chapter 9 application of remote sensing
TRANSCRIPT
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APPLICATION OF
REMOTE SENSINGCG 505
Source: NASA
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Example Applications
visible / NIR / MIR - day only, no cloudcover
vegetation presence
geological mapping (structure, mineral /petroleum exploration)
urban and land use
phytoplankton blooms
meteorology (clouds, atmospheric
scattering)
DEM generation (stereo imagery)
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Thermal infrared - day / night, rate of heating /cooling
heat loss (urban)
thermal plumes (pollution)mapping temperature
geology
forest fires
meteorology (cloud temp, height)
Example Applications
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Active microwave - little affected byatmospheric conditions, day / night
surface roughness (erosion)
water content (hydrology) - top few cmsvegetation - structure (leaf, branch, trunk
properties)
DEM production (SAR interferometry)
Example Applications
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Pemetaan KedalamanObjective : To extract depth information from satellite data, and
to devise a fast and cost-effective alternative
for acquiring depth informationStudy Area : Pulau Tioman
Satellite remote sensing data
Landsat Thematic Mapper - band 1
Determination of depth information
Elimination of atmospheric & geometric errors
Computation of depth
Depth information in digital file
Production of Hydrographic Chart
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Depth information in digital file Production of
Hydrographic Chart
Digital File of Depth Information Automatic Generation of Hydrographic Cha
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Objective : To extract sea bottom information from satellite data and
to devise a fast and cost-effective alternative
for acquiring sea bottom information
Study Area : Langkawi
Determination of sea bottom features
Elimination of atmospheric & geometric errors
Formation of depth invariant index for sea bottom features
Classification of sea bottom features
based on depth invariant
Pemetaan Dasar Laut
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Product from Sea bottom feature mapping
Production of Sea bottom features Plan
Sea bottom featuresinformation is vital for :
navigational hazards
monitoring
dredging operation
exploration
offshore engineering
fisheries application
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Water Quality
Objective : To map water quality and determine suspended sediment
from satellite data
Study Area : Straits of Klang
Satellite remote sensing data
Landsat Thematic Mapper - band 1
Automatic Production of SSC Maps
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Objectives : To develop a suitable methodology for mapping
coastal features and land cover using multi-temporal
ERS-1 SAR satellite data
Study Area : Kuala Terengganu & Baram, Sarawak
Wave Spectra Analysis
Detection of Oil Slicks
Mapping of Natural & Artificial Features
Modeling for Vegetation Backscattering
Modeling Shallow Water Bathymetry
Radar Remote Sensing for Land and Coastal
Applications
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Objective : Identifying & analysing biomass for vegetation
mapping
Study Area : Raub, Pahang
Data from Red and Infrared Bands ofLandsat-5 TM and NOAA AVHRR Satellites
Computation of Vegetation Indices
Correlation of index to ground biomass
Vegetation Index Mapping
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Automatic Generation of Sea Surface Temperature
off coastal waters surrounding Peninsular Malaysia
SST is one of the prime
input into analysis of
fisheries / marine
research.
SST can be associated
with pelagic fish
species, hence, offers
a powerful
forecasting tool indeep sea fishing
industries of Japan and
Nordic countries.
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Biomass
Estimation Mapover study area
JERS-1 SAR
data over Sg.Pulai, Johore
Mangrove
forestsegmented
from SAR data.
Field verification of
calculated biomass
Retrieval of
treeparameters for
model
generation
Figure 1 : Measurement of in-situ data for biomass
obsevation.
Figure 2 : Determination of mangrove patches using
specific segmentation algorithm.
Figure 3 : Corrected image of JERS-1 SAR
(Synthetic Aperture Radar ) of study area.
Figure 4 : Biomass estimation map over study area.
Figure 5 : Survey of the study area carried out
jointly with Johore Forestry Department.
Global Rainforest Mapping Activities in Malaysia: Radar
Remote Sensing For Forest Survey and Biomass Indicator
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Phytoplankton sampling at
the time of satellite pass in the study area.
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Ocean colour mapping
(NOAA satellite)
Phytoplanktondistribution of
Kedah waters
(Landsat
image )
Seagrass
distribution in
Kedah waters
( Landsat image )
Derived sea-grass (a)and ocean colour (b) covering Langkawi island
Ocean colour and seagrass mapping from satellite
remotely sensed data for fisheries application
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Spectral Signature: Surface
Surfaces dont reflect allwavelengths equally. They tendto absorb certain wavelengths,while reflecting others.
The percentage of reflectanceacross the ElectromagneticSpectrum that a surface reflectsis called its spectral signature.
Spectral signatures can be
affected by the time of year,weather, and environmentalfactors.
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Spectral Signature: Water
The spectral signature for water
exhibits moderate reflectance inthe visible portion of theElectromagnetic Spectrum, butplunges to almost nothing in theNIR.
In images displaying NIR, waterappears black because of itslow reflectivity in the NearInfrared.
Blue0.4um-0.5um
Green0.5um-0.6um
Red0.6um-0.7um
Near Infrared (NIR)0.7um-1.2um