Fixed-point ocean observatory
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A fixed-point ocean observatory is an autonomous system of automatic sensors that continuously gathers data from deep sea, water column and lower atmosphere, and transmit the data to shore in real or near real-time.
Infrastructure
Fixed-point ocean observatories are typically composed of a cable anchored to the sea floor to which several automatic sensors and samplers are attached. The cable ends with a buoy at the ocean surface that may have some more sensors attached.[1] In most of the observatories the communicating buoys allow not only the data to be transmitted to shore, but also the scientists to change the acquisition method of the sensors, as an answer to a phenomena. These unmanned platforms can be linked via a cable to the shore transmitting data via an internet connection, or they can transmit data to relay buoys which are able to provide a satellite link to the shore.
Instrumentation
A typical multidisciplinary observatory is equipped with sensors and instruments to measure physical and biogeochemical variables along the water column:.[2] Main measured variables:
Sea surface | Sea-surface temperature (SST)
Sea-surface salinity (SSS)
|
Sub-surface | Temperature
Salinity
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In order to do so, typically the ocean observatories are equipped with instruments like:
- ADCP- Acoustic Doppler current profiler, to measure currents;
- CTD (conductivity, temperature and depth) sensors, to measure conductivity and thermal variations at a known depth;
- Hydrophone- to record sounds;
- Sediment Trap- to quantify the quantity of sinking material;
- Deep sea camera- to capture footage on location;
- Seismometer- to record the earth motion;
- CO2 analyser- to measure CO2;
- Dissolved Oxygen sensor- to measure dissolved oxygen;
- Fluorometers- to measure Chlorophyll;
- Turbidity sensor- to measure turbidity.
Purpose
Ocean observatories can collect data for different purposes from scientific research to environmental monitoring for marine operations or governance for the benefit of economy and society as a whole. Ocean observatories provide real-time, or near real time data allowing to detect changes as they happen, such as geo-hazards for example. Furthermore continuous time series data allow to investigate interannual-to-decadal changes and to capture episodic events, changes in ocean circulation, water properties, water mass formation and ecosystems, to quantify air-sea fluxes, and to analyse the role of the oceans for the climate .[3]
The data collected by the several ocean observatories around the globe on the sub-sea-floor, seafloor, and water column, allows to improve our knowledge [4] of the ocean including :
- Ocean physics and climate change
- Biodiversity and ecosystem assessment
- Carbon cycle and ocean acidification
- Geophysics and geodynamics
Moreover networks of ocean observatories can also be used to input data into global ocean models and to calibrate them thus allowing for the investigation of future changes in ocean circulation and ecosystems.
External links
FixO3 Fixed-Point Open Ocean Observatories Project
JERICO-NEXT Project (Joint European Research Infrastructure network for Coastal Observatories)
European Multidisciplinary Seafloor and water-column Observatory
European Ocean Observatory Network
References
- ^ FixO3 Project Factsheet, (2015).
- ^ Ruhl et al, Societal need for improved understanding of climate change, anthropogenic impacts, and geo-hazard warning drive development of ocean observatories in European Seas, Progress in Oceanography, Volume 91, Issue 1, October 2011, Pages 1–33 (doi:10.1016/j.pocean.2011.05.001) , additional text.
- ^ Ocean Reference Stations, Meghan F. Cronin, Robert A. Weller, Richard S. Lampitt and Uwe Send (2012). Ocean Reference Stations, Earth Observation, Dr. Rustam Rustamov (Ed.), InTech, DOI: 10.5772/27423. Available from: http://www.intechopen.com/books/earth-observation/ocean-reference-stations.
- ^ Seafloor Observatories, A New Vision of the Earth from the Abyss Favali, Paolo ; Beranzoli, Laura; De Santis, Angelo; Springer, 2015. - 688 p. (DOI 10.1007/978-3-642-11374-1)