A meteorological and chemical overview of the DACCIWA field campaign in West Africa in June–July 2016

Abstract

<p><strong>Abstract.</strong> In June and July 2016 the Dynamics–Aerosol–Chemistry–Cloud Interactions in West Africa (DACCIWA) project organised a major international field campaign in southern West Africa (SWA) including measurements from three inland ground supersites, urban sites in Cotonou and Abidjan, radiosondes and three research aircraft. A significant range of different weather situations was encountered during this period, including the monsoon onset. The purpose of this paper is to characterise the large-scale setting for the campaign as well as synoptic and mesoscale weather systems affecting the study region in the light of existing conceptual ideas, mainly using objective and subjective identification algorithms based on (re-) analysis and satellite products. In addition, it is shown how the described synoptic variations influence the atmospheric composition over SWA through advection of mineral-dust, biomass-burning and urban-pollution plumes. <br><br> The boreal summer of 2016 was characterised by Pacific La Niña, Atlantic El Niño and warm eastern Mediterranean conditions, whose competing influences on precipitation led to an overall average rainy season. During the relatively dusty pre-onset Phase 1 (1–21 June 2016), three westward propagating coherent cyclonic vortices between 4 and 13° N modulated winds and rainfall in the Guinea coastal area. The monsoon onset occurred in connection with a marked extratropical trough and cold surge over northern Africa, leading to a breakdown of the Saharan heat low and African easterly jet and a suppression of rainfall. During this period, quasi-stationary low-level vortices associated with the trough transformed into more tropical, propagating disturbances resembling an African easterly wave (AEW). To the east of this system, moist southerlies penetrated deep into the continent. The post-onset Phase 2 (22 June–20 July 2016) was characterised by a significant increase of low-level cloudiness, unusually dry conditions and strong northeastward dispersion of urban pollution plumes in SWA as well as rainfall modulation by westward propagating AEWs in the Sahel. Around 12–14 July 2016 an interesting and so-far undocumented cyclonic-anticyclonic vortex couplet crossed SWA. The anticyclonic centre had its origin in the southern hemisphere and transported unusually dry air filled with aged aerosol into the region. During Phase 3 (21–26 July 2016), a similar vortex couplet slightly farther north created enhanced westerly moisture transports into SWA and extraordinarily wet conditions, accompanied by a deep penetration of the biomass-burning plume from central Africa. Finally, a return to more undisturbed monsoon conditions took place during Phase 4 (27–31 July 2016). The in-depth synoptic analysis reveals that several significant weather systems during the DACCIWA campaign cannot be attributed unequivocally to any of the tropical waves and disturbances described in the literature, and thus deserve further study.</p>

Light absorption properties of aerosols over Southern West Africa

“…These elevated aerosol layers were dominated by either dust or biomass burning aerosols, which is consistent with what would be expected on the basis of the atmospheric circulations during the monsoon season (McConnell et al, 2008;Knippertz et al, 2017). However, during one flight a mixture of dust and biomass burning was found in a layer at around 3 km amsl, implying that there may be substantial variability in the idealized picture.…”

“…We believe the set of DACCIWA observations presented here is representative of the regional mean and variability in aerosol optical properties that can be observed during the monsoon season over SWA, as the main dynamical features were in line with climatology (Knippertz et al, 2017).…”

“…Figure 3 shows a statistical analysis of N fine , N coarse and σ ext derived from the in-situ measurements of vertical profiles. The aerosol vertical structure is strongly related to the meteorological structure of the atmosphere (see Knippertz et al, 2017 for an overview of the DACCIWA field campaign). The observed wind profiles highlight the presence of several distinct layers in the lower troposphere.…”

Remote biomass burning dominates southern West African air pollution during the monsoon

“…The aircraft campaign took place after the monsoon onset and was characterised by a northward-shifted intertropical discontinuity, which resulted in unusually dry conditions for this 70 time of year. This period has been described as Phase 2 of the 2016 West African Monsoon (Knippertz et al, 2017).…”

Measurements of nitric oxide and ammonia soil fluxes from a wet savanna ecosystem site in West Africa during the DACCIWA field campaign

“…Knippertz et al (2017) Knippertz et al (2017)). The division into phases is mainly based on the north-south precipitation difference between the coastal zone (0-7.5° N) and the Sudanian-Sahelian zone (7.5-15° N), both averaged across the longitude range 8° W-8°E…”