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APPLICATIONS IN
CONSERVATION OF
MANAGEMENT OF FISH
FAUNAL DIVERSITY
•
•
•
•
•

INTRODUCTION
REMOTE SENSING – DEFINITION
PROCESS OF REMOTE SENSING
TYPES OF REMOTE SENSING
RS IN AQUACULTURE DEVELOPMENT &
MANAGEMENT
• APPLICATION OF RS IN AQUACULTURE
• CASE STUDY
• CONCLUSION
• The major problem currently faced by world
fisheries and aquaculture management challenges
large geographic areas, including inland
areas, coastal zones and open oceans.
• As a result, remote sensing (from fixed coastal
locations, aircraft and satellites) has been used to
provide a large range of observation data to support
fisheries and aquaculture management, which
complement and extend data acquired from in situ
observations.
• “The science and art of obtaining information
about an object, area or phenomenon through the
analysis of data acquired by a device that is not in
contact with the object, area or phenomenon
under investigation”
• The devices are sensors mounted on satellites or
aircraft, or are installed at fixed coastal locations, that
measure the electromagnetic radiation (EMR) that is
emitted or reflected by features of the earth’s
surface, and which then convert the EMR into a signal
that can be recorded and displayed as either numerical
data or as an image.
• The full range of wavelengths of electromagnetic energy is
often referred to as the electromagnetic spectrum and classes
of wavelengths are often called spectral bands.
Active- own source
Passive – reflected EMR

Scanning - motion
Non scanning - fixed

Imaging – 2 dimensional
image
Non imaging –
1dimensional image
Optical and radar remote sensing systems are widely
used.
• Optical: These images are intuitive to interpret, but cloud
cover can limit their availability.
1. Visible and infrared – Sensors can provide land
cover and land use information for inland fisheries
applications, ocean condition data such as
chlorophyll-a and suspended sediment
concentration, bathymetry and sea surface
temperature (SST), and data to support coastal zone
fisheries and aquaculture management.
2. Light detection and ranging (LIDAR) – An airborne
system that can provide precise elevation
data, usually for small areas. When combined with
detailed visible and infrared optical imagery, this can
be used for land cover and topography mapping, for
1. Imaging radar – Images can contain unique
information compared with optical images, such as the
flooded status of vegetation or surface roughness of a
waterbody, but it typically can determine fewer land
cover classes than optical data.
2. Radar altimeter – Can be processed to provide
information on sea surface height, surface
currents, waves and winds.
1. Sea surface temperature :
• Advanced Very High Resolution Radiometer (AVHRR)
sensors on the National Oceanic and Atmospheric
Administration (NOAA)
• The National Aeronautics and Space Administration
(NASA) Moderate Resolution Imaging Spectroradiometer
(MODIS) sensors on board the Earth Observing System
(EOS) Aqua and Terra satellites
• NOAA’s Geostationary Orbiting Earth Satellites (GOES)
that are geostationary over the Western Hemisphere
• Selecting and acquiring data provides some information on
obtaining SST products from these satellites.
2. Ocean colour
• Ocean colour refers to obtaining information about
the ocean using optical sensors, including
parameters such as concentration of chlorophylla, which is a measure of primary productivity, and
total suspended matter (TSM), which is related to
turbidity.
• The International Ocean Colour Coordinating
Group (IOCCG) provides a good summary of the
current and future availability of ocean colour
sensors.
• Oceansat-1 (India)
3. Ocean salinity:
• Passive radar detects the low levels of emitted
microwave radiation from the earth’s surface. The
data have very coarse spatial resolution, meaning
that they are not generally used for fisheries and
aquaculture applications.
• Launched in 2011, the joint Argentina and the United
States of America Aquarius satellite provides monthly
maps of global changes in ocean surface salinity with
a resolution of 150 km, showing how salinity changes
from month to month, season to season, and year to
year at a global scale.
• European Space Agency Soil Moisture and Ocean
Salinity (SMOS) satellite.
• Mapping coastal aquaculture and fisheries structures
by satellite imaging radar. Case study of the
Lingayen Gulf, the Philippines.
• Mapping fish ponds and fish cages, using images from
ascending and descending orbits acquired within a
limited time interval.
• Fisheries and aquaculture are practiced worldwide in vastly
variable environments and at greatly varying scales, but the
biological systems and sustainable human exploitation are
controlled to a greater or lesser extent by many variables
that can be measured by remote sensing.
• Remote sensing will play an important role in
monitoring, planning and management activities, especially
given the large proportion of the earth’s surface that is
covered by aquatic environments and the costs that would
be involved in collecting data requirements by other means.
• The unique capability of satellite remote sensing to provide
regular, repeated observations of the entire globe or specific
regions at different spatial scales is also increasingly
important in the context of global climate change.
Remote sensing

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Remote sensing

  • 2. • • • • • INTRODUCTION REMOTE SENSING – DEFINITION PROCESS OF REMOTE SENSING TYPES OF REMOTE SENSING RS IN AQUACULTURE DEVELOPMENT & MANAGEMENT • APPLICATION OF RS IN AQUACULTURE • CASE STUDY • CONCLUSION
  • 3. • The major problem currently faced by world fisheries and aquaculture management challenges large geographic areas, including inland areas, coastal zones and open oceans. • As a result, remote sensing (from fixed coastal locations, aircraft and satellites) has been used to provide a large range of observation data to support fisheries and aquaculture management, which complement and extend data acquired from in situ observations.
  • 4. • “The science and art of obtaining information about an object, area or phenomenon through the analysis of data acquired by a device that is not in contact with the object, area or phenomenon under investigation”
  • 5. • The devices are sensors mounted on satellites or aircraft, or are installed at fixed coastal locations, that measure the electromagnetic radiation (EMR) that is emitted or reflected by features of the earth’s surface, and which then convert the EMR into a signal that can be recorded and displayed as either numerical data or as an image.
  • 6. • The full range of wavelengths of electromagnetic energy is often referred to as the electromagnetic spectrum and classes of wavelengths are often called spectral bands.
  • 7.
  • 8.
  • 9.
  • 10. Active- own source Passive – reflected EMR Scanning - motion Non scanning - fixed Imaging – 2 dimensional image Non imaging – 1dimensional image
  • 11.
  • 12.
  • 13. Optical and radar remote sensing systems are widely used. • Optical: These images are intuitive to interpret, but cloud cover can limit their availability. 1. Visible and infrared – Sensors can provide land cover and land use information for inland fisheries applications, ocean condition data such as chlorophyll-a and suspended sediment concentration, bathymetry and sea surface temperature (SST), and data to support coastal zone fisheries and aquaculture management. 2. Light detection and ranging (LIDAR) – An airborne system that can provide precise elevation data, usually for small areas. When combined with detailed visible and infrared optical imagery, this can be used for land cover and topography mapping, for
  • 14. 1. Imaging radar – Images can contain unique information compared with optical images, such as the flooded status of vegetation or surface roughness of a waterbody, but it typically can determine fewer land cover classes than optical data. 2. Radar altimeter – Can be processed to provide information on sea surface height, surface currents, waves and winds.
  • 15. 1. Sea surface temperature : • Advanced Very High Resolution Radiometer (AVHRR) sensors on the National Oceanic and Atmospheric Administration (NOAA) • The National Aeronautics and Space Administration (NASA) Moderate Resolution Imaging Spectroradiometer (MODIS) sensors on board the Earth Observing System (EOS) Aqua and Terra satellites • NOAA’s Geostationary Orbiting Earth Satellites (GOES) that are geostationary over the Western Hemisphere • Selecting and acquiring data provides some information on obtaining SST products from these satellites.
  • 16.
  • 17. 2. Ocean colour • Ocean colour refers to obtaining information about the ocean using optical sensors, including parameters such as concentration of chlorophylla, which is a measure of primary productivity, and total suspended matter (TSM), which is related to turbidity. • The International Ocean Colour Coordinating Group (IOCCG) provides a good summary of the current and future availability of ocean colour sensors. • Oceansat-1 (India)
  • 18.
  • 19. 3. Ocean salinity: • Passive radar detects the low levels of emitted microwave radiation from the earth’s surface. The data have very coarse spatial resolution, meaning that they are not generally used for fisheries and aquaculture applications. • Launched in 2011, the joint Argentina and the United States of America Aquarius satellite provides monthly maps of global changes in ocean surface salinity with a resolution of 150 km, showing how salinity changes from month to month, season to season, and year to year at a global scale. • European Space Agency Soil Moisture and Ocean Salinity (SMOS) satellite.
  • 20. • Mapping coastal aquaculture and fisheries structures by satellite imaging radar. Case study of the Lingayen Gulf, the Philippines. • Mapping fish ponds and fish cages, using images from ascending and descending orbits acquired within a limited time interval.
  • 21.
  • 22.
  • 23. • Fisheries and aquaculture are practiced worldwide in vastly variable environments and at greatly varying scales, but the biological systems and sustainable human exploitation are controlled to a greater or lesser extent by many variables that can be measured by remote sensing. • Remote sensing will play an important role in monitoring, planning and management activities, especially given the large proportion of the earth’s surface that is covered by aquatic environments and the costs that would be involved in collecting data requirements by other means. • The unique capability of satellite remote sensing to provide regular, repeated observations of the entire globe or specific regions at different spatial scales is also increasingly important in the context of global climate change.