Global warming-induced upper-ocean freshening and the intensification of super typhoons
Super typhoons (STYs), intense tropical cyclones of the western North Pacific, rank among the most destructive natural hazards globally. The violent winds of these storms induce deep mixing of the upper ocean, resulting in strong sea surface cooling and making STYs highly sensitive to ocean density...
Main Authors: | , , , |
---|---|
Other Authors: | |
Format: | Article |
Language: | en_US |
Published: |
Nature Publishing Group
2017
|
Online Access: | http://hdl.handle.net/1721.1/107629 https://orcid.org/0000-0002-2066-2082 |
_version_ | 1811086287105425408 |
---|---|
author | Balaguru, Karthik Foltz, Gregory R. Leung, L. Ruby 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 Balaguru, Karthik Foltz, Gregory R. Leung, L. Ruby Emanuel, Kerry Andrew |
author_sort | Balaguru, Karthik |
collection | MIT |
description | Super typhoons (STYs), intense tropical cyclones of the western North Pacific, rank among the most destructive natural hazards globally. The violent winds of these storms induce deep mixing of the upper ocean, resulting in strong sea surface cooling and making STYs highly sensitive to ocean density stratification. Although a few studies examined the potential impacts of changes in ocean thermal structure on future tropical cyclones, they did not take into account changes in near-surface salinity. Here, using a combination of observations and coupled climate model simulations, we show that freshening of the upper ocean, caused by greater rainfall in places where typhoons form, tends to intensify STYs by reducing their ability to cool the upper ocean. We further demonstrate that the strengthening effect of this freshening over the period 1961–2008 is ∼53% stronger than the suppressive effect of temperature, whereas under twenty-first century projections, the positive effect of salinity is about half of the negative effect of ocean temperature changes. |
first_indexed | 2024-09-23T13:23:47Z |
format | Article |
id | mit-1721.1/107629 |
institution | Massachusetts Institute of Technology |
language | en_US |
last_indexed | 2024-09-23T13:23:47Z |
publishDate | 2017 |
publisher | Nature Publishing Group |
record_format | dspace |
spelling | mit-1721.1/1076292022-10-01T15:01:28Z Global warming-induced upper-ocean freshening and the intensification of super typhoons Balaguru, Karthik Foltz, Gregory R. Leung, L. Ruby Emanuel, Kerry Andrew Massachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciences Lorenz Center (Massachusetts Institute of Technology) Emanuel, Kerry Andrew Super typhoons (STYs), intense tropical cyclones of the western North Pacific, rank among the most destructive natural hazards globally. The violent winds of these storms induce deep mixing of the upper ocean, resulting in strong sea surface cooling and making STYs highly sensitive to ocean density stratification. Although a few studies examined the potential impacts of changes in ocean thermal structure on future tropical cyclones, they did not take into account changes in near-surface salinity. Here, using a combination of observations and coupled climate model simulations, we show that freshening of the upper ocean, caused by greater rainfall in places where typhoons form, tends to intensify STYs by reducing their ability to cool the upper ocean. We further demonstrate that the strengthening effect of this freshening over the period 1961–2008 is ∼53% stronger than the suppressive effect of temperature, whereas under twenty-first century projections, the positive effect of salinity is about half of the negative effect of ocean temperature changes. United States. Dept. of Energy. Regional & Global Climate Modeling Program 2017-03-22T13:27:30Z 2017-03-22T13:27:30Z 2016-11 2016-04 Article http://purl.org/eprint/type/JournalArticle 2041-1723 http://hdl.handle.net/1721.1/107629 Balaguru, Karthik et al. “Global Warming-Induced Upper-Ocean Freshening and the Intensification of Super Typhoons.” Nature Communications 7 (2016): 13670. https://orcid.org/0000-0002-2066-2082 en_US http://dx.doi.org/10.1038/ncomms13670 Nature Communications Creative Commons Attribution 4.0 International License http://creativecommons.org/licenses/by/4.0/ application/pdf Nature Publishing Group Nature |
spellingShingle | Balaguru, Karthik Foltz, Gregory R. Leung, L. Ruby Emanuel, Kerry Andrew Global warming-induced upper-ocean freshening and the intensification of super typhoons |
title | Global warming-induced upper-ocean freshening and the intensification of super typhoons |
title_full | Global warming-induced upper-ocean freshening and the intensification of super typhoons |
title_fullStr | Global warming-induced upper-ocean freshening and the intensification of super typhoons |
title_full_unstemmed | Global warming-induced upper-ocean freshening and the intensification of super typhoons |
title_short | Global warming-induced upper-ocean freshening and the intensification of super typhoons |
title_sort | global warming induced upper ocean freshening and the intensification of super typhoons |
url | http://hdl.handle.net/1721.1/107629 https://orcid.org/0000-0002-2066-2082 |
work_keys_str_mv | AT balagurukarthik globalwarminginducedupperoceanfresheningandtheintensificationofsupertyphoons AT foltzgregoryr globalwarminginducedupperoceanfresheningandtheintensificationofsupertyphoons AT leunglruby globalwarminginducedupperoceanfresheningandtheintensificationofsupertyphoons AT emanuelkerryandrew globalwarminginducedupperoceanfresheningandtheintensificationofsupertyphoons |