Analysis of Large-Scale Environmental Features during Maximum Intensity of Tropical Cyclones Using Reanalysis Data
The present study investigates the variation in large-scale environments during the maximum intensity of tropical cyclones (TCs) formed in the Bay of Bengal. TC tracks are classified into four groups based on their direction of movement using the <i>k</i>-means clustering technique. Resu...
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| Format: | Article |
| Language: | English |
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MDPI AG
2023-02-01
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| Series: | Atmosphere |
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| Online Access: | https://www.mdpi.com/2073-4433/14/2/333 |
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| author | Mohan Murali Krishna Gorja Venkata Sai Gulakaram Naresh Krishna Vissa Yesubabu Viswanadhapalli Bhishma Tyagi |
| author_facet | Mohan Murali Krishna Gorja Venkata Sai Gulakaram Naresh Krishna Vissa Yesubabu Viswanadhapalli Bhishma Tyagi |
| author_sort | Mohan Murali Krishna Gorja |
| collection | DOAJ |
| description | The present study investigates the variation in large-scale environments during the maximum intensity of tropical cyclones (TCs) formed in the Bay of Bengal. TC tracks are classified into four groups based on their direction of movement using the <i>k</i>-means clustering technique. Results from the pressure level and azimuthal-averaged radial-height wind fields near the vortex centre show weak deep layer wind shear (WS) and abundant moisture in all clusters. However, large-scale environmental differences in the northwest quadrant are identified with a contrasting combination of WS and humid environment between clusters. The composites of OLR are also analyzed during maximum intensities of TCs. Results show that anomalous high OLR in the west–northwest direction from the vortex centre, along with the low OLR around the vortex centre, signify the formation of a strong OLR dipole during TC peak intensity. Furthermore, OLR dipole metrics, such as magnitude, orientation, and distance, are observed by having mean of 235 Wm<sup>−2</sup>, 147, and 1782 km along with standard deviation of 14 Wm<sup>−2</sup>, 34°, and 492 km, respectively. The identified large-scale environmental fields from this study could provide valuable insights for predicting the intensity and movement of TCs. |
| first_indexed | 2024-03-11T09:09:59Z |
| format | Article |
| id | doaj.art-6f4adc7cb49c4b8abd4f60964f31d3a9 |
| institution | Directory Open Access Journal |
| issn | 2073-4433 |
| language | English |
| last_indexed | 2024-03-11T09:09:59Z |
| publishDate | 2023-02-01 |
| publisher | MDPI AG |
| record_format | Article |
| series | Atmosphere |
| spelling | doaj.art-6f4adc7cb49c4b8abd4f60964f31d3a92023-11-16T19:03:22ZengMDPI AGAtmosphere2073-44332023-02-0114233310.3390/atmos14020333Analysis of Large-Scale Environmental Features during Maximum Intensity of Tropical Cyclones Using Reanalysis DataMohan Murali Krishna Gorja0Venkata Sai Gulakaram1Naresh Krishna Vissa2Yesubabu Viswanadhapalli3Bhishma Tyagi4Department of Earth and Atmospheric Sciences, National Institute of Technology Rourkela, Rourkela 769008, IndiaIndian National Centre for Ocean Information Services (INCOIS), Hyderabad 500090, IndiaDepartment of Earth and Atmospheric Sciences, National Institute of Technology Rourkela, Rourkela 769008, IndiaWeather and Climate Research Group, National Atmospheric Research Laboratory, Gadanki, Tirupati 517112, IndiaDepartment of Earth and Atmospheric Sciences, National Institute of Technology Rourkela, Rourkela 769008, IndiaThe present study investigates the variation in large-scale environments during the maximum intensity of tropical cyclones (TCs) formed in the Bay of Bengal. TC tracks are classified into four groups based on their direction of movement using the <i>k</i>-means clustering technique. Results from the pressure level and azimuthal-averaged radial-height wind fields near the vortex centre show weak deep layer wind shear (WS) and abundant moisture in all clusters. However, large-scale environmental differences in the northwest quadrant are identified with a contrasting combination of WS and humid environment between clusters. The composites of OLR are also analyzed during maximum intensities of TCs. Results show that anomalous high OLR in the west–northwest direction from the vortex centre, along with the low OLR around the vortex centre, signify the formation of a strong OLR dipole during TC peak intensity. Furthermore, OLR dipole metrics, such as magnitude, orientation, and distance, are observed by having mean of 235 Wm<sup>−2</sup>, 147, and 1782 km along with standard deviation of 14 Wm<sup>−2</sup>, 34°, and 492 km, respectively. The identified large-scale environmental fields from this study could provide valuable insights for predicting the intensity and movement of TCs.https://www.mdpi.com/2073-4433/14/2/333Bay of BengalERA5OLR dipoletropical cyclones |
| spellingShingle | Mohan Murali Krishna Gorja Venkata Sai Gulakaram Naresh Krishna Vissa Yesubabu Viswanadhapalli Bhishma Tyagi Analysis of Large-Scale Environmental Features during Maximum Intensity of Tropical Cyclones Using Reanalysis Data Atmosphere Bay of Bengal ERA5 OLR dipole tropical cyclones |
| title | Analysis of Large-Scale Environmental Features during Maximum Intensity of Tropical Cyclones Using Reanalysis Data |
| title_full | Analysis of Large-Scale Environmental Features during Maximum Intensity of Tropical Cyclones Using Reanalysis Data |
| title_fullStr | Analysis of Large-Scale Environmental Features during Maximum Intensity of Tropical Cyclones Using Reanalysis Data |
| title_full_unstemmed | Analysis of Large-Scale Environmental Features during Maximum Intensity of Tropical Cyclones Using Reanalysis Data |
| title_short | Analysis of Large-Scale Environmental Features during Maximum Intensity of Tropical Cyclones Using Reanalysis Data |
| title_sort | analysis of large scale environmental features during maximum intensity of tropical cyclones using reanalysis data |
| topic | Bay of Bengal ERA5 OLR dipole tropical cyclones |
| url | https://www.mdpi.com/2073-4433/14/2/333 |
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