Assimilation of IASI at the Met Office and assessment of its impact through observing system experiments

Observations from the Infrared Atmospheric Sounding Interferometer (IASI), onboard EUMETSAT's MetOp satellite, have been assimilated at the Met Office in global and regional numerical weather‐prediction systems since 27 November 2007. Pre‐operational trials of IASI assimilation in the global model during the summer of 2007 delivered a positive impact on forecasts approximately twice as large as that shown by the Atmospheric InfraRed Sounder (AIRS) on the EOS‐Aqua satellite. A series of observing system experiments confirmed the relative performance of IASI and AIRS, and showed that impact from IASI is equivalent to a single Advanced Microwave Sounding Unit‐A (AMSU‐A) combined with a single Microwave Humidity Sounder (MHS). The results of an IASI assimilation trial for the winter of 2007 were consistent with those of the summer trial, although the impact was slightly lower overall. The assessment of impact is strongly dependent on the variables and methods chosen for verification: assimilation trials with the regional model showed similar improvements to the large‐scale fields (e.g. mean‐sea‐level pressure and geopotential height) as seen in the global model, but no forecast impact was seen for variables such as visibility and rain‐rate. © Crown Copyright 2009. Reproduced with the permission of the Controller of HMSO. Published by John Wiley & Sons, Ltd.

[1]  J. Eyre,et al.  The assimilation of cloud‐affected infrared satellite radiances for numerical weather prediction , 2008 .

[2]  Andrew Collard,et al.  Selection of IASI channels for use in numerical weather prediction , 2007 .

[3]  A. Lorenc,et al.  The Met Office global four‐dimensional variational data assimilation scheme , 2007 .

[4]  J. Thepaut,et al.  The assimilation of AIRS radiance data at ECMWF , 2006 .

[5]  E. Pavelin,et al.  Plans for the assimilation of cloud-affected infrared soundings at the Met Office , 2006 .

[6]  P. Brunel,et al.  AAPP status report and preparations for processing METOP data , 2006 .

[7]  A. Staniforth,et al.  A new dynamical core for the Met Office's global and regional modelling of the atmosphere , 2005 .

[8]  A. Collard,et al.  Operational Use of AIRS Observations at the Met Office , 2005 .

[9]  William L. Smith,et al.  A principal component noise filter for high spectral resolution infrared measurements , 2004 .

[10]  Graeme Kelly,et al.  A satellite radiance‐bias correction scheme for data assimilation , 2001 .

[11]  Stephen J. English,et al.  A comparison of the impact of TOVS arid ATOVS satellite sounding data on the accuracy of numerical weather forecasts , 2000 .

[12]  Stephen J. English,et al.  A cloud‐detection scheme for use with satellite sounding radiances in the context of data assimilation for numerical weather prediction , 1999 .

[13]  D. Siméoni,et al.  Infrared atmospheric sounding interferometer , 1997 .

[14]  L. Larrabee Strow,et al.  Fast computation of monochromatic infrared atmospheric transmittances using compressed look-up tables , 1996, Optics + Photonics.

[15]  Philippe Courtier,et al.  Use of cloud‐cleared radiances in three/four‐dimensional variational data assimilation , 1994 .

[16]  Roger Saunders,et al.  RTTOV-7 : A Satellite Radiance Simulator for the New Millennium , .