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AGU: Journal of Geophysical Research, Atmospheres

 

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  • Atmospheric Composition and Structure: Middle atmosphere—constituent transport and chemistry
  • Atmospheric Composition and Structure: Pressure, density, and temperature
  • Atmospheric Composition and Structure: Instruments and techniques
Abstract
Cited By (3)
 

Abstract

JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 107, 8260, 18 PP., 2002
doi:10.1029/2001JD001379

Accuracy of analyzed stratospheric temperatures in the winter Arctic vortex from infrared Montgolfier long-duration balloon flights 1. Measurements

Jean-Pierre Pommereau

Service d'Aéronomie, CNRS, Verrières le Buisson, France

Anne Garnier

Service d'Aéronomie, CNRS, Verrières le Buisson, France

Bjoern M. Knudsen

Danish Meteorological Institute, Copenhagen, Denmark

Gérard Letrenne

Centre National d'Etudes Spatiales, Toulouse, France

Marc Durand

Centre National d'Etudes Spatiales, Toulouse, France

Manuel Nunes-Pinharanda

Service d'Aéronomie, CNRS, Verrières le Buisson, France

Laurent Denis

Service d'Aéronomie, CNRS, Verrières le Buisson, France

Francois Vial

Laboratoire de Météorologie Dynamique, Palaiseau, France

Albert Hertzog

Laboratoire de Météorologie Dynamique, Palaiseau, France

Francesco Cairo

Istituto de Fisica dell'Atmosfera, CNR, Rome, Italy

Long series of temperature measurements in the winter Arctic stratosphere have been obtained from infrared Montgolfier (MIR) long-duration balloon flights in 1997, 1999, and 2000, from which the performance of a variety of meteorological analyses has been investigated. In this first paper of a series of two, the experimental setup and the measurements are described. First flown in the winter Arctic in 1997, the MIR platform appears well adapted to perform flights for several weeks in the vortex. Flights of 12 and 22 days (1997), 7 and 17 days (1999), and 3 and 18 days (2000) have been achieved along which altitude, pressure, and temperature have been sampled every 9–10 min. Comparisons between various independent sensors on the same balloon, and to Vaisala and Russian radiosondes, have made it possible to evaluate the performances of the instruments. The accuracy of the altitude/location of the Global Positioning System proved to be ±100 m but that of the pressure sensors only ±2 hPa. The most accurate method for deriving pressure appears to be the use of GPS altitude together with the ECMWF (European Centre for Medium-Range Weather Forecasts) geopotential height. Finally, the temperature was demonstrated to be measured with a precision of ±0.4 K and an average bias of less than ±0.5 K, but during nighttime and at an altitude below only 28 km.

Published 13 August 2002.

Citation: Pommereau, J.-P., A. Garnier, B. M. Knudsen, G. Letrenne, M. Durand, M. Nunes-Pinharanda, L. Denis, F. Vial, A. Hertzog, and F. Cairo (2002), Accuracy of analyzed stratospheric temperatures in the winter Arctic vortex from infrared Montgolfier long-duration balloon flights 1. Measurements, J. Geophys. Res., 107(D20), 8260, doi:10.1029/2001JD001379.

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