The present study describes artificial neural network (ANN) based approach for the retrieval of atmospheric temperature profiles from AMSU-A microwave temperature sounder. The nonlinear relationship between the temperature profiles and satellite brightness temperatures dictates the use of ANN, which is inherently nonlinear in nature. Since latitudinal variation of temperature is dominant one in the Earth’s atmosphere, separate network configurations have been established for different latitudinal belts, namely, tropics, mid-latitudes, and polar regions. Moreover, as surface emissivity in the microwave region of electromagnetic spectrum significantly influences the radiance (or equivalently the brightness temperature) at the satellite altitude, separate algorithms have been developed for land and ocean for training the networks. Temperature profiles from National Center for Environmental Prediction (NCEP) analysis and brightness temperature observations of AMSU-A onboard NOAA-19 for the year 2010 have been used for training of the networks. Further, the algorithm has been tested on the independent dataset comprising several months of 2012 AMSU-A observations. Finally, an error analysis has been performed by comparing retrieved profiles with collocated temperature profiles from NCEP. Errors in the tropical region are found to be less than those in the mid-latitude and polar regions. Also, in each region the errors over ocean are less than the corresponding ones over land. 1. Introduction Numerical weather prediction (NWP) is crucially dependent on proper initialization of NWP models, which effectively boils down to an accurate estimation of the present atmospheric state, a vitally important component of which is the atmospheric temperature profile. Such profiles can be estimated from observations taken by satellite-borne sounders operating in the microwave region of electromagnetic spectrum. The Advanced Microwave Sounding Unit (AMSU) A on board the latest generation of the National Oceanic and Atmospheric Administration (NOAA) polar orbiting satellites measures the outgoing radiances from the atmosphere and the Earth surface. With channels in the oxygen absorption band, AMSU-A is designed to retrieve the atmospheric temperature from about 3?hPa (~45?km) down to the Earth’s surface. The AMSU sounding unit operates on board the NOAA satellites since 1998. AMSU-A has 11 channels located close to the oxygen absorption lines below 60?GHz and four window channels at 23.8, 31.4, 50.3, and 89?GHz. The instrument has instantaneous fields of view of 3.3° and
References
[1]
T. Mo, “Prelaunch calibration of the advanced microwave sounding unit—a for NOAA-K,” IEEE Transactions on Microwave Theory and Techniques, vol. 44, no. 8, pp. 1460–1469, 1996.
[2]
T. Mo, “AMSU-a antenna pattern corrections,” IEEE Transactions on Geoscience and Remote Sensing, vol. 37, no. 1, pp. 103–112, 1999.
[3]
G. Goodrum, K. B. Kidwell, and W. Winston, NOAA KLM User’s Guide, National Oceanic and Atmospheric Administration, 1999.
[4]
L. Shi, “Retrieval of atmospheric temperature profiles from AMSU-A measurement using a neural network approach,” Journal of Atmospheric and Oceanic Technology, vol. 18, no. 3, pp. 340–347, 2001.
[5]
P. W. Rosenkranz, “Retrieval of temperature and moisture profiles from AMSU-A and AMSU-B measurements,” IEEE Transactions on Geoscience and Remote Sensing, vol. 39, no. 11, pp. 2429–2435, 2001.
[6]
S.-A. Boukabara, K. Garrett, W. Chen, et al., “MiRS: an all-weather 1DVAR satellite data assimilation and retrieval system,” IEEE Transactions on Geoscience and Remote Sensing, vol. 49, no. 9, pp. 3249–3272, 2011.
[7]
Z. Yao, H. Chen, and L. Lin, “Retrieving atmospheric temperature profiles from AMSU-A data with neural networks,” Advances in Atmospheric Sciences, vol. 22, no. 4, pp. 606–616, 2005.
[8]
F. Aires, A. Chédin, N. A. Scott, and W. B. Rossow, “A regularized neural net approach for retrieval of atmospheric and surface temperatures with the IASI instrument,” Journal of Applied Meteorology, vol. 41, no. 2, pp. 144–159, 2002.
[9]
J. Cheng, Q. Xiao, X. Li, Q. Liu, Y. Du, and A. Nie, “Multi-layer perceptron neural network based algorithm for simultaneous retrieving temperature and emissivity from hyperspectral FTIR dataset,” in Proceedings of the IEEE International Geoscience and Remote Sensing Symposium (IGARSS '07), pp. 4383–4385, June 2007.
[10]
W. J. Blackwell, “Neural network Jacobian analysis for high-resolution profiling of the atmosphere,” Eurasip Journal on Advances in Signal Processing, vol. 2012, no. 1, article 71, 2012.
[11]
Z. Tao, W. J. Blackwell, and D. H. Staelin, “Error variance estimation for individual geophysical parameter retrievals,” IEEE Transactions on Geoscience and Remote Sensing, vol. 51, no. 3, pp. 1718–1727, 2013.
[12]
E. Kalnay, M. Kanamitsu, R. Kistler et al., “The NCEP/NCAR 40-year reanalysis project,” Bulletin of the American Meteorological Society, vol. 77, no. 3, pp. 437–471, 1996.
[13]
G. L. Martin and J. A. Pittman, “Recognizing hand-printed letters and digits using backpropagation learning,” Neural Computation, vol. 3, no. 2, pp. 258–267, 1991.
[14]
M. A. Al-Alaoui, L. Al-Kanj, J. Azar, and E. Yaacoub, “Speech recognition using artificial neural networks and hidden Markov models,” IEEE Multidisciplinary Engineering Education Magazine, vol. 3, no. 3, pp. 77–86, 2008.
[15]
G. K. Venayagamoorthy, V. Moonasar, and K. Sandrasegaran, Voice Recognition Using Neural Networks, IEEE, 1998.
[16]
J. E. Dayhoff, Neural Network Architectures—An Introduction, Van Nostrand Reinhold, 1990.
[17]
J. Hertz, A. Krogh, and R. G. Palmer, Introduction to the Theory of Neural Computation, Addison-Wesley, 1991.
[18]
A. Cichocki and R. Unbehauen, Neural Networks for Optimization and Signal Processing, John Wiley & Sons, 1993.
[19]
Y. Chauvin and D. E. Rumelhart, Backpropagation: Theory, Architectures, and Applications, Lawrence Erlbaum Associates, 1995.
[20]
R. Rojas, Neural Networks—A Systematic Introduction, Springer, 1996.