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Retrieval of Atmospheric Temperature Profiles from AMSU-A Measurement Using Artificial Neural Network and Its Applications for Estimating Tropical Cyclone Intensity for ‘Gonu’ and ‘Nargis’

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Abstract

The vertical structure of temperature and water vapour plays an important role in the meteorological processes of the atmosphere. For years the radiosonde network has been the primary observing system for monitoring tropospheric temperature and water vapour. Routine observations are very difficult over the oceanic region due to logistic problems and high cost factors. The radiosonde networks are limited only over land regions. The interpretation of satellite radiances requires the inversion of the radiative transfer equation (RTE), where measurements of radiation performed at different frequencies are related to the energy from different atmospheric regions. The solution, thus obtained, is highly indeterminate for a set of observed radiances. The degree of indetermination is associated with the spectral resolution and the number of spectral channels. These radiances are basically a function of the vertical distribution of water vapour and temperature in the atmosphere and not simply of their average values. The retrieval of these vertical profiles from the radiances is an illposed problem that cannot be solved directly (Isaacs et al., 1986). Due to the difficulty of obtaining correct RTE solutions, several approaches and methods were developed to extract information from the satellite data by retrieving geophysical parameters from satellite radiances.

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Mitra, A.K., Sharma, A.K., Kundu, P.K. (2014). Retrieval of Atmospheric Temperature Profiles from AMSU-A Measurement Using Artificial Neural Network and Its Applications for Estimating Tropical Cyclone Intensity for ‘Gonu’ and ‘Nargis’. In: Mohanty, U.C., Mohapatra, M., Singh, O.P., Bandyopadhyay, B.K., Rathore, L.S. (eds) Monitoring and Prediction of Tropical Cyclones in the Indian Ocean and Climate Change. Springer, Dordrecht. https://doi.org/10.1007/978-94-007-7720-0_34

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