Effect of Upper-Ocean Evolution on Projected Trends in Tropical Cyclone Activity
Recent work has highlighted the possible importance of changing upper-ocean thermal and density stratification on observed and projected changes in tropical cyclone activity. Here seven CMIP phase 5 (CMIP5)-generation climate model simulations are downscaled under IPCC representative concentration p...
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| Format: | Article |
| Language: | en_US |
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American Meteorological Society
2016
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| Online Access: | http://hdl.handle.net/1721.1/102255 https://orcid.org/0000-0002-2066-2082 |
| _version_ | 1826203673218252800 |
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| author | Emanuel, Kerry Andrew |
| author2 | Massachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciences |
| author_facet | Massachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciences Emanuel, Kerry Andrew |
| author_sort | Emanuel, Kerry Andrew |
| collection | MIT |
| description | Recent work has highlighted the possible importance of changing upper-ocean thermal and density stratification on observed and projected changes in tropical cyclone activity. Here seven CMIP phase 5 (CMIP5)-generation climate model simulations are downscaled under IPCC representative concentration pathway 8.5 using a coupled atmosphere–ocean tropical cyclone model, generating 100 events per year in the western North Pacific from 2006 to 2100. A control downscaling in which the upper-ocean thermal structure is fixed at its monthly values in the year 2006 is compared to one in which the upper ocean is allowed to evolve, as derived from the CMIP5 models. As found in earlier work, the thermal stratification generally increases as the climate warms, leading to increased ocean mixing–induced negative feedback on tropical cyclone intensity. While trends in the frequency of storms are unaffected, the increasing stratification of the upper ocean leads to a 13% reduction in the increase of tropical cyclone power dissipation over the twenty-first century, averaged across the seven climate models. Much of this reduction is associated with a moderation of the increase in the frequency of category-5 storms. |
| first_indexed | 2024-09-23T12:41:15Z |
| format | Article |
| id | mit-1721.1/102255 |
| institution | Massachusetts Institute of Technology |
| language | en_US |
| last_indexed | 2024-09-23T12:41:15Z |
| publishDate | 2016 |
| publisher | American Meteorological Society |
| record_format | dspace |
| spelling | mit-1721.1/1022552022-10-01T10:31:01Z Effect of Upper-Ocean Evolution on Projected Trends in Tropical Cyclone Activity Emanuel, Kerry Andrew Massachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciences Lorenz Center (Massachusetts Institute of Technology) Emanuel, Kerry Andrew Recent work has highlighted the possible importance of changing upper-ocean thermal and density stratification on observed and projected changes in tropical cyclone activity. Here seven CMIP phase 5 (CMIP5)-generation climate model simulations are downscaled under IPCC representative concentration pathway 8.5 using a coupled atmosphere–ocean tropical cyclone model, generating 100 events per year in the western North Pacific from 2006 to 2100. A control downscaling in which the upper-ocean thermal structure is fixed at its monthly values in the year 2006 is compared to one in which the upper ocean is allowed to evolve, as derived from the CMIP5 models. As found in earlier work, the thermal stratification generally increases as the climate warms, leading to increased ocean mixing–induced negative feedback on tropical cyclone intensity. While trends in the frequency of storms are unaffected, the increasing stratification of the upper ocean leads to a 13% reduction in the increase of tropical cyclone power dissipation over the twenty-first century, averaged across the seven climate models. Much of this reduction is associated with a moderation of the increase in the frequency of category-5 storms. National Science Foundation (U.S.) (Grant 1342810) 2016-04-19T14:52:10Z 2016-04-19T14:52:10Z 2015-10 2015-08 Article http://purl.org/eprint/type/JournalArticle 0894-8755 1520-0442 http://hdl.handle.net/1721.1/102255 Emanuel, Kerry. “Effect of Upper-Ocean Evolution on Projected Trends in Tropical Cyclone Activity.” J. Climate 28, no. 20 (October 2015): 8165–8170. © 2015 American Meteorological Society https://orcid.org/0000-0002-2066-2082 en_US http://dx.doi.org/10.1175/jcli-d-15-0401.1 Journal of Climate Article is made available in accordance with the publisher's policy and may be subject to US copyright law. Please refer to the publisher's site for terms of use. application/pdf American Meteorological Society American Meteorological Society |
| spellingShingle | Emanuel, Kerry Andrew Effect of Upper-Ocean Evolution on Projected Trends in Tropical Cyclone Activity |
| title | Effect of Upper-Ocean Evolution on Projected Trends in Tropical Cyclone Activity |
| title_full | Effect of Upper-Ocean Evolution on Projected Trends in Tropical Cyclone Activity |
| title_fullStr | Effect of Upper-Ocean Evolution on Projected Trends in Tropical Cyclone Activity |
| title_full_unstemmed | Effect of Upper-Ocean Evolution on Projected Trends in Tropical Cyclone Activity |
| title_short | Effect of Upper-Ocean Evolution on Projected Trends in Tropical Cyclone Activity |
| title_sort | effect of upper ocean evolution on projected trends in tropical cyclone activity |
| url | http://hdl.handle.net/1721.1/102255 https://orcid.org/0000-0002-2066-2082 |
| work_keys_str_mv | AT emanuelkerryandrew effectofupperoceanevolutiononprojectedtrendsintropicalcycloneactivity |