Mesoscale rainfall patterns observed around wetlands in sub-Saharan Africa

Taylor, Christopher M. ORCID: https://orcid.org/0000-0002-0120-3198; Prigent, Catherine; Dadson, Simon J.. 2018 Mesoscale rainfall patterns observed around wetlands in sub-Saharan Africa. Quarterly Journal of the Royal Meteorological Society, 144 (716). 2118-2132. 10.1002/qj.3311

Before downloading, please read NORA policies.

Preview

Text N520094JA.pdf - Published Version Available under License Creative Commons Attribution 4.0. Download (2MB) | Preview

Abstract/Summary

Wetlands are dynamic components of the landscape, responding to local and upstream rainfall, river flow and groundwater variability, and to water management. At the same time, in regions of strong evaporative demand, wetlands can present very strong land surface heterogeneity to the atmosphere, driving marked gradients in sensible and latent heat fluxes. At certain times of year, wetlands can therefore potentially provide a land surface feedback on rainfall. Here we assess the influence of wetlands on rainfall across Sub‐Saharan Africa (SSA). Using a well‐established multi‐satellite based product of wetland extent with monthly temporal resolution, we find significant wetland coverage (>10%) occurs at some point in the 15‐year dataset for about 22% of SSA. We analyse rainfall patterns in the vicinity of major wetlands using satellite data, and find a consistent signal across SSA of locally suppressed rainfall over the wetlands as compared to nearby drier areas. This signal contrasts with a simple atmospheric water balance perspective which would suggest increased rain in response to increased local evaporation. The observed signal is strongest during the afternoon and weakens overnight. Using cloud‐top temperature data from the Sahel, we find that afternoon convective initiation is favoured close to wetlands, consistent with forcing by a thermally‐induced circulation from gradients in sensible heat fluxes. We also find that in this region, where the vast majority of rainfall is associated with remotely‐triggered Mesoscale Convective Systems (MCS), convection weakens when these systems pass over wetlands. From this study, we conclude that wetlands across the range of climate zones spanning SSA influence rainfall patterns locally, and where MCS are an important component of rainfall, this influence can extend over a larger region, associated with the tracks of long‐lived MCS.

Item Type:	Publication - Article
Digital Object Identifier (DOI):	10.1002/qj.3311
UKCEH and CEH Sections/Science Areas:	Hydro-climate Risks (Science Area 2017-)
ISSN:	0035-9009
Additional Information. Not used in RCUK Gateway to Research.:	Open Access paper - full text available via Official URL link.
Additional Keywords:	African rainfall, convection, land–atmosphere interactions, wetlands
NORA Subject Terms:	Meteorology and Climatology
Date made live:	17 May 2018 10:57 +0 (UTC)
URI:	https://nora.nerc.ac.uk/id/eprint/520094

Actions (login required)

View Item

Document Downloads

More statistics for this item...