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But ocean subsurface temperature data are very sparse in time and space, and they contain systematic biases for some instruments.
The ability of bacteria to grow at low temperatures is not unexpected, since the average subsurface temperature of soil in the temperate zone is about 12 °C (54 °F) and 90 percent of the oceans measure 5 °C (41 °F) or colder.
Furthermore, greater shallow subsurface temperature change occurs when the injection is conducted at shallower depths.
Using these temperature records, we calculated the influence of BWT variations on subsurface temperature distributions at WT1a, WT2, and WT3.
Constant and temperature-dependent thermal profiles indicate that thermal conductivity has an important impact on subsurface temperature distributions.
However, Fig. 11 clearly shows how variations in the depth of the K horizon affect the general subsurface temperature distribution.
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Those embedded in the road surface record pavement and subsurface temperatures; infrared "grip sensors" are beamed onto the road surface from nearby poles.
The house also has a geothermal system that taps into subsurface temperatures to supply all heating and cooling needs, augmented by passive solar.
With subsurface temperatures ranging from 46° F (8° C) in the south to about 39° F (4° C) in the north, the current exerts a moderating influence on the climate of Norway and northern Europe.
1950-57 Theofies of Moon's formation are incorporated in efforts to explain origin of solar system; radiometric age dating is employed in meteorite research; lunar subsurface temperatures are measured by microwave radiometry; relative ages of lunar features are derived from principles of stratigraphy (study of rock layers and their chronological relationship).
The estimations of subsurface temperatures resulted in widely differing and even inconsistent data.
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