Abstract

Abstract. The retrieval of accurate profiles of temperature and water vapour is important for the study of atmospheric convection. Recent development in computational techniques motivated us to use adaptive techniques in the retrieval algorithms. In this work, we have used an adaptive neuro-fuzzy inference system (ANFIS) to retrieve profiles of temperature and humidity up to 10 km over the tropical station Gadanki (13.5° N, 79.2° E), India. ANFIS is trained by using observations of temperature and humidity measurements by co-located Meisei GPS radiosonde (henceforth referred to as radiosonde) and microwave brightness temperatures observed by radiometrics multichannel microwave radiometer MP3000 (MWR). ANFIS is trained by considering these observations during rainy and non-rainy days (ANFIS(RD + NRD)) and during non-rainy days only (ANFIS(NRD)). The comparison of ANFIS(RD + NRD) and ANFIS(NRD) profiles with independent radiosonde observations and profiles retrieved using multivariate linear regression (MVLR: RD + NRD and NRD) and artificial neural network (ANN) indicated that the errors in the ANFIS(RD + NRD) are less compared to other retrieval methods. The Pearson product movement correlation coefficient (r) between retrieved and observed profiles is more than 92% for temperature profiles for all techniques and more than 99% for the ANFIS(RD + NRD) technique Therefore this new techniques is relatively better for the retrieval of temperature profiles. The comparison of bias, mean absolute error (MAE), RMSE and symmetric mean absolute percentage error (SMAPE) of retrieved temperature and relative humidity (RH) profiles using ANN and ANFIS also indicated that profiles retrieved using ANFIS(RD + NRD) are significantly better compared to the ANN technique. The analysis of profiles concludes that retrieved profiles using ANFIS techniques have improved the temperature retrievals substantially; however, the retrieval of RH by all techniques considered in this paper (ANN, MVLR and ANFIS) has limited success.

Highlights

  • Atmospheric convection plays an important role in the energy circulation of the atmosphere by transporting heat, momentum and moisture from the boundary layer to the free atmosphere

  • We have presented a formulation of the adaptive neuro-fuzzy inference system (ANFIS) model for the retrieval of atmospheric profile temperature and humidity using brightness temperatures observed at different microwave frequencies mentioned above by microwave radiometers (MWRs)

  • In this work we found that ANFIS(RD + NRD) is more suitable for retrieving vertical profiles of the atmosphere by observing the power received on the ground due to different emissions at different microwave frequencies

Read more

Summary

Introduction

Atmospheric convection plays an important role in the energy circulation of the atmosphere by transporting heat, momentum and moisture from the boundary layer to the free atmosphere. The vertical transport of these fluxes (heat, momentum and moisture) determines the evolution of multiscale convective phenomena such as thunderstorms and tornadoes (Lane and Moncrieff, 2010; Shaw and Lane, 2013). It is difficult to study the evolution of convection using these observations due to their temporal resolution (frequency of vertical profiles). These observations have a limited availability: operational radiosonde profiles are generally available at 00:00 and 12:00 UTC of every day as it is very expensive to launch radiosonde operationally at regular intervals of 1 h.

Methods
Results
Conclusion
Full Text
Published version (Free)

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call