The Driftsonde observing system was developed by the National Center for Atmospheric Research (NCAR) to produce vertical profiles of in-situ measurements, at a low cost above oceans, remote Artic, Antarctic, or continental regions where in-situ measurements from radiosondes are not possible from the ground or from aircraft. Another goal is to provide such measurements in regions covered with extensive cloud shields so that satellite measurements are limited.
At left we can see an scheme of the flight system (click for more details of the gondola). The Driftsonde gondola houses the system electronics which includes an embedded computer, a GPS navigation system, flight level Pressure Temperature Humidity (PTH) sensors, a battery power system, an Iridium satellite two-way connmunication system, a 400 MHz receiver for dropsonde telemetry, and up to approximately 50 dropsonde tubes for the Miniature In-situ Sounding Technology (MIST) dropsonde.
The MIST dropsondes can be dropped down under parachute from the altitude of the carrier balloon to the ground, reaching a landing speed of about 7 m/s. During the descent through the atmosphere, the radiosonde makes measurements once per second, including GPS position, temperature, pressure and humidity. The radiosonde measurements are transmitted to the Driftsonde gondola by a Radio Frequence link in the 400 MHZ band, and then relayed to the operation control center via the Iridium satellite communications system. The radiosondes can be automatically released at predetermined times by the onboard computer or on command through the Iridium satellite link between the Driftsonde gondola using a WEB based system.
For this particular mission, the Driftsonde system was transported by a long-duration super pressure balloon developed by Zodiac with a diameter of 12 meters.
Balloon launched on: 10/19/2010
Launch site: McMurdo Station, Antarctica
Balloon launched by: Centre National d'Etudes Spatiales (CNES)
Balloon manufacturer/size/composition: Super Pressure Balloon
Flight identification number: MSD11
End of flight (L for landing time, W for last contact, otherwise termination time): 12/29/2010
Balloon flight duration (F: time at float only, otherwise total flight time in d:days / h:hours or m:minutes - ): 71 d
Landing site: Southern Pacific Ocean
This flight was part of CONCORDIASI a multidisciplinary effort jointly operated by France and the United States to study the lower stratosphere and troposphere above Antarctica as well as the land surface of the Antarctic continent carried out in 2010. An constellation of balloons provided a unique set of measurements covering both volume and time. The balloons drifted for several months on isopycnic surfaces in the lowermost stratosphere around 18 km, circling over Antarctica in the winter vortex.
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