Heat-lows are low pressure systems that have been qualitatively compared to dry tropical cyclones (TCs) given their low-level cyclonic circulation which is co-located with strong surface sensible heat fluxes. Many transient heat-lows in West Africa are likely associated with dry African Easterly Waves (AEWs). This work examines the climatology of West African heat-lows and their relationship to TCs by extending potential intensity (PI) over land. Using ERA5 reanalysis, we calculate PI over land from sensible heat flux and land surface roughness and use pre-existing data of tracked dry low-pressure systems to create composite West African heat-lows during Summer. PI spatial distribution correlates well with that of heat-low tracks and closely matches the peak heat-low wind speeds. The asymmetric and baroclinic structure of heat-low composites and the lack of marked diurnal cycles suggest that West African heat-lows are likely dominated by the traditional mixed baroclinic barotropic energy pathways of dry AEWs.