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Three experiments are conducted. Two use the coupled model with a horizontal resolution of either 1\u2009km (HRL) or 3\u2009km (LRL). The third (NoTCFB) is the same as LRL but excludes tropical cyclone (TC)\u2010induced sea\u2010surface temperature (SST) cooling. HRL reasonably reproduces <jats:italic>Muifa<\/jats:italic>\u2032s intensity during its rapid intensification and weakening periods. The azimuthal mean tangential and radial momentum budgets are analysed before the RI rates diverge between HRL and LRL. Results show that the dominant processes responsible for <jats:italic>Muifa<\/jats:italic>\u2032s intensification are different in HRL and LRL. For HRL, the net eddy effect intensifies the storm\u2032s circulation and contracts the eyewall during early RI, and it dominates the net mean\u2010flow effect inside the radius of maximum wind (RMW), except near the surface and between 2 and 5\u00a0km close to the RMW. In contrast, the mean and eddy effects in LRL almost cancel inside the RMW, while the mean\u2010flow effects dominate and intensify tangential winds outside. Without TC\u2010induced SST cooling, <jats:italic>Muifa<\/jats:italic> in NoTCFB reaches a similar storm intensity as in HRL but its rapid weakening rate is substantially underestimated. The dominant mechanisms for tangential wind intensification in NoTCFB are similar to those in LRL, but their magnitudes are larger, implying a misrepresentation of the dominant momentum transfer processes in NoTCFB during RI. For the radial momentum budget analysis, the dominant processes are similar among the three experiments except for some differences in their locations and strengths.<\/jats:p>","DOI":"10.1002\/qj.4379","type":"journal-article","created":{"date-parts":[[2022,10,10]],"date-time":"2022-10-10T15:27:50Z","timestamp":1665415670000},"page":"3639-3659","update-policy":"https:\/\/doi.org\/10.1002\/crossmark_policy","source":"Crossref","is-referenced-by-count":3,"title":["Impacts of model resolution and ocean coupling on mean and eddy momentum transfer during the rapid intensification of super\u2010typhoon <i>Muifa<\/i> (2011)"],"prefix":"10.1002","volume":"148","author":[{"ORCID":"https:\/\/orcid.org\/0000-0002-5527-1540","authenticated-orcid":false,"given":"Yang","family":"Yu","sequence":"first","affiliation":[{"name":"Department of Land, Air, and Water Resources University of California  Davis California USA"},{"name":"Key Laboratory of Ocean Circulation and Waves, Institute of Oceanology and 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