Estimating Tropical Cyclone Intensity by Satellite Imagery Utilizing Convolutional Neural Networks

Author:

Chen Buo-Fu1,Chen Boyo2,Lin Hsuan-Tien2,Elsberry Russell L.3

Affiliation:

1. National Center for Atmospheric Research, Boulder, Colorado

2. Department of Computer Science and Information Engineering, National Taiwan University, Taipei, Taiwan

3. Department of Meteorology, Naval Postgraduate School, Monterey, California, and Trauma, Health, and Hazards Center, University of Colorado–Colorado Springs, Colorado Springs, Colorado

Abstract

Abstract Accurately estimating tropical cyclone (TC) intensity is one of the most critical steps in TC forecasting and disaster warning/management. For over 40 years, the Dvorak technique (and several improved versions) has been applied for estimating TC intensity by forecasters worldwide. However, the operational Dvorak techniques primarily used in various agencies have several deficiencies, such as inherent subjectivity leading to inconsistent intensity estimates within various basins. This collaborative study between meteorologists and data scientists has developed a deep-learning model using satellite imagery to estimate TC intensity. The conventional convolutional neural network (CNN), which is a mature technology for object classification, requires several modifications when being used for directly estimating TC intensity (a regression task). Compared to the Dvorak technique, the CNN model proposed here is objective and consistent among various basins; it has been trained with satellite infrared brightness temperature and microwave rain-rate data from 1097 global TCs during 2003–14 and optimized with data from 188 TCs during 2015–16. This paper also introduces an upgraded version that further improves the accuracy by using additional TC information (i.e., basin, day of year, local time, longitude, and latitude) and applying a postsmoothing procedure. An independent testing dataset of 94 global TCs during 2017 has been used to evaluate the model performance. A root-mean-square intensity difference of 8.39 kt (1 kt ≈ 0.51 m s−1) is achieved relative to the best track intensities. For a subset of 482 samples analyzed with reconnaissance observations, a root-mean-square intensity difference of 8.79 kt is achieved.

Funder

Ministry of Science and Technology, Taiwan

Directorate for Geosciences

Publisher

American Meteorological Society

Subject

Atmospheric Science

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