| Instrument: Microwave Temperature Profiler (MTP)
Principal Investigator: Michael J. ("MJ") Mahoney Organization: Jet Propulsion Laboratory
Phone:
(818)-354-5584
|
![]() |
The most fundamental use of the MTP is to provide meteorological context
for measurements made by in situ and remote sensors of atmospheric
gases and aerosols. In arctic regions for example, the ATP can be used
to locate altitudes where the air is cold enough to condense nitric acid
or water vapor to form polar stratospheric clouds. In addition, the temperature
field can used to determine the tropopause altitude, which is extremely
important to interpreting other measurements. The ATP can also be used
to derive the altitudes of isentrope surfaces to look for the presence
of meso- to synoptic-scale atmospheric waves. The "waviness" of isentropic
surfaces is used to characterize the magnitude of temperature fluctuations,
which is needed for deriving effective temperatures to be used in atmospheric
chemistry calculations involving reaction rates and solubility.
The
MTP on the WB57 consists of three components: the sensor unit (located
behind the fairing in the figure above), the data unit (which controls
the sensor unit and records data from it), and the real-time analysis
computer (which converts the measured brightness temperatures into
an altitude temperature profile). The latter two components are located
in the pod adapter ring rack. A video feed of the ATP is available for
display in the back seat of the WB57 (shown to the right), and this information
can be used in real-time to control the altitude of the WB57 with respect
to the tropopause. The total mass of the instrument is ~ 15 kg, split roughly
equally between the three components.