Preprints
https://doi.org/10.5194/wcd-2022-61
https://doi.org/10.5194/wcd-2022-61
 
30 Nov 2022
30 Nov 2022
Status: this preprint is currently under review for the journal WCD.

Classification of Large-Scale Environments that drive the formation of Mesoscale Convective Systems over Southern West Africa

Francis Nkrumah1,2, Cornelia Klein3,5, Kwesi Akumenyi Quagraine1,4, Rebecca Berkoh-Oforiwaa2,6, Nana Ama Browne Klutse2,6, Patrick Essien1,2, Gandomè Mayeul Leger Davy Quenum2,7, and Hubert Azoda Koffi6 Francis Nkrumah et al.
  • 1Department of Physics, University of Cape Coast, Private Mail Bag, Cape Coast, Ghana
  • 2African Institute of Mathematical Sciences (AIMS), Sector Remera, Kigali 20093, Rwanda
  • 3U.K. Centre for Ecology and Hydrology, Wallingford, United Kingdom
  • 4Climate System Analysis Group (CSAG), ENGEO, University of Cape Town, Private Bag X3, Rondebosch, Cape Town 7701, South Africa
  • 5Department of Atmospheric and Cryospheric Sciences, University of Innsbruck, Innsbruck, Austria
  • 6Department of Physics, University of Ghana, Legon P.O. Box LG 63, Ghana
  • 7National Institute of Water (NIW), University of Abomey-Calavi, Godomey, Cotonou 01 PB: 4521, Benin

Abstract. Mesoscale convective systems (MCSs) are frequently observed over southern West Africa (SWA) throughout most of the year. However, it has not yet been identified what variations in typical large-scale environments of the West African monsoon seasonal cycle may favour MCS occurrence in this region. Here, six distinct synoptic states are identified and are further associated with being either a dry season, pre-, post-, or peak-monsoon synoptic circulation type using self organizing maps (SOMs) with inputs from reanalysis data. We identified a pronounced annual cycle of MCS numbers with frequency peaks in June and September which can be associated with peak rainfall during the major and minor rainy seasons respectively across SWA. Comparing daily MCS frequencies, MCSs are most likely to develop during post-monsoon conditions featuring a northward-displaced moisture anomaly (0.42 MCSs per day), which can be linked to strengthened low-level westerlies. Considering that these post-monsoon conditions occur predominantly from September and into November, these patterns may in some cases be representative of a delayed monsoon retreat. On the other hand, under peak monsoon conditions, we observe easterly wind anomalies during MCS days, which reduce moisture content over the Sahel but introduce more moisture over the coast. Finally, we find all MCS-day synoptic states to exhibit positive shear anomalies. Seasons with the strongest shear anomalies are associated with the strongest low-level temperature anomalies to the north of SWA, highlighting that a warmer Sahel can promote MCS-favourable conditions in SWA. These significant positive zonal shear anomalies for MCS days illustrate the importance of shear for MCS development in SWA throughout the year.

Francis Nkrumah et al.

Status: final response (author comments only)

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse

Francis Nkrumah et al.

Francis Nkrumah et al.

Viewed

Total article views: 313 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
230 73 10 313 2 3
  • HTML: 230
  • PDF: 73
  • XML: 10
  • Total: 313
  • BibTeX: 2
  • EndNote: 3
Views and downloads (calculated since 30 Nov 2022)
Cumulative views and downloads (calculated since 30 Nov 2022)

Viewed (geographical distribution)

Total article views: 306 (including HTML, PDF, and XML) Thereof 306 with geography defined and 0 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 
Latest update: 01 Feb 2023
Download
Short summary
The study identified six types of favourable Mesoscale Convective System (MCS) environments in Southern West Africa using Self Organizing Maps (SOM). The identified environmental types are noted to represent patterns of the seasonal rainfall cycle. Our results show that MCSs develop on average in similar high moisture, high shear local environments under all large-scale situations throughout the year. The latter however defines the frequency at which favourable MCS environments can occur.