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. During the boreal summer, the monsoon season that takes place in West Africais accompanied by low stratus clouds over land that stretch from the Guinean coastseveral hundred kilometers inland.Numerical climate and weather models need finer description and knowledge of cloud macrophysical characteristics and of the dynamical and thermodynamical structuresoccupying the lowest troposphere, in order to be properly evaluated in this region.The Dynamics-Aerosol-Chemistry-Cloud Interactions in West Africa (DACCIWA) field experiment, which tookplace in summer 2016, addresses this knowledge gap. Low-level atmospheric dynamics and stratiform low-level cloud macrophysical properties are analyzed using in situ and remote sensing measurements continuously collectedfrom 20 June to 30 July at Save, Benin, roughly 180 km from the coast.The macrophysical characteristics of the stratus clouds are deduced from a ceilometer,an infrared cloud camera, and cloud radar. Onset times, evolution, dissipation times,base heights, and thickness are evaluated. The data from an ultra-high-frequency (UHF) wind profiler, a microwave radiometer, and an energy balance stationare used to quantify the occurrence and characteristics of the monsoon flow, the nocturnal low-level jet, and the cold air mass inflow propagating northward from the coast of the Gulf of Guinea.The results show that these dynamical structures are very regularly observed during the entire 41 d documented period. Monsoon flow is observed every day during our study period.The so-called “maritime inflow” and the nocturnal low-level jet are also systematic features in this area.According to synoptic atmospheric conditions, the maritime inflow reaches Save around 18:00–19:00 UTC on average.This timing is correlated with the strength of the monsoon flow.This time of arrival is close to the time range of the nocturnal low-level jet settlement. As a result, these phenomena are difficult to distinguish at the Save site.The low-level jet occurs every night, except during rain events, and is associated 65 % of the time with low stratus clouds.Stratus clouds form between 22:00 and 06:00 UTC at an elevation close to the nocturnal low-level jet core height.The cloud base height, 310±30  m above ground level (a.g.l.), is rather stationary during the night and remains below the jet core height.The cloud top height, at 640±100  m a.g.l., is typically found above the jet core.The nocturnal low-level jet, low-level stratiform clouds, monsoon flow, and maritime inflowreveal significant day-to-day and intra-seasonal variability during the summer given the importance of the different monsoon phases and synoptic atmospheric conditions. Distributions of strength, depth, onset time,breakup time, etc. are quantified here. These results contribute to satisfy the main goals of DACCIWA and allow a conceptual model of the dynamical structures in the lowest troposphere over the southern part of West Africa.

Low-level stratiform clouds and dynamical features observed within the southern West African monsoon