Sea Technology

OCT 2015

The industry's recognized authority for design, engineering and application of equipment and services in the global ocean community

Issue link: http://sea-technology.epubxp.com/i/586584

Contents of this Issue

Navigation

Page 19 of 76

www.sea-technology.com October 2015 / st 19 Mastodon Mooring System To Measure Seabed Temperature Data Logger With Ballast, Release Device at European Continental Shelf By Pascal Lazure • David Le Berre • Laurent Gautier S ea temperature is an essential environmental parameter because it infuences both the dynamics of the ocean and the structure of the whole benthic ecosystem. For decades, sea surface temperature (SST) has been measured by satel- lites whose spatial resolution is constantly being improved. The spatial and temporal variability of SST is now relatively well-known for most of the ocean. In coastal areas, including the European Continental Shelf (depths ranging from 0 to 150 m), the vertical profle of temperature depends mainly on turbulence conditions. In some areas, such as the eastern English Channel, the strong tidal current constantly mixes the water column, and the SST can be extrapolated directly to the seabed. However, in most coastal areas, thermal stratifcation occurs seasonally from spring to autumn and assessment of seabed temperatures requires in-situ devices. The de- ployment of a temperature sensor for several months on the seabed entails a mooring system, because most of the depths are diffcult or impossible to reach by scuba diving. Although temperature data loggers are now affordable, the deployment of a mooring system for several months is gen- erally a risky and expensive operation. These barriers are probably the reason that seabed temperature time series are so scarce for coastal areas. The goal of the Mastodon mooring system is to record the spatial and temporal changes in the seabed temperature during the stratifed period that lasts for at least six months at middle latitudes. The required precision of the temperature measurement was set at 0.1° C, a commonly adopted value for coastal observatory systems. The low cost of the instru- ment enabled deploying several instruments in the same area to ensure suffcient in-situ spatial resolution. 3D diagram of the mooring system: (1) electronics; (2) foat compartment; (3) traffc cone; (4) ballasts; (5) rope spool; and (6) wire grate.

Articles in this issue

Links on this page

Archives of this issue

view archives of Sea Technology - OCT 2015
loading...
Sea Technology
Welcome!
If you're not a subscriber, please click here for a free subscription.