Rocketsonde
The rocketsonde is similar to a dropsonde except that a
rocket is used to carry the sonde to the desired
deployment altitude where the sonde is ejected and
floats to Earth on a small parachute. Two types of
rocketsondes are in use today, and are classified
according to their maximum altitude. High-altitude
rocketsondes are used primarily by the military and use a large rocket to carry the sensor package to
altitudes in excess of 70 km. The Super Loki solid-fuel
rocket motor is typically the launch vehicle for highaltitude
rocketsonde deployments. Two meters long, it
accelerates to 1500m per second, and delivers its
meteorological payload above the stratosphere into
the mesosphere. The typical payload package, called a
dart, is approximately 1.1m long with an inside tube
diameter of less than 5 cm, and contains the meteorological
sonde. After the rocket motor burns out, the
dart continues to coast to an altitude ranging from 70
to 110 km. At apogee, a timed detonation of a small
explosive charge located in the tail of the dart ejects the
meteorological payload, which then begins its parachute-
aided descent. The payload consists of either a
meteorological sensor package – the rocketsonde – or
an inflatable sphere. The high-altitude rocketsondes
often contain a transponder, a miniature receiver–
transmitter that can be tracked by a radio direction
finding and ranging system to determine winds and
altitude. The inflatable sphere provides atmospheric
density data, obtained from its fall velocity as determined
by a precision tracking radar.
The second type of rocketsonde is smaller and less
expensive, and is used to measure only thermodynamic
variables in the lower 1–3km of the atmosphere
above earth. The Vaisala RK91 low-altitude rocketsonde
(Figure 12) is primarily designed for naval shipboard operations that require observations of the
refractive index profile near the ocean surface, but can
also be used over land where only thermodynamic
data are required. The RK91 can be prepared for
launch in less than 10 min; it reaches apogee in less
than 20 s, and provides a detailed thermodynamic
profile with 1 s resolution. After ejection of the sonde
payload, the sonde drifts on a parachute to the surface
from an altitude of 1 km in less than 6 min. Vertical
resolution is dependent on the rate of descent (typically
3msꠑ1), rate of data transmission (1 Hz) and
sensor response time. At temperatures above freezing,
vertical resolution is about 3m.
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