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A multidecadal simulation of Atlantic tropical cyclones using a variable‐resolution global atmospheric general circulation model
dc.contributor.authorZarzycki, Colin M.en_US
dc.contributor.authorJablonowski, Christianeen_US
dc.date.accessioned2014-11-04T16:35:44Z
dc.date.availableWITHHELD_11_MONTHSen_US
dc.date.available2014-11-04T16:35:44Z
dc.date.issued2014-09en_US
dc.identifier.citationZarzycki, Colin M.; Jablonowski, Christiane (2014). "A multidecadal simulation of Atlantic tropical cyclones using a variable‐resolution global atmospheric general circulation model." Journal of Advances in Modeling Earth Systems 6(3): 805-828.en_US
dc.identifier.issn1942-2466en_US
dc.identifier.issn1942-2466en_US
dc.identifier.urihttps://hdl.handle.net/2027.42/109331
dc.description.abstractUsing a variable‐resolution option within the National Center for Atmospheric Research/Department of Energy Community Atmosphere Model (CAM) Spectral Element (SE) global model, a refined nest at 0.25° (∼28 km) horizontal resolution located over the North Atlantic is embedded within a global 1° (∼111 km) grid. The grid is designed such that fine grid cells are located where tropical cyclones (TCs) are observed to occur during the Atlantic TC season (June–November). Two simulations are compared, one with refinement and one control case with no refinement (globally uniform 1° grid). Both simulations are integrated for 23 years using Atmospheric Model Intercomparison Protocols. TCs are tracked using an objective detection algorithm. The variable‐resolution simulation produces significantly more TCs than the unrefined simulation. Storms that do form in the refined nest are much more intense, with multiple storms strengthening to Saffir‐Simpson category 3 intensity or higher. Both count and spatial distribution of TC genesis and tracks in the variable‐resolution simulation are well matched to observations and represent significant improvements over the unrefined simulation. Some degree of interannual skill is noted, with the variable‐resolution grid able to reproduce the observed connection between Atlantic TCs and the El Niño‐Southern Oscillation (ENSO). It is shown that Genesis Potential Index (GPI) is well matched between the refined and unrefined simulations, implying that the introduction of variable‐resolution does not affect the synoptic environment. Potential “upscale” effects are noted in the variable‐resolution simulation, suggesting stronger TCs in refined nests may play a role in meridional transport of momentum, heat, and moisture. Key Points Variable‐resolution models can improve the representation of tropical cyclones CAM produces realistic Atlantic TC climatology at 0.25° resolution Addition of local refinement in CAM does not impact synoptic scalesen_US
dc.publisherSpringeren_US
dc.publisherWiley Periodicals, Inc.en_US
dc.subject.otherVariable‐Resolutionen_US
dc.subject.otherHurricanesen_US
dc.subject.otherGeneral Circulation Modelsen_US
dc.subject.otherTropical Cyclonesen_US
dc.titleA multidecadal simulation of Atlantic tropical cyclones using a variable‐resolution global atmospheric general circulation modelen_US
dc.typeArticleen_US
dc.rights.robotsIndexNoFollowen_US
dc.subject.hlbsecondlevelGeological Sciencesen_US
dc.subject.hlbtoplevelScienceen_US
dc.description.peerreviewedPeer Revieweden_US
dc.description.bitstreamurlhttp://deepblue.lib.umich.edu/bitstream/2027.42/109331/1/jame20104.pdf
dc.identifier.doi10.1002/2014MS000352en_US
dc.identifier.sourceJournal of Advances in Modeling Earth Systemsen_US
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dc.owningcollnameInterdisciplinary and Peer-Reviewed


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