ESA's CryoSat-2 and NASA's DC-8 star in Arctic cooperation

Apr 23, 2010
On 20 April 2010, NASA flew a DC-8 directly under CryoSat-2 orbiting above. The DC-8 flight trajectory is marked in yellow and CryoSat-2's orbit is in orange. The DC-8, equipped with instruments to measure ice elevation, is used as part of NASA's Operation Ice Bridge campaign. The measurements acquired by NASA offer an early opportunity to check the quality of the newly launched CryoSat-2 satellite data over sea ice. Credits: NASA - M. Studinger/IBCAO

(PhysOrg.com) -- Taking advantage of NASA's 'Operation Ice Bridge' campaign, measurements of Arctic sea ice have been acquired from an aircraft flying under CryoSat-2's orbital path. These measurements offer an early opportunity to check the quality of the newly launched CryoSat-2 satellite data over sea ice.

Since ESA's ice mission CryoSat-2 was launched on 8 April, the satellite's primary instrument, the Synthetic Aperture Interferometric Radar Altimeter (SIRAL) has been switched on and is delivering its first radar echo data since 11 April. However, the mission still has to go through a six-month commissioning phase before it delivers calibrated and validated data to the wider scientific community. Nevertheless, ESA is very pleased with the quality of data so far.

This early opportunity to compare airborne with measurements arose though NASA's 'Operation Ice Bridge', which is a six-year field campaign to bridge the gap between its ICESat-I and ICESat-II missions. The campaign uses a DC-8 aircraft carrying, among other instruments, a laser called the 'Airborne Topographic Mapper', which sends pulses of light in circular scans to the ground. The pulses that are reflected back to the aircraft are converted into elevation maps of the ice surface below.

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The satellite is in a polar orbit, reaching latitudes of 88°. This orbit brings it closer to the poles than previous Earth observation satellites, covering an additional 4.6 million sq km - an area larger than all 27 European Union member states put together. Credits: ESA - AOES Medialab

Since the campaign is currently being carried out in the Arctic, ESA and NASA seized the opportunity to collaborate to divert and time one of the DC-8's flights to coincide with CryoSat-2 orbiting above.

Consequently, on 20 April the NASA aircraft flew from Thule in northwestern Greenland over the to pass directly under the satellite as it orbited close to the North Pole. In parallel, ESA's European Operations Centre (ESOC) in Germany switched CryoSat-2's SIRAL instrument from 'health monitoring mode' into its sea-ice measuring 'SAR mode'.

Robert Cullen, ESA's CryoSat-2 Commissioning Manager said, "Since SIRAL has been in excellent working order since we switched it on a few days after launch we decided to take advantage of the NASA underflight. Although we were testing the SIRAL at the time, the CryoSat flight control team manually switched the instrument into its sea-ice measurement mode for the duration of the underflight and quickly switched back to carry on our maintenance work afterwards."

The plane took around 750 kilometres worth of data, which will be compared in the future with CryoSat-2 observations from space.

"ESA welcomes the kind support of our NASA colleagues to the ongoing commissioning activities. This coordinated NASA DC-8 underflight provides a unique chance to engage the NASA-funded scientists involved in both Icebridge and CryoSat calibration and validation team activities," said Mark Drinkwater, Head of ESA's Earth Observation Mission Science Division.

"This collaboration will contribute to the evaluation of the quality of the data, and subsequently will ensure the broadest possible use of the data in climate science."

For a satellite mission aimed at providing global maps of ice-thickness change over time, down to centimetre level, validation is an essential element of the mission. To this end, ESA is planning extensive validation campaigns in the polar regions throughout the lifetime of the satellite. This involves taking measurements from the ground and from aircraft.

These campaigns are carried out as essential input to the software that transforms CryoSat-2's measurements into ice-thickness maps, and to make a direct comparison between ground and satellite measurements. ESA's next campaign in the Arctic is planned for this summer.

In the meantime, this first 'under flight' provides an early opportunity to verify the first CryoSat-2 data and sets the stage for future collaboration between ESA and NASA for future validation activities.

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