On Earth, monsoon seasons typically occur in West Africa, Asia and Australia.

A season during which changes in atmospheric circulation associated with the asymmetric heating of land and sea cause moisture to be brought inland by monsoon winds, leading to increased rainfall as moisture-laden air rises and cools over land.

Pending decision of placement of season as one-dimensional temporal region, we should add axioms cross linking to monsoon winds, as well as increased prevalence of water-based rainfall.

http://purl.obolibrary.org/obo/envo.owl

https://www.who.int/publications/i/item/public-health-for-mass-gatherings-key-considerations

http://orcid.org/0000-0002-4366-3088

https://orcid.org/0000-0002-3884-3420

http://orcid.org/0000-0002-3410-4655