Difference between revisions of "Optical remote sensing"

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This article provides an introduction of optical [[remote sensing]] techniques. This technique can be used to detect all kind of in-water properties. This article describes the general principles of optical remote sensing, the way data can be processed and the restrictions with respect to the application of optical remote sensing.  
{{Definition|title=Passive optical remote sensing
 
|definition= ''Passive optical sensors detect natural energy (radiation) that is emitted or reflected by the object or scene being observed. Reflected sunlight is the source of radiation measured by passive optical sensors.'' <ref name="multiple"/>
 
[http://en.wikipedia.org/wiki/Remote_sensing].
 
}}
 
  
Remote sensing using satellite and airborne sensors is a powerful, often-preferred tool for monitoring coastal zones, as these detection instruments can provide accurate, large scale, synoptic environmental data essential for understanding and managing marine ecosystems. Optical multi- or hyperspectral sensors enable the detection of in-water properties, such as suspended matter and phytoplankton concentration, and provide information on benthic substrate type, vegetation composition, and bathymetry in optically-shallow waters (see “Applications”).   
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==Introduction==
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[[Remote sensing]] using satellite and airborne sensors is a powerful, operational tool for monitoring coastal zones. This technology can provide accurate, large-scale, synoptic environmental information essential for understanding and managing marine ecosystems.  
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Optical multi- or hyperspectral sensor data allows the assessment of in-water properties, such as suspended matter or phytoplankton concentration, benthic substrate type, vegetation composition, and [[bathymetry]] in (optically-)shallow waters.   
  
==See also==
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===Principles===
 
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In the broadest sense, remote sensing is the measurement or acquisition of information of an object or phenomenon, by a recording device that is not in physical or intimate contact with the object. In practice, remote sensing is the utilization at a distance (as from aircraft, spacecraft, satellite, or ship) of any device for gathering information about the environment <ref name="multiple">[http://www.wikipedia.org From Wikipedia, the free encyclopaedia]</ref>.
[[Hyperspectral seafloor mapping and direct bathymetry calculation in littoral zones]]
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Passive optical sensors detect natural energy (radiation) that is emitted or reflected by the object or scene being observed. Reflected sunlight is the source of radiation measured by passive optical sensors.
 
 
[[Optical remote sensing: habitat mapping, SPM maps, chlorophyll maps, bathymetry]]
 
  
...
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In marine and aquatic environments, the sunlight spectrum is modified on its way through the atmosphere, the water surface, and the water body. In each of these boundary layers sunlight is absorbed, scattered, and reflected in a specific manner, depending on the wavelength. As a result, the reflected light carries spectral information about the particular composition of these matters.
  
==Principles==
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[[Image:Reflection.jpg |thumb|250px|right| Remote sensing process of water bodies (airborne)]]
Optical remote sensing using passive satellite or airborne sensors is the spatially resolved detection and utilization of sunlight which has been transmitted through the atmosphere and reflected back from the earth’s surface to the sensor. <ref name="multiple"> WIKIPEDIA (From Wikipedia, the free encyclopedia) </ref>
 
  
In marine and aquatic environments, the sunlight spectrum is modified on its way through the atmosphere, water surface, and water body. Materials in each of these boundary layers absorbs, scatters, and reflects the different light wavelengths in a specific manner. As a result, the reflected light carries spectral information about the composition of these substances.
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===Sensors===
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Each sensor has its own technical characteristics in terms of temporal, spatial, spectral, and radiometric resolution. Depending on specific requirements of a project, such as area size, availability or thematic specifications, multi- or hyperspectral detectors on space- or airborne platforms are applied.  
  
==Sensors==
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The space agencies NASA ([[SeaWiFS]], [[MODIS]]) and ESA ([[MERIS]]) operate the main optical remote sensing satellites currently used for aquatic and coastal remote sensing.
This spectral information is detected differently, in terms of accuracy, for temporal, spatial, spectral, and radiometric resolution, and is characteristic for each different sensor. Multi- or hyperspectral detectors on space or airborne platforms may be chosen depending upon specific requirements, such as cost, area size, or availability.  
 
  
 
==Data processing==
 
==Data processing==
Different remote sensing data processing methods are available, and each evaluates or interprets the spectral information in a slightly different manner. To best retrieve the content information with regards to space and time, the output from a number of different algorithms can be compared against ground-based observational data.  
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Different [[remote sensing]] data processing methods are available to retrieve thematic information from remote sensing data. With mathematical and statistical methods the spectral information is analysed. Pixels are compared to specific class signatures and assigned depending on the similarity.
  
 
===Physics-based retrieval algorithms===
 
===Physics-based retrieval algorithms===
Physics-based retrieval algorithms can generally be applied world wide and are very flexible under all conditions covered by the optical models upon which they were based. Once set up, they do not rely on manual adaptations in order to generate map products and are frequently completely independent of input from ground truth measurements.  
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Physics-based retrieval algorithms model the complex light interactions with the atmosphere and the water body based on physical principles. Once set up, these optical models do not require manual adaptation in order to generate map products and are often independent of ground truth measurements. These algorithms are very flexible and may be applied world wide and are very under all conditions covered by the optical models upon which they are based.
  
=== Empirical algorithms ===
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===Empirical algorithms===
Empirical algorithms are powerful analytical tools, which rely on accompanied ground truth measurements and thus are typically not transferable between different types of aquatic and marine ecosystems.  
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Empirical algorithms are powerful analytical tools, which rely on ground truth measurements and are typically not transferable between different aquatic and marine ecosystems.  
  
=== Generic processing systems ===
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===Generic processing systems===
 
Generic processing systems cover a wide range of applications and can be applied to new sites, applications, and sensors due to a systematic, modular approach and easy adaptations for sensor- and site-specific properties.
 
Generic processing systems cover a wide range of applications and can be applied to new sites, applications, and sensors due to a systematic, modular approach and easy adaptations for sensor- and site-specific properties.
  
=== Geo-rectification ===
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===Geo-rectification===
Geo-rectification procedures are applied to remote sensing data in order to assign each spatially-resolved pixel with a geographic coordinate. Accurate, geo-coded maps can then be produced and incorporated into Geographical Information System (GIS) software. The trigonometric principles and procedures for geo-referencing are essentially developed and operational, therefore, sub-pixel accuracies can be achieved given adequate navigation data were available during collection. In practice, the spatial accuracy of operational geo-coded products depends on the accuracy of the satellite or airborne platform‘s navigation system. Therefore, for high-precision tasks, many satellite or airborne images have to be refined using manual geo-rectification approaches or automatic matching algorithms.  
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Geo-rectification procedures are applied to remote sensing data in order to assign each spatially-resolved pixel with a geographic coordinate. Accurate, geo-coded maps can be produced and incorporated into Geographical Information System (GIS) software.  
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Complex trigonometric principles and procedures for geo-referencing are operational, therefore, sub-pixel accuracies can be achieved given adequate navigation data were available during collection. In practice, the spatial accuracy of operational geo-coded products depends on the accuracy of the satellite or airborne platform‘s navigation system. Therefore, for high-precision tasks, many satellite or airborne images have to be refined using manual geo-rectification approaches or automatic matching algorithms.
  
 
==Restrictions==
 
==Restrictions==
Restrictions apply whenever the object-specific signals are masked or interfered with in any ambiguous manner, with regards to both the sensor resolution and retrieval methods. Therefore only a few restrictions can be identified in general and most restrictions can only be determined with site-specific observations, sensors used, or algorithms applied.  
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Restrictions occur whenever the object-specific signals are masked or interfered with in any ambiguous manner, with regards to both the sensor resolution and retrieval methods. Therefore only few general restrictions can be identified and most restrictions can only be determined with site-specific observations, sensors used, or algorithms applied.  
  
===Examples of general restrictions===  
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===General restrictions===  
Examples of general restrictions are clouds masking optical signals reflected from the earth surface or geometric recording conditions from the water surface that add intense sun glitter <ref> Sun glitter is defined as (spatial usually very variable) the contribution of direct sunlight that is reflected at the water surface and substantially increases the intensity of radiance measured at the sensor. It appears at specific geometric recording conditions between sun, the water surface, and the sensor, and affects approximately 30-70% of all earth observation images. </ref>
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Examples of general restrictions are clouds masking optical signals reflected from the earth surface or direct reflections from the water surface resulting in intense contributions to the recorded signal [[sun glitter]].
contributions to the signal.  
 
  
===Examples of case-dependent restrictions===
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===Case-dependent restrictions===
a) Intermediate sun glitter conditions can be treated only if the radiometric and spectral (and depending on the algorithm, maybe also spatial) resolution of the sensor is sufficient and the processing approach supports such a correction or consideration of this effect (> example).  
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Examples of case-dependent restrictions are:
b) The spatial resolution of the sensor must be better in most cases than the spatial heterogeneity of the target areas to be mapped. Sub-pixel classification of surfaces is only possible for a very restricted number of spectral endmembers. At the very least, every contribution of members not implemented into the model will create errors.  
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# Intermediate [[sun glitter]] sun glitter effects can be corrected only if the radiometric and spectral resolution of the sensor is adequate and the processing approach supports respective correction procedures (> example).  
c) The spectral behaviour of optical classes must differ significantly from each other with respect to the sensor’s spectral resolution. e.g. Chlorophyll and Gelbstoff cannot be estimated independently if the sensor’s spectral and radiometric resolution is insufficient and/or the ecosystem specific absorption spectra are too similar for an independent, quantitative estimate.
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# The spatial resolution of the [[sensor]] must be higher than the spatial heterogeneity of the target areas to be mapped. Sub-pixel classification of surfaces is only possible for a very restricted number of spectral end members. At the very least, every contribution of members not implemented into the model will create inaccuracies.  
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# The spectral behaviour of optical classes must differ significantly from each other with respect to the sensor’s spectral resolution. E.g. Chlorophyll and dissolved organic matter (Gelbstoff) cannot be estimated independently if the sensor’s spectral and radiometric resolution is insufficient and/or the ecosystem specific absorption spectra are too similar for an independent, quantitative estimate.
  
==References==
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==See also==
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* [[Optical measurements in coastal waters]]
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* [[Hyperspectral seafloor mapping and direct bathymetry calculation in littoral zones]]
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* [[Light fields and optics in coastal waters]]
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* [[Optical backscatter point sensor (OBS)]]
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* [[General principles of optical and acoustical instruments]]
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* [[Optical Laser diffraction instruments (LISST)]]
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* [[Use of Lidar for coastal habitat mapping]]
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* [[data processing and output of Lidar]]
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==Notes and references==
 
<references/>
 
<references/>
  
[[Category:Techniques and methods in coastal management]]
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----
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{{author
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|AuthorID=12962
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|AuthorFullName=Thomas Heege
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|AuthorName=Thomas Heege}}
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[[Category:Coastal and marine observation and monitoring]]

Revision as of 20:05, 29 June 2019

This article provides an introduction of optical remote sensing techniques. This technique can be used to detect all kind of in-water properties. This article describes the general principles of optical remote sensing, the way data can be processed and the restrictions with respect to the application of optical remote sensing.

Introduction

Remote sensing using satellite and airborne sensors is a powerful, operational tool for monitoring coastal zones. This technology can provide accurate, large-scale, synoptic environmental information essential for understanding and managing marine ecosystems. Optical multi- or hyperspectral sensor data allows the assessment of in-water properties, such as suspended matter or phytoplankton concentration, benthic substrate type, vegetation composition, and bathymetry in (optically-)shallow waters.

Principles

In the broadest sense, remote sensing is the measurement or acquisition of information of an object or phenomenon, by a recording device that is not in physical or intimate contact with the object. In practice, remote sensing is the utilization at a distance (as from aircraft, spacecraft, satellite, or ship) of any device for gathering information about the environment [1]. Passive optical sensors detect natural energy (radiation) that is emitted or reflected by the object or scene being observed. Reflected sunlight is the source of radiation measured by passive optical sensors.

In marine and aquatic environments, the sunlight spectrum is modified on its way through the atmosphere, the water surface, and the water body. In each of these boundary layers sunlight is absorbed, scattered, and reflected in a specific manner, depending on the wavelength. As a result, the reflected light carries spectral information about the particular composition of these matters.

Remote sensing process of water bodies (airborne)

Sensors

Each sensor has its own technical characteristics in terms of temporal, spatial, spectral, and radiometric resolution. Depending on specific requirements of a project, such as area size, availability or thematic specifications, multi- or hyperspectral detectors on space- or airborne platforms are applied.

The space agencies NASA (SeaWiFS, MODIS) and ESA (MERIS) operate the main optical remote sensing satellites currently used for aquatic and coastal remote sensing.

Data processing

Different remote sensing data processing methods are available to retrieve thematic information from remote sensing data. With mathematical and statistical methods the spectral information is analysed. Pixels are compared to specific class signatures and assigned depending on the similarity.

Physics-based retrieval algorithms

Physics-based retrieval algorithms model the complex light interactions with the atmosphere and the water body based on physical principles. Once set up, these optical models do not require manual adaptation in order to generate map products and are often independent of ground truth measurements. These algorithms are very flexible and may be applied world wide and are very under all conditions covered by the optical models upon which they are based.

Empirical algorithms

Empirical algorithms are powerful analytical tools, which rely on ground truth measurements and are typically not transferable between different aquatic and marine ecosystems.

Generic processing systems

Generic processing systems cover a wide range of applications and can be applied to new sites, applications, and sensors due to a systematic, modular approach and easy adaptations for sensor- and site-specific properties.

Geo-rectification

Geo-rectification procedures are applied to remote sensing data in order to assign each spatially-resolved pixel with a geographic coordinate. Accurate, geo-coded maps can be produced and incorporated into Geographical Information System (GIS) software. Complex trigonometric principles and procedures for geo-referencing are operational, therefore, sub-pixel accuracies can be achieved given adequate navigation data were available during collection. In practice, the spatial accuracy of operational geo-coded products depends on the accuracy of the satellite or airborne platform‘s navigation system. Therefore, for high-precision tasks, many satellite or airborne images have to be refined using manual geo-rectification approaches or automatic matching algorithms.

Restrictions

Restrictions occur whenever the object-specific signals are masked or interfered with in any ambiguous manner, with regards to both the sensor resolution and retrieval methods. Therefore only few general restrictions can be identified and most restrictions can only be determined with site-specific observations, sensors used, or algorithms applied.

General restrictions

Examples of general restrictions are clouds masking optical signals reflected from the earth surface or direct reflections from the water surface resulting in intense contributions to the recorded signal sun glitter.

Case-dependent restrictions

Examples of case-dependent restrictions are:

  1. Intermediate sun glitter sun glitter effects can be corrected only if the radiometric and spectral resolution of the sensor is adequate and the processing approach supports respective correction procedures (> example).
  2. The spatial resolution of the sensor must be higher than the spatial heterogeneity of the target areas to be mapped. Sub-pixel classification of surfaces is only possible for a very restricted number of spectral end members. At the very least, every contribution of members not implemented into the model will create inaccuracies.
  3. The spectral behaviour of optical classes must differ significantly from each other with respect to the sensor’s spectral resolution. E.g. Chlorophyll and dissolved organic matter (Gelbstoff) cannot be estimated independently if the sensor’s spectral and radiometric resolution is insufficient and/or the ecosystem specific absorption spectra are too similar for an independent, quantitative estimate.

See also

Notes and references


The main author of this article is Thomas Heege
Please note that others may also have edited the contents of this article.

Citation: Thomas Heege (2019): Optical remote sensing. Available from http://www.coastalwiki.org/wiki/Optical_remote_sensing [accessed on 28-03-2024]