6.6 Measurement of Temperature
Temperature in the ocean has been measured many ways. Thermistors and mercury thermometers are commonly used on ships and buoys. These are calibrated in the laboratory before being used, and after use if possible, using mercury or platinum thermometers with accuracy traceable to national standards laboratories. Infrared radiometers on satellites measure the ocean's surface temperature.
One very important mercury thermometer is the reversing thermometer (Figure 6.11) carried on Nansen bottles, which are described in the next section. It is a thermometer that has a constriction in the mercury capillary that causes the thread of mercury to break at a precisely determined point when the thermometer is turned upside down. The thermometer is lowered deep into the ocean in the normal position; and it is allowed to come to equilibrium with the water. Mercury expands into the capillary, and the amount of mercury in the capillary is proportional to temperature. The thermometer is then flipped upside down, the thread of mercury breaks trapping the mercury in the capillary, and the thermometer is brought back. The mercury in the capillary of the reversed thermometer is read on deck along with the temperature of a normal thermometer, which gives the temperature at which the reversed thermometer is read. The two readings give the temperature of the water at the depth where the thermometer was reversed.
The reversing thermometer is carried inside a glass tube which protects the thermometer from the ocean's pressure because high pressure can squeeze additional mercury into the capillary. If the thermometer is unprotected, the apparent temperature read on deck is proportional to temperature and pressure at the depth where the thermometer was flipped A pair of protected and unprotected thermometers gives temperature and pressure of the water at the depth the thermometer was reversed.
Pairs of reversing thermometers carried on Nansen bottles were the primary source of subsea measurements of temperature as a function of pressure from around 1900 to 1970.
Platinum Resistance Thermometer
Bucket temperatures The temperature of surface waters has been routinely measured at sea by putting a mercury thermometer into a bucket which is lowered into the water, letting it sit at a depth of about a meter for a few minutes until the thermometer comes to equilibrium, then bringing it aboard and reading the temperature before water in the bucket has time to change temperature. The accuracy is around 0.1°C. This is a very common source of direct surface temperature measurements.
Ship Injection Temperature The temperature of the water drawn into the ship to cool the engines has been recorded routinely for decades. These recorded values of temperature are called injection temperatures. Errors are due to ship's structure warming water before it is recorded. This happens when the temperature recorder is not placed close to the point on the hull where water is brought in. Accuracy is 0.5°-1°C.
Advanced Very High Resolution Radiometer
The instrument was originally designed to measure cloud temperatures and hence cloud height. The instrument had, however, sufficient accuracy and precision that it was soon used to measure regional and global temperature patterns at the sea surface.
The instrument is a radiometer that converts infrared radiation into electrical signals. It includes a mirror that scans from side to side across the subsatellite track and reflects radiance from the ground into a telescope, a telescope that focuses the radiance on detectors, detectors sensitive to different wavelengths that convert the radiance at those wavelengths into electrical signals, and electronic circuitry to digitize and store the radiance values. The instruments observes a 2700-km wide swath centered on the subsatellite track. Each observation along the scan is from a pixel that is roughly one kilometer in diameter near the center of the scan and that increases in size with distance from the subsatellite track.
The radiometers measures infrared radiation emitted from the surface in five wavelength bands: three infrared bands: 3.55–3.93 µm, 10.30–11.30 µm, and 11.50–12.50 µm; a near-infrared band at 0.725–1.00 µm; and a visible-light band at 0.58–0.68 µm. All infrared bands include radiation emitted from the sea and from water vapor in the air along the path from the satellite to the ground. The 3.7 µm band is least sensitive to water vapor and other errors, but it works only at night because sunlight has radiance in this band. The two longest wavelength bands at 10.8 µm and 12.0 µm are used to observe sea-surface temperature and water vapor along the path in daylight.
Data with 1-km resolution are transmitted directly to ground stations that view the satellite as it passes the station. This is the Local Area Coverage mode. Data are also averaged to produce observations from 4km × 4km pixels. These data are stored on tape recorders and later transmitted to NOAA receiving stations. This is the Global Area Coverage mode.
The swath width is sufficiently wide that the satellite views the entire Earth twice per day, at approximately 09:00 AM and 9:00 PM local time. Areas at high latitudes may be observed as often as eight or more times per day. The most important errors are due to:
Maps of temperature processed from Local Area Coverage of cloud-free regions show variations of temperature with a precision of 0.1°C. These maps are useful for observing local phenomena including patterns produced by local currents. Figure 10.16 shows such patterns off the California coast.
Global maps are made by the U. S. Naval Oceanographic Office, which receives the global AVHRR data directly from NOAA's National Environmental Satellite, Data and Information Service in near-real time each day. The data are carefully processed to remove the influence of clouds, water vapor, aerosols, and other sources of error. Data are then used to produce global maps between ± 70° with an accuracy of ± 0.6°C (May et a.,l 1998). The maps of sea-surface temperature are sent to the U.S. Navy and to NOAA's National Centers for Environmental Prediction. In addition, the office produces daily 100km global and 14km regional maps of temperature.
Global Maps of Sea-Surface Temperature
Maps of mean temperature have also been made from ICOADS data. The data are poorly distributed in time and space except for some areas of the northern hemisphere. In addition, Reynolds and Smith (1994) found that ship temperature data had errors twice as large as temperature errors in data from buoys and AVHRR. Thus, space data processed by Reynolds are more accurate, and better distributed than ICOADS.
Anomalies of sea-surface temperature are calculated using mean sea-surface temperature from the period 1950-979 calculated from ICOADS supplemented with four years of satellite data 1982-1985 (Reynolds and Smith, 1995).
|Department of Oceanography, Texas A&M University
Robert H. Stewart, email@example.com
All contents copyright © 2005 Robert H. Stewart,
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Updated on September 15, 2008