Version 2 of the IASI NH.sub.3 neural network retrieval algorithm: near-real-time and reanalysed datasets

• Published in: Atmospheric measurement techniques Vol. 10; no. 12; pp. 4905 - 9809
• Main Authors: Van Damme, Martin, Whitburn, Simon, Clarisse, Lieven, Clerbaux, Cathy, Hurtmans, Daniel, Coheur, Pierre-François
• Format: Journal Article
• Language: English
• Published: Copernicus GmbH 15.12.2017
• Subjects: Algorithms; Artificial neural networks; Methods; Remote sensing
• ISSN: 1867-1381

Recently, Whitburn et al.(2016) presented a neural-network-based algorithm for retrieving atmospheric ammonia (NH.sub.3) columns from Infrared Atmospheric Sounding Interferometer (IASI) satellite observations. In the past year, several improvements have been introduced, and the resulting new baseline version, Artificial Neural Network for IASI (ANNI)-NH.sub.3 -v2.1, is documented here. One of the main changes to the algorithm is that separate neural networks were trained for land and sea observations, resulting in a better training performance for both groups. By reducing and transforming the input parameter space, performance is now also better for observations associated with favourable sounding conditions (i.e. enhanced thermal contrasts). Other changes relate to the introduction of a bias correction over land and sea and the treatment of the satellite zenith angle. In addition to these algorithmic changes, new recommendations for post-filtering the data and for averaging data in time or space are formulated. We also introduce a second dataset (ANNI-NH.sub.3 -v2.1R-I) which relies on ERA-Interim ECMWF meteorological input data, along with surface temperature retrieved from a dedicated network, rather than the operationally provided Eumetsat IASI Level 2 (L2) data used for the standard near-real-time version. The need for such a dataset emerged after a series of sharp discontinuities were identified in the NH.sub.3 time series, which could be traced back to incremental changes in the IASI L2 algorithms for temperature and clouds. The reanalysed dataset is coherent in time and can therefore be used to study trends. Furthermore, both datasets agree reasonably well in the mean on recent data, after the date when the IASI meteorological L2 version 6 became operational (30 September 2014).