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(Risk and coastal zone policy: example from the Netherlands)
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==Risk and coastal zone policy: example from the Netherlands==
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==Optical measurements in coastal waters==
  
[[image:Nederland.PNG|thumb|275px|right|Flood defences along the Dutch coast ''(Modified after:CPD, 2000)'']]
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This article gives an introduction of the instruments available (and the application of these instruments) to measure optical properties in coastal waters. Attention is paid to optical measurements in general, regional characteristics and implications for [[remote sensing]].
  
Risk and probability are widely used in today's policies. It is also possible to adapt probabilistic design  in coastal zone management. The risk of flooding poses a threat to present and future socio-economic activities. In this case risk can be defined as the probability of occurrence of an extreme event (storms, tsunamis) leading to erosion and flooding multiplied by the (socio-) economic damage caused by the storm event. The design water level of flood defences along the dutch coast are designed using the probabilistic approach. These levels are related to extreme storm surge water levels with a certain probability of occurrence. The level of the flood defence also on the value in the [[coastal hinterland|hinterland]]. Besides the design level, an probability of failure is taken into account.
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Optical measuments using satellite and airborne sensors is a powerful, operational tool for monitoring [[coastal zone]]s. This technology can provide accurate, large-scale, synoptic environmental information essential for understanding and managing marine [[ecosystems]].
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Optical sensor data allows the assessment of in-water properties, such as suspended matter or [[phytoplankton]] concentration, [[benthic]] substrate type, vegetation composition, and [[bathymetry]]. Optical sampling methods enable for example the continuous and contactless measurement of sediment concentrations, which is an important advantage compared to the mechanical sampling methods.
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Optical characteristics of a light-transmitting medium can be specified in terms of its inherent optical properties (IOPs). The main IOPs are:
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* the absorption coefficient (a) (m<sup>-1</sup>)
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* the scattering coefficient (b) (m<sup>-1</sup>)
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* the attenuation coefficient (c), with c = a + b (m<sup>-1</sup>)
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* the scattering phase function (&beta;) (sr<sup>-1</sup>)
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The total IOPs of a body of seawater can be considered as the sum of the partial contributions from water itself and a number of optically significant constituents. Four classes of constituents can be distinguished:
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#[[Phytoplankton]] cells and colonies (Phyt)
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#Mineral suspended solids (MSS)
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#Coloured dissolved organic matter (CDOM)
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#Organic suspended solids or [[detritus]] (OSS)

Revision as of 11:36, 15 December 2008

Optical measurements in coastal waters

This article gives an introduction of the instruments available (and the application of these instruments) to measure optical properties in coastal waters. Attention is paid to optical measurements in general, regional characteristics and implications for remote sensing.

Optical measuments 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 sensor data allows the assessment of in-water properties, such as suspended matter or phytoplankton concentration, benthic substrate type, vegetation composition, and bathymetry. Optical sampling methods enable for example the continuous and contactless measurement of sediment concentrations, which is an important advantage compared to the mechanical sampling methods.

Optical characteristics of a light-transmitting medium can be specified in terms of its inherent optical properties (IOPs). The main IOPs are:

  • the absorption coefficient (a) (m-1)
  • the scattering coefficient (b) (m-1)
  • the attenuation coefficient (c), with c = a + b (m-1)
  • the scattering phase function (β) (sr-1)

The total IOPs of a body of seawater can be considered as the sum of the partial contributions from water itself and a number of optically significant constituents. Four classes of constituents can be distinguished:

  1. Phytoplankton cells and colonies (Phyt)
  2. Mineral suspended solids (MSS)
  3. Coloured dissolved organic matter (CDOM)
  4. Organic suspended solids or detritus (OSS)