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It has been hypothesized that rain's suppression of ocean surface gravity waves and centimeter\u2010scale wave enhancement should alter the nature of air\u2010sea momentum flux, resulting in increased near\u2010surface current. Here, we use field observations to describe this impact and measure the very near\u2010surface current response to rainfall. During heavy rain, surface\u2010roughening ring waves were generated and longer gravity waves were suppressed; immediately following, the magnitude of the near\u2010surface current increased in response to wind forcing but died as the rain subsided and long waves recovered. These first\u2010of\u2010their\u2010kind field observations indicate that rain reduces ocean wave form drag in favor of tangential stress, resulting in the acceleration of current near the sea surface.<\/jats:p>","DOI":"10.1029\/2020gl087287","type":"journal-article","created":{"date-parts":[[2020,3,18]],"date-time":"2020-03-18T22:41:40Z","timestamp":1584571300000},"update-policy":"https:\/\/doi.org\/10.1002\/crossmark_policy","source":"Crossref","is-referenced-by-count":30,"title":["The Impact of Rain on Ocean Surface Waves and Currents"],"prefix":"10.1029","volume":"47","author":[{"ORCID":"https:\/\/orcid.org\/0000-0002-0373-9236","authenticated-orcid":false,"given":"Nathan J. 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