Can synoptic patterns influence the track and formation of tropical cyclones in the Mozambique Channel?

Chibuike Chiedozie Ibebuchi; Chibuike Chiedozie Ibebuchi

doi:10.3934/geosci.2022003

AIMS Geosciences

2022, Volume 8, Issue 1: 33-51. doi: 10.3934/geosci.2022003

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Research article

Can synoptic patterns influence the track and formation of tropical cyclones in the Mozambique Channel?

Chibuike Chiedozie Ibebuchi ^,

Institute of Geography and Geology, University of Würzburg, Am Hubland, 97074 Würzburg, Germany

Received: 17 October 2021 Revised: 06 January 2022 Accepted: 10 January 2022 Published: 14 January 2022

The influence of large-scale circulation patterns on the track and formation of tropical cyclones (TCs) in the Mozambique Channel is investigated in this paper. The output of the hourly classification of circulation types (CTs), in Africa, south of the equator, using rotated principal component analysis on the T-mode matrix (variable is time series and observation is grid points) of sea level pressure (SLP) from ERA5 reanalysis from 2010 to 2019 was used to investigate the time development of the CTs at a sub-daily scale. The result showed that at specific seasons, certain CTs are dominant so that their features overlap with other CTs. CTs with synoptic features, such as enhanced precipitable water and cyclonic activity in the Mozambique Channel that can be favorable for the development of TC in the Channel were noted. The 2019 TC season in the Mozambique Channel characterized by TC Idai in March and TC Kenneth afterward in April were used in evaluating how the CTs designated to have TC characteristics played role in the formation and track of the TCs towards their maximum intensity. The results were discussed and it generally showed that large-scale circulation patterns can influence the formation and track of the TCs in the Mozambique Channel especially through (ⅰ) variations in the position and strength of the anticyclonic circulation at the western branch of the Mascarene high; (ⅱ) modulation of wind speed and wind direction; hence influencing convergence in the Channel; (ⅲ) and modulation of the intensity of cyclonic activity in the Channel that can influence large-scale convection.
- circulation type,
- tropical cyclones,
- hourly classification,
- Mozambique Channel,
- Africa south of the equator
Citation: Chibuike Chiedozie Ibebuchi. Can synoptic patterns influence the track and formation of tropical cyclones in the Mozambique Channel?[J]. AIMS Geosciences, 2022, 8(1): 33-51. doi: 10.3934/geosci.2022003

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Abstract

The influence of large-scale circulation patterns on the track and formation of tropical cyclones (TCs) in the Mozambique Channel is investigated in this paper. The output of the hourly classification of circulation types (CTs), in Africa, south of the equator, using rotated principal component analysis on the T-mode matrix (variable is time series and observation is grid points) of sea level pressure (SLP) from ERA5 reanalysis from 2010 to 2019 was used to investigate the time development of the CTs at a sub-daily scale. The result showed that at specific seasons, certain CTs are dominant so that their features overlap with other CTs. CTs with synoptic features, such as enhanced precipitable water and cyclonic activity in the Mozambique Channel that can be favorable for the development of TC in the Channel were noted. The 2019 TC season in the Mozambique Channel characterized by TC Idai in March and TC Kenneth afterward in April were used in evaluating how the CTs designated to have TC characteristics played role in the formation and track of the TCs towards their maximum intensity. The results were discussed and it generally showed that large-scale circulation patterns can influence the formation and track of the TCs in the Mozambique Channel especially through (ⅰ) variations in the position and strength of the anticyclonic circulation at the western branch of the Mascarene high; (ⅱ) modulation of wind speed and wind direction; hence influencing convergence in the Channel; (ⅲ) and modulation of the intensity of cyclonic activity in the Channel that can influence large-scale convection.

References

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