
  • Knowledge of the use of GIS across a range of
    applications in physical geography including
    terrain analysis, hydrology, landscape evaluation
    and environmental assessment
  • Familiarity with the use and application of the
    ArcGIS package and
  • Knowledge of environmental data sources, skills
    in the interpretation of spatial environmental
    data and an awareness of specific problems and
    issues relating to data quality, spatial data
    models and methods of interpolation.

4
GIS Objectives
  1. Identify principles and functional issues
    pertaining to physical geography applications of
    GIS
  2. Examine and review specific application areas
    where GIS is a useful tool
  3. Investigate techniques provided by GIS which have
    particular relevance to physical geography
    applications and problem solving and
  4. Identify and address problem areas such as data
    sources, modelling, error and uncertainty.

5
Overall Learning Outcomes
  • On completion of this module students should be
    able to
  • Demonstrate a clear knowledge and understanding
    of the key concepts concerning the application of
    Earth observation and GIS to problems in physical
    geography
  • Critique and evaluate the applicability of Earth
    observation and GIS in relation to physical
    geography applications and
  • Demonstrate a high level of skill in the
    application of Earth observation GIS software
    to the solving of environmental problems.

6
Dates Times
  • GIS Semester 2
  • 10 x 1hr lectures, Monday 10-11am, Geography
    Lecture Theatre
  • 10 x 2hr practicals, Tuesday 3-5pm or Friday
    9am-1pm, Textiles G34 Computer Lab

7
Module Assessment
  • Semester 2 - GIS
  • 5 practical worksheets contributing 5 each to
    the final module mark
  • 1 x 1hr exam (short answer) at the end of the
    semester (2 questions from 5) contributing 25 of
    module mark
  • Overall assessment based on
  • 10 Practicals 50 of final module mark (5 x
    Earth Observation 25 done already last
    semester)
  • 2 exams 50 of final module mark (Earth
    Observation 25 done already last semester)

8
GIS Syllabus Semester 2 (Weeks)
  • 14. Introduction to GIS for environmental
    applications
  • 15. Spatial Temporal variability and
    environmental data
  • 16. Error Uncertainty
  • 17. Interpolation of environmental data
  • 18. Principles of grid-based modelling
  • 19. Terrain modelling the basics
  • 20. Reading week
  • 21. Terrain modelling applications
  • 22. Hydrological modelling
  • 23. Environmental assessment
  • 24. Making Decisions

9
Lecture 11Introduction to GIS for
environmental applications
  • Outline
  • what makes physical geography applications of GIS
    different?
  • environmental science and management
  • the role of GIS?

10
What makes physical geography applications of GIS
different?
  • The natural environment is
  • extremely complex
  • highly variable (space and time)
  • complicated further by human action
  • Understanding of natural systems
  • very basic
  • multiple approaches to natural science

11
From this
to this
12
Spatio-temporal variation
  • Range of variability over a range of spatial and
    temporal scales
  • variation depends on the scale of observation
  • e.g. vegetation (species, community, ecosystem)
  • sliding scale to represent both spatial and
    temporal variability
  • i.e. space from infinitesimal (zero) to infinite
  • i.e. time from the instantaneous to for ever

13
Spatio-temporal scales of operation
  • Variety of spatial and temporal scales
  • micro scale - meso scale - macro scale
  • e.g. Hydrology
  • Micro runoff plots, infiltrometer, hillslope
  • Meso sub-catchment, headwaters, reach
  • Macro whole catchment, region, watershed
  • now - sec - min - day - year - century - etc.
  • e.g. Climatology
  • Seconds Wind speeds
  • Minutes Incoming solar radiation
  • Day Anabatic/katabatic winds
  • Year Annual temperature variation
  • Millennium Glacial/interglacial periodicity

14
Complexity
  • Complex nature of environmental systems makes
    possibility of realistic modelling seem remote
  • Frustrated by lack of understanding
  • e.g. influence of human activity
  • Variations in complexity
  • most GIS applications model only 1 or 2 processes
    with assumptions/simplification

15
Question
  • How can sampling strategies be matched to
    spatio-temporal scales?

16
Sampling theory
  • Sampling spatial processes
  • the sampling frequency needs to be small enough
    to record local variations without undue
    generalisation of spatial pattern but coarse
    enough so as to avoid data redundancy
  • Sampling temporal processes
  • in order to record variations in temporal
    processes sampling frequency needs to be about
    half the wavelength of the process to avoid
    measurement bias and too much detail
  • Sampling dependent on process(es) operating

17
Sampling theory
DEM
Cell size 1
Cell size 2
1 wavelength
Rate
amplitude
Time
18
Question
  • How do we choose appropriate sampling frequencies?

19
Advantages of GIS
  • GIS is good at
  • handling spatial data
  • visualisation of spatial data
  • integrating spatial data
  • framework for
  • analysis and modelling
  • decision support

20
(dis)Advantages of GIS
  • GIS is not so good at
  • handling temporal data
  • visualisation of temporal data
  • integrating spatial and temporal data
  • framework for
  • analysis and modelling of time dependent data
  • volumetric analysis
  • uncertainty

21
GIS alone is not enough
  • Integrated systems
  • limited off-the-shelf spatial analysis and
    modelling
  • framework for developing better integrated
    systems
  • GIS - image processing systems
  • GIS - modelling systems
  • GIS - statistical software
  • facilitated through
  • specialist programming languages (e.g. AML and
    Avenue)
  • universal programming languages (e.g. Java and
    Visual Basic)
  • access to source code (e.g. GRASS)

22
Integrated systems
  • Combined (symbiotic) systems
  • Example
  • NERC/ESRC Land Use Programme (NELUP) decision
    support for land use change in UK
  • GRASS GIS
  • models hydrological (SHE), agricultural
    economics and ecological
  • Graphic User Interface (GUI)
  • Spatial Decision Support System (SDSS)

23
NELUP
24
Conclusions
  • The physical world is complex and our
    understanding simple
  • environmental data is highly variable
  • implications for GIS applications
  • GIS has important role to play in environmental
    science and management
  • handling and analysing spatial data
  • problems with temporal data

25
Practical
  • Spatial variability in environmental data
  • Task Investigate the spatial variability in
    terrain datasets and determine the effects of a)
    sampling strategy, and b) resolution on the data.
  •  Data The following datasets are provided for
    the Leeds area
  • 10m resolution DEM (110,000 OS Profile data)
  • 50m resolution DEM (150,000 OS Panorama data)
  • 10m interval contour data (110,000 OS Profile
    data)

26
Practical
  • Steps
  • Display both elevation datasets in ArcMap and
    look for visible differences - do these result
    from differences in sampling strategy or
    resolution or both? Use the IDENTIFY tool to
    interrogate the images.
  • Calculate the slope (gradient) from both the 10m
    and 50m data is there any striping in the
    slope data and what might this be due to? (use
    the slope tool in ArcMap or ArcGRID to calculate
    slope)

27
Learning outcomes
  • Familiarity with scale issues especially
    resolution and sampling in relation to spatial
    variation in environmental data
  • Experience/practice in use of analysis and
    display functions in ArcMap
  • Familiarity with OS terrain model products

28
Useful web links
  • NELUP web site
  • http//www.ncl.ac.uk/wrgi/wrsrl/projects/nelup/nel
    up.html

29
Next week
  • Spatial and temporal variability and
    environmental data
  • general characteristics of environmental data
  • environmental data sources
  • toward integrated databases
  • Practical Using Digimap to access OS data
    products
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