Conductivity, temperature, depth
A CTD (often also CTD-rosette or CTD water sampler) is an essential instrument for physical and biological oceanography which is operated from a ship to measure the three main state variables of the ocean, Conductivity, Temperature, and Depth in order to improve the understanding of the world ocean. Often the device is mounted on a carousel of so-called Niskin bottles which close at predefined depths. This overall construction explains the name rosette. The closing of the sampling bottles is triggered either manually or by an on-board computer. The probed water can be analyzed further on board of the vessel for biological and chemical parameters. Besides, it is used for the calibration of the sensors.[1]
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Measured properties [edit]
The instrument is a cluster of sensors that measure continuous data of depth, salinity, and temperature, from which measurements of density can be derived. Sensors commonly scan at a rate of 24 Hz. Depth measurements are derived from measurement of hydrostatic pressure, and salinity is measured from electrical conductivity.[2] Sensors are arranged inside a metal housing, the metal used for the housing determining the depth to which the CTD can be lowered. Titanium housings allow sampling of the water column down to more than 10,000 m (~34,000 ft).[3] Other sensors may be added to the cluster, including some that measure chemical or biological parameters, such as dissolved oxygen and chlorophyll fluorescence, the latter an indication of the concentration of microscopic photosynthetic organisms (phytoplankton) contained in the water.
Deployment [edit]
Deployment of the CTD is made from the deck of the research vessel. The instrument is lowered into the water in what is called the downcast to a determined depth or to a few meters above the ocean floor, generally at a rate of about 0.5 m s-1. Most of the time a conducting wire cable is attached to the CTD frame connecting the CTD to an onboard computer, and allows instantaneous uploading and real time visualization of the collected data on the computer screen. The water column profile of the downcast is often used to determine the depths at which the CTD will be stopped on its way back to the surface, or the upcast, to collect the water samples.
Technological development [edit]
The CTD system was developed by Neil Brown, of the Woods Hole Oceanographic Institution, to overcome the limitations of an earlier similar system also developed by Brown, called an STD. The improvement was made possible thanks to increased reliability and reduced cost of computer technology.[4]
Advantages and Limitations [edit]
The advantage of CTD casts is the acquisition of high resolution data. The limitation of CTD sampling is that only a point in space (the sampling site) can be sampled at one time, and many casts, which are costly and time consuming, are needed to acquire a broad picture of the marine environment of interest. From the information gathered during CTD casts, however, scientists can investigate how physical parameters are related, for example, to the observed distribution and variation of organisms that live in the ocean, thus deepening our understanding of the processes that govern ocean life.
References [edit]
- ^ "CTD Instrument and Water Sampler". Alfred-Wegener-Institute for Polar- and Marine Research. Retrieved 19 September 2012.
- ^ Pickard and Emery 1990, p 100
- ^ http://www.seabird.com/products/profilers.htm
- ^ Baker 1981, pp 416-418
- Baker D. J. 1981 "Ocean instruments and experiment design" Chapter 14 pp 416–418, available at http://ocw.mit.edu/resources/res-12-000-evolution-of-physical-oceanography-spring-2007/part-3/wunsch_chapter14.pdf
- Pickard George L. and William J. Emery "Descriptive Physical Oceanography, An introduction" 5th ed., Butterworth-Heineman (Elsevier Science): 1990
