Preprints
https://doi.org/10.5194/egusphere-2023-1092
https://doi.org/10.5194/egusphere-2023-1092
13 Jun 2023
 | 13 Jun 2023

Warm conveyor belt characteristics and impacts along the life cycle of extratropical cyclones: Case studies and climatological analysis based on ERA5

Katharina Heitmann, Michael Sprenger, Hanin Binder, Heini Wernli, and Hanna Joos

Abstract. This study presents a systematic and global investigation of the characteristics and impacts of warm conveyor belts (WCBs). For this purpose, we compile a new WCB climatology (1980–2022) of trajectories calculated with the most recent reanalysis dataset ERA5 from the European Centre for Medium-Range Weather Forecasts (ECMWF). Based on this new climatology, two-dimensional masks are defined, which represent the inflow, ascent and outflow locations of WCBs. These masks are then used to objectively quantify the key characteristics (intensity, ascent rate, and ascent curvature) and impacts (precipitation and potential vorticity (PV) anomalies) of WCBs in order to (i) attribute them to different stages in the life cycle of the associated cyclones and to (ii) evaluate differences in the outflow of the cyclonic and anticyclonic branches.

The method is first tested and illustrated through three case studies of well-documented cyclones, revealing both the similarities and the case-to-case variability in the evolution of the WCB characteristics and impacts. We then extend the analysis to about 5'000 cyclones that occurred in winter between 1980–2022 in the North Atlantic. The case studies and the climatological analysis both show that WCBs are typically most intense (in terms of air mass transported, ascent rate, precipitation rate, and volume) during the intensification period of the associated cyclone. The northward displacement along the storm track and diabatic PV production lead to an increase in low-level PV in the region of WCB ascent during the cyclone life cycle. The negative PV anomaly at upper levels, associated with the WCB outflow, remains relatively constant. The investigation of the WCB branches reveals an increasing intensity of the cyclonic WCB branch with time, linked to the increasing strength of the cyclonic wind field around the cyclone. Due to a lower altitude, the outflow of the cyclonic branch is associated with a weaker negative PV anomaly than the anticyclonic WCB branch, which ascends to higher altitudes. In summary, this study highlights the distinct evolution of WCB characteristics and impacts during the cyclone life cycle and the marked differences between the cyclonic and anticyclonic branches.

Katharina Heitmann, Michael Sprenger, Hanin Binder, Heini Wernli, and Hanna Joos

Status: final response (author comments only)

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on egusphere-2023-1092', Anonymous Referee #1, 01 Aug 2023
  • RC2: 'Comment on egusphere-2023-1092', Jeffrey Chagnon, 14 Aug 2023
  • AC1: 'Final response', Katharina Heitmann, 29 Sep 2023
Katharina Heitmann, Michael Sprenger, Hanin Binder, Heini Wernli, and Hanna Joos
Katharina Heitmann, Michael Sprenger, Hanin Binder, Heini Wernli, and Hanna Joos

Viewed

Total article views: 562 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
360 186 16 562 42 14 8
  • HTML: 360
  • PDF: 186
  • XML: 16
  • Total: 562
  • Supplement: 42
  • BibTeX: 14
  • EndNote: 8
Views and downloads (calculated since 13 Jun 2023)
Cumulative views and downloads (calculated since 13 Jun 2023)

Viewed (geographical distribution)

Total article views: 549 (including HTML, PDF, and XML) Thereof 549 with geography defined and 0 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 
Latest update: 29 Feb 2024
Download
Short summary
Warm conveyor belts (WCBs) are coherently ascending air streams that occur in extratropical cyclones where they form precipitation and often affect the large-scale flow. We quantified the key characteristics and impacts of WCBs and linked them to different phases in the cyclone life cycle and to different WCB branches. A climatology of these metrics revealed that WCBs are most intense during cyclone intensification and that the cyclonic and anticyclonic WCB branches show distinct differences.