HOPKINS GLOSSARY OF WEATHER TERMS T
target
telemetry
- The study of the remote sensing and measurement of quantities.
theodolite
- An optical or radio instrument used to make accurate measurements
of vertical and horizontal angles; used in tracking instrument
packages on weather balloons and rockets. Optical theodolites
use a telescope to aid in tracking.
thermistor
- A type of electrical therometer whose electrical resistance
decreases markedly and monotonically as the temperature increases.
This instrument is often used on radiosondes or rocketsondes
.
thermogram
- A continuous trace of temperature variation
with time, typically produced by a thermograph.
thermograph
- A self-recording thermometer that produces a permanent
thermogram.
thermometer
- Any instrument that measures temperature with a sensor element
that utilizes the variation of the physical properties of a substances
associated with their temperature. Examples include liquid-in-glass
, deformation-type, electrical and radiation
thermometers.
thermosphere
- The region of the earth's atmosphere above the mesopause
, starting at 80 km (50 mi) altitude, where the air temperature
increases with altitude. The thermosphere extends outward toward
space and includes the exosphere and most or all of the
ionosphere.
transponder
- A miniature receiver-transmitter that can be tracked by a
radio-direction finder.
tropopause
- The cold region in the earth's atmosphere located about 10
km (8 mi) above the surface, at which the usual vertical temperature
decrease in the troposphere ceases; by convention, the
tropopause is defined as where the temperature lapse rate
to less than 2 C per kilometer for an extended depth (usually
2 km). This boundary marks the top of the troposphere and the
base of the stratosphere, and can vary with season and
latitude, with a altitude ranging from 6 km (4 mi) in polar regions
to 16 km (10 mi) in the tropics
troposphere
- The lowest region of the earth's atmosphere that extends from
the surface to the tropopause, located at an altitude of
6 to 16 km (4 to 10 mi). Normally this region has a more or less
regular decrease of air temperature with increasing altitude,
considerable vertical wind motion, appreciable water vapor, and
weather.
Last update 6 June 1996
Edward J. Hopkins, Ph.D.
Department of Atmospheric and Oceanic Sciences
University of Wisconsin-Madison
hopkins@meteor.wisc.edu