On the verification of the quality of SABER temperature, geopotential height, and wind fields by comparison with Met Office assimilated analyses

[1] The Sounding of the Atmosphere using Broadband Emission Radiometry (SABER) experiment on the Thermosphere-Ionosphere-Mesosphere Energetics and Dynamics satellite has delivered over 1 year of radiance profile data from which middle atmosphere temperature profiles have been retrieved. Version 1.01 temperatures are precise and sufficiently accurate, such that one can obtain estimates of their synoptic distributions on pressure surfaces. A sequential estimation algorithm was used to generate daily, zonal Fourier coefficients of temperature (through zonal wave number 6), and maps on constant pressure surfaces were generated using those coefficients. Maps of temperature, geopotential height, and geostrophic winds are compared with products from the Met Office analyses. Stratospheric differences are within about 2 K for temperature and 160 m for geopotential height. The respective wind fields indicate flow patterns that are similar. Examples of the fields are shown for a period in February 2002 during a sudden stratospheric warming event that occurred in the Northern Hemisphere. A cooling of the middle mesosphere accompanies the warming. It is anticipated that large-scale, middle atmospheric dynamics and transport studies can be undertaken and that data assimilation products can be extended to near the mesopause using the SABER profiles.

[1]  Frank Moulaert,et al.  Conclusions and prospects , 1995 .

[2]  J. Barnett,et al.  Planetary waves in the winter mesosphere ‐ preliminary analysis of nimbus 6 PMR results , 1977 .

[3]  K. Labitzke Temperature Changes in the Mesosphere and Stratosphere Connected with Circulation Changes in Winter , 1972 .

[4]  J. Russell,et al.  Estimation of Synoptic Fields of Middle Atmosphere Parameters from Nimbus-7 LIMS Profile Data , 1990 .

[5]  T. Dunkerton Midwinter Deceleration of the Subtropical Mesospheric Jet and Interannual Variability of the High-Latitude Flow in UKMO Analyses , 2000 .

[6]  E. Remsberg,et al.  Variability of diurnal tides and planetary waves during November 1978-May 1979 , 2004 .

[7]  John C. Gille,et al.  The Limb Infrared Monitor of the Stratosphere: Experiment Description, Performance, and Results , 1984 .

[8]  M. Salby A Ubiquitous Wavenumber-5 Anomaly in the Southern Hemisphere During FGGE , 1982 .

[9]  Martin Riese,et al.  The CRISTA‐2 mission , 2002 .

[10]  J. Gille,et al.  Sounding the Stratosphere and Mesosphere by Infrared Limb Scanning from Space , 1980, Science.

[11]  James M. Russell,et al.  Retrieval of mesospheric and lower thermospheric kinetic temperature from measurements of CO2 15 µm Earth Limb Emission under non‐LTE conditions , 2001 .

[12]  T. Dunkerton,et al.  The subtropical mesospheric jet observed by the Nimbus 7 Limb Infrared Monitor of the Stratosphere , 1985 .

[13]  W. Grose,et al.  Comparison of LIMS temperatures and geostrophic winds with Berlin radiosonde temperature and wind measurements , 1988 .

[14]  Joseph J. Tansock,et al.  Overview of the SABER experiment and preliminary calibration results , 1999, Optics & Photonics.

[15]  T. Miles,et al.  Transient Medium-Scale Wave Activity in the Summer Stratosphere , 1986 .

[16]  Richard Swinbank,et al.  A Stratosphere-Troposphere Data Assimilation System , 1994 .

[17]  N. B. Ingleby,et al.  The Met. Office global three‐dimensional variational data assimilation scheme , 2000 .