Preprints
https://doi.org/10.5194/cp-2020-162
https://doi.org/10.5194/cp-2020-162

  26 Jan 2021

26 Jan 2021

Review status: a revised version of this preprint is currently under review for the journal CP.

Influence of the representation of convection on the mid-Holocene West African Monsoon

Leonore Jungandreas1, Cathy Hohenegger1, and Martin Claussen1,2 Leonore Jungandreas et al.
  • 1Max Planck Institute for Meteorology, Bundesstraße 53, 20146 Hamburg
  • 2Center for Earth System Research and Sustainability, Universität Hamburg, Bundesstraße 53, 20146 Hamburg

Abstract. Global climate models have difficulties to simulate the northward extension of the monsoonal precipitation over north Africa during the mid-Holocene as revealed by proxy data. A common feature of these models is that they usually operate on too coarse grids to explicitly resolve convection, but convection is the most essential mechanism leading to precipitation in the west African monsoon region. Here, we investigate how the representation of tropical deep convection in the ICON climate model affects the meridional distribution of monsoonal precipitation during the mid-Holocene, by comparing regional simulations of the summer monsoon season (July to September, JAS) with parameterized (40 km-P) and explicitly resolved convection (5 km-E).

The spatial distribution and intensity of precipitation, are more realistic in the explicitly resolved convection simulations than in the simulations with parameterized convection.

However, in the JAS-mean the 40 km-P simulation produces more precipitation and extents further north than the 5 km-E simulation, especially between 12° N and 17° N. The higher precipitation rates in the 40 km-P simulation are consistent with a stronger monsoonal circulation over land. Furthermore, the atmosphere in the 40 km-P simulation is less stably stratified and notably moister. The differences in atmospheric water vapor are the result of substantial differences in the probability distribution function of precipitation and its resulting interactions with the land surface. The parametrization of convection produces light and large-scale precipitation, keeping the soils moist and supporting the development of convection. In contrast, less frequent but locally intense precipitation events lead to high amounts of runoff in explicitly resolved convection simulations. The stronger runoff inhibits the moistening of the soil during the monsoon season and limits the amount of water available to evaporation.

Leonore Jungandreas et al.

Status: final response (author comments only)

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Review of cp-2020-162', Anonymous Referee #1, 15 Feb 2021
  • RC2: 'Comment on cp-2020-162', Aiko Voigt, 23 Feb 2021
  • RC3: 'Comment on cp-2020-162', Anonymous Referee #3, 05 Mar 2021

Leonore Jungandreas et al.

Leonore Jungandreas et al.

Viewed

Total article views: 526 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
415 97 14 526 2 3
  • HTML: 415
  • PDF: 97
  • XML: 14
  • Total: 526
  • BibTeX: 2
  • EndNote: 3
Views and downloads (calculated since 26 Jan 2021)
Cumulative views and downloads (calculated since 26 Jan 2021)

Viewed (geographical distribution)

Total article views: 465 (including HTML, PDF, and XML) Thereof 464 with geography defined and 1 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 
Latest update: 10 May 2021
Download
Short summary
We investigate the impact of explicitly resolving convection on the mid-Holocene West African monsoon rain belt by employing the ICON climate model in high resolution. While the spatial distribution and intensity of the precipitation is improved by this technique, the monsoon extents further north and the mean summer rainfall is higher in the simulation with parameterized convection.