Difference between revisions of "Argus video"
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This article is a summary of chapter 11 of the [[Manual Sediment Transport Measurements in Rivers, Estuaries and Coastal Seas]]<ref>Rijn, L. C. van (1986). ''Manual sediment transport measurements''. Delft, The Netherlands: Delft Hydraulics Laboratory</ref>. This summary provides a short introduction of the [[Argus video monitoring system]]. | This article is a summary of chapter 11 of the [[Manual Sediment Transport Measurements in Rivers, Estuaries and Coastal Seas]]<ref>Rijn, L. C. van (1986). ''Manual sediment transport measurements''. Delft, The Netherlands: Delft Hydraulics Laboratory</ref>. This summary provides a short introduction of the [[Argus video monitoring system]]. | ||
Revision as of 19:35, 14 June 2013
This article is a summary of chapter 11 of the Manual Sediment Transport Measurements in Rivers, Estuaries and Coastal Seas[1]. This summary provides a short introduction of the Argus video monitoring system.
Contents
Introduction of Argus video
Using digital imaging technology, shore-based video systems now provide the additional capability of automated data collection, encompassing a much greater range of time and spatial scales than were previously possible.
An ARGUS monitoring system typically consists of four to five video cameras, spanning a 180º view, and allowing full coverage of about four to six kilometres of beach. The cameras are mounted on a high location along the coast and connected to an ordinary PC on site, which in turn communicates to the outside world using conventional techniques such as analogue modems, ISDN, DSL, or a wireless LAN (see also video technology and underwater video systems). Data sampling is usually hourly (although any schedule can be specified) and continues during rough weather conditions. As the process of data collection is fully automated, the marginal operating costs are virtually zero.
Each standard hourly collection usually consists of three types of images:
- snapshot images,
- time exposure images averaging out natural modulations in wave breaking to reveal a smooth pattern of bright image intensities, which are an excellent proxy for the underlying, submerged sand bar topography and
- variance images helping to identify regions which are changing in time (like the sea surface).
For more information on images, see also Argus image types and conventions and Argus standard image processing.
See also
Summaries of the manual
- Manual Sediment Transport Measurements in Rivers, Estuaries and Coastal Seas
- Chapter 1: Introduction, problems and approaches in sediment transport measurements
- Chapter 2: Definitions, processes and models in morphology
- Chapter 3: Principles, statistics and errors of measuring sediment transport
- Chapter 4: Computation of sediment transport and presentation of results
- Chapter 5: Measuring instruments for sediment transport
- Chapter 6: Measuring instruments for particle size and fall velocity
- Chapter 7: Measuring instruments for bed material sampling
- Chapter 8: Laboratory and in situ analysis of samples
- Chapter 9: In situ measurement of wet bulk density
- Chapter 10: Instruments for bed level detection
- Chapter 12: Measuring instruments for fluid velocity, pressure and wave height
Other internal links
External links
References
- ↑ Rijn, L. C. van (1986). Manual sediment transport measurements. Delft, The Netherlands: Delft Hydraulics Laboratory
Please note that others may also have edited the contents of this article.
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Please note that others may also have edited the contents of this article.
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- Reviewed articles
- Articles by Rijn, Leo van
- Articles by Roberti, Hans
- Theme 9
- Manual sediment transport measurements
- Techniques and methods in coastal management
- Land and ocean interactions
- Coastal erosion management
- Shoreline management
- Coastal erosion
- Sediment shorelines
- Remote Sensing in Coastal and Marine Research
