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Climate change can affect tropical cyclones in a variety of ways: an intensification of rainfall and wind speed, a decrease in overall frequency, an increase in the frequency of very intense storms and a poleward extension of where the cyclones reach maximum intensity are among the possible consequences of human-induced climate change.^[1] Tropical cyclones use warm, moist air as their source of energy or "fuel". As climate change is warming ocean temperatures, there is potentially more of this fuel available.^[2] Between 1979 and 2017, there was a global increase in the proportion of tropical cyclones of Category 3 and higher on the Saffir–Simpson scale. The trend was most clear in the North Atlantic and in the Southern Indian Ocean. In the North Pacific, tropical cyclones have been moving poleward into colder waters and there was no increase in intensity over this period.^[3] With 2 °C (3.6 °F) warming, a greater percentage (+13%) of tropical cyclones are expected to reach Category 4 and 5 strength.^[1] A 2019 study indicates that climate change has been driving the observed trend of rapid intensification of tropical cyclones in the Atlantic basin. Rapidly intensifying cyclones are hard to forecast and therefore pose additional risk to coastal communities.^[4]

Warmer air can hold more water vapor: the theoretical maximum water vapor content is given by the Clausius–Clapeyron relation, which yields ≈7% increase in water vapor in the atmosphere per 1 °C (1.8 °F) warming.^[5]^[6] All models that were assessed in a 2019 review paper show a future increase of rainfall rates.^[1] Additional sea level rise will increase storm surge levels.^[7]^[8] It is plausible that extreme wind waves see an increase as a consequence of changes in tropical cyclones, further exacerbating storm surge dangers to coastal communities.^[9] The compounding effects from floods, storm surge, and terrestrial flooding (rivers) are projected to increase due to global warming.^[8]

There is currently no consensus on how climate change will affect the overall frequency of tropical cyclones.^[1] A majority of climate models show a decreased frequency in future projections.^[9] For instance, a 2020 paper comparing nine high-resolution climate models found robust decreases in frequency in the Southern Indian Ocean and the Southern Hemisphere more generally, while finding mixed signals for Northern Hemisphere tropical cyclones.^[10] Observations have shown little change in the overall frequency of tropical cyclones worldwide,^[11] with increased frequency in the North Atlantic and central Pacific, and significant decreases in the southern Indian Ocean and western North Pacific.^[12] There has been a poleward expansion of the latitude at which the maximum intensity of tropical cyclones occurs, which may be associated with climate change.^[13] In the North Pacific, there may also have been an eastward expansion.^[7] Between 1949 and 2016, there was a slowdown in tropical cyclone translation speeds. It is unclear still to what extent this can be attributed to climate change: climate models do not all show this feature.^[9]

Background

A tropical cyclone is a rapidly rotating storm system characterized by a low-pressure center, a closed low-level atmospheric circulation,

strong winds and a spiral arrangement of thunderstorms that produce heavy rain or squalls. The majority of these systems form each year in one of seven tropical cyclone basins, which are monitored by a variety of meteorological services and warning centres.

The factors that determine tropical cyclone activity are relatively well understood: warmer sea levels are favourable to tropical cyclones, as well as an unstable and moist mid-troposphere, while vertical wind shear suppresses them. All of these factors will change under climate change, but is not always clear which factor dominates.^[14]

Tropical cyclones are known as hurricanes in the Atlantic Ocean and the northeastern Pacific Ocean, typhoons in the northwestern Pacific Ocean, and cyclones in the southern Pacific or the Indian Ocean.^[15] Fundamentally, they are all the same type of storm.

Data and models

Measurement

Based on satellite imagery, the Dvorak technique is the primary technique used to estimate globally the tropical cyclone intensity.^[16]

The Potential Intensity (PI) of tropical cyclones can be computed from observed data, primarily derived from vertical profiles of temperature, humidity and sea surface temperatures (SSTs). The convective available potential energy (CAPE), was computed from radiosonde stations in parts of the tropics from 1958 to 1997, but is considered to be of poor quality. The Power Dissipation Index (PDI) represents the total power dissipation for the North Atlantic and western North Pacific, and is strongly correlated with tropical SSTs.^[17] Various tropical cyclone scales exist to classify a system.

Historical record

Since the satellite era, which began around 1970, trends are considered to be robust enough in regards to the connection of storms and sea surface temperatures. Agreement exists that there were active storm periods in the more distant past, but the sea surface temperature related Power Dissipation Index was not as high.^[17] Paleotempestology is the science of past tropical cyclone activity by means of geological proxies (flood sediment), or historical documentary records, such as shipwrecks or tree ring anomalies. As of 2019^[update], paleoclimate studies are not yet sufficiently consistent to draw conclusions for wider regions, but they do provide some useful information about specific locations.^[18]

Modelling tropical cyclones

Climate models are used to study expected future changes in cyclonic activity. Lower-resolution climate models cannot represent convection directly, and instead use parametrizations to approximate the smaller scale processes. This poses difficulties for tropical cyclones, as convection is an essential part of tropical cyclone physics.

Higher-resolution global models and regional climate models may be more computer-intensive to run, making it difficult to simulate enough tropical cyclones for robust statistical analysis. However, with growing advancements in technology, climate models have improved simulation abilities for tropical cyclone frequency and intensity.^[19]^[20]

One challenge that scientists face when modeling is determining whether the recent changes in tropical cyclones are associated with anthropogenic forcing, or if these changes are still within their natural variability.^[21] This is most apparent when examining tropical cyclones at longer temporal resolutions. One study found a decreasing trend in tropical storms along the eastern Australian coast over a century-long historical record.^[22]

Changes in tropical cyclones

Climate change may affect tropical cyclones in a variety of ways: an intensification of rainfall and wind speed, a decrease in overall frequency, an increase in frequency of very intense storms and a poleward extension of where the cyclones reach maximum intensity are among the possible consequences of human-induced climate change.^[23]

Rainfall

Warmer air can hold more water vapor: the theoretical maximum water vapor content is given by the Clausius–Clapeyron relation, which yields ≈7% increase in water vapor in the atmosphere per 1 °C warming.^[24]^[25] All models that were assessed in a 2019 review paper show a future increase of rainfall rates, which is the rain that falls per hour.^[23] The World Meteorological Organization stated in 2017 that the quantity of rainfall from Hurricane Harvey had very likely been increased by climate change.^[26]^[27]

A tropical cyclone's rainfall area (in contrast to rate) is primarily controlled by its environmental sea surface temperature (SST) – relative to the tropical mean SST, called the relative sea surface temperature. Rainfall will expand outwards as the relative SST increases, associated with an expansion of a storm wind field. The largest tropical cyclones are observed in the western North Pacific tropics, where the largest values of relative SST and mid-tropospheric relative humidity are located. Assuming that ocean temperatures rise uniformly, a warming climate is not likely to impact rainfall area.^[28]

Intensity

Tropical cyclones use warm, moist air as their source of energy or "fuel". As climate change is warming ocean temperatures, there is potentially more of this fuel available.^[30] A study published in 2012 suggests that SSTs may be valuable as a proxy to measure potential intensity (PI) of tropical cyclones, as cyclones are sensitive to ocean basin temperatures.^[31] Between 1979 and 2017, there was a global increase in the proportion of tropical cyclones of Category 3 and higher on the Saffir–Simpson scale, which are cyclones with wind speeds over 178 km per hour. The trend was most clear in the North Atlantic and in the Southern Indian Ocean. In the North Pacific, tropical cyclones have been moving poleward into colder waters and there was no increase in intensity over this period.^[32] With 2 °C warming, a greater percentage (+13%) of tropical cyclones are expected to reach Category 4 and 5 strength.^[23] A study of 2020's storms of at least tropical storm-strength concluded that human-induced climate change increased extreme 3-hourly storm rainfall rates by 10%, and extreme 3-day accumulated rainfall amounts by 5%, and for hurricane-strength storms the figures increased to 11% and 8%.^[33]

Climate change has likely been driving the observed trend of rapid intensification of tropical cyclones in the Atlantic basin, with the proportion of storms undergoing intensification nearly doubling over the years 1982 to 2009.^[34]^[35]Rapidly intensifying cyclones are hard to forecast and pose additional risk to coastal communities.^[36] Storms have also begun to decay more slowly once they make landfall, threatening areas further inland than in the past.^[37] The 2020 Atlantic hurricane season was exceptionally active and broke numerous records for frequency and intensity of storms.^[38]

Frequency

There is no consensus on how climate change will affect the overall frequency of tropical cyclones.^[23] A majority of climate models show a decreased frequency in future projections.^[18] For instance, a 2020 paper comparing nine high-resolution climate models found robust decreases in frequency in the Southern Indian Ocean and the Southern Hemisphere more generally, while finding mixed signals for Northern Hemisphere tropical cyclones.^[39] Observations have shown little change in the overall frequency of tropical cyclones worldwide.^[40]

A study published in 2015 concluded that there would be more tropical cyclones in a cooler climate, and that tropical cyclone genesis is possible with sea surface temperatures below 26 °C.^[41]^[42] With warmers sea surface temperatures, especially in the Southern Hemisphere, in tandem with increased levels of carbon dioxide, it is likely tropical cyclone frequency will be reduced in the future.^[31]^[43]

Research conducted by Murakami et al. following the 2015 hurricane season in the eastern and central Pacific Ocean where a record number of tropical cyclones and three simultaneous category 4 hurricanes occurred, concludes that greenhouse gas forcing enhances subtropical Pacific warming which they project will increase the frequency of extremely active tropical cyclones in this area.^[44]

Storm tracks

There has been a poleward expansion of the latitude at which the maximum intensity of tropical cyclones occurs, which may be associated with climate change.^[45] In the North Pacific, there may also be an eastward expansion.^[46] Between 1949 and 2016, there was a slowdown in tropical cyclone translation speeds. It is unclear still to what extent this can be attributed to climate change: climate models do not all show this feature.^[18]

Storm surges and flood hazards

Additional sea level rise will increase storm surge levels.^[46]^[47] It is plausible that extreme wind waves see an increase as a consequence of changes in tropical cyclones, further exacerbating storm surge dangers to coastal communities.^[18] Between 1923 and 2008, storm surge incidents along the US Atlantic coast showed a positive trend.^[48] A 2017 study looked at compounding effects from floods, storm surge, and terrestrial flooding (rivers), and projects an increase due to climate change.^[47]^[49] However, scientists are still uncertain whether recent increases of storm surges are a response to anthropogenic climate change.^[50]

Tropical cyclones in different basins

Hurricanes

Studies conducted in 2008 and 2016 looked at the duration of the Atlantic hurricane season, and found it may be getting longer, particular south of 30°N and east of 75°W, or the tendency toward more early- and late-season storms, correlated to warming sea surface temperatures. However, uncertainty is still high, and one study found no trend, another mixed results.^[51]

A 2011 study linked increased activity of intense hurricanes in the North Atlantic with a northward shift and amplification of convective activities from the African easterly waves (AEWs).^[52]In addition to cyclone intensity, both size and translation speed have been shown to be substantial contributors to the impacts resulting from hurricane passage. A 2014 study investigated the response of AEWs to high emissions scenarios, and found increases in regional temperature gradients, convergence and uplift along the Intertropical Front of Africa, resulting in strengthening of the African easterly waves, affecting the climate over West Africa and the larger Atlantic basin.^[53]

A 2017 study concluded that the 2015 highly active hurricane season could not be attributed solely to a strong El Niño event. Instead, subtropical warming was an important factor as well, a feature more common as a consequence of climate change.^[44] A 2019 study found that increasing evaporation and the larger capability of the atmosphere to hold water vapor linked to climate change, already increased the amount of rainfall from hurricanes Katrina, Irma and Maria by 4 to 9 percent. Future increases of up to 30% were projected.^[54]

A 2018 study found no significant trends in landfalling hurricane frequency nor intensity for the continental United States since 1900. Furthermore, growth in coastal populations and regional wealth served as the overwhelming drivers of observed increases in hurricane-related damage.^[55]

Typhoons

Research based on records from Japan and Hawaii indicate that typhoons in the north-west Pacific intensified by 12–15% on average since 1977. The observed strongest typhoons doubled, or tripled in some regions, the intensity of particular landfalling systems is most pronounced. This uptick in storm intensity affects coastal populations in China, Japan, Korea and the Philippines, and has been attributed to warming ocean waters. The authors noted that it is not yet clear to what extent global warming caused the increased water temperatures, but observations are consistent with what the IPCC projects for warming of sea surface temperatures.^[56] Vertical wind shear has seen decreasing trends in and around China, creating more favourable conditions for intense tropical cyclones. This is mainly in response to the weakening of the East Asian summer monsoon, a consequence of global warming.^[57]

Risk management and adaptation

The most effective strategy to manage risks has been the development of early warning systems.^[58] A further policy that would mitigate risks of flooding is reforestation of inland areas in order to strengthen the soil of the communities and reduce coastal inundation.^[59] It is also recommended that local schools, churches, and other community infrastructure be permanently equipped to become cyclone shelters.^[59] Focusing on applying resources towards immediate relief to those affected may divert attention from more long-term solutions. This is further exacerbated in lower-income communities and countries as they suffer most from the consequences of tropical cyclones.^[59]

Pacific region

Specific national and supranational decisions have already been made and are being implemented. The Framework for Resilient Development in the Pacific (FRDP) has been instituted to strengthen and better coordinate disaster response and climate change adaptation among nations and communities in the region. Specific nations such as Tonga and the Cook Islands in the Southern Pacific under this regime have developed a Joint National Action Plan on Climate Change and Disaster Risk Management (JNAP) to coordinate and execute responses to the rising risk for climate change.^[59]^[60] These countries have identified the most vulnerable areas of their nations, generated national and supranational policies to be implemented, and provided specific goals and timelines to achieve these goals.^[60] These actions to be implemented include reforestation, building of levees and dams, creation of early warning systems, reinforcing existing communication infrastructure, finding new sources of fresh water, promoting and subsidizing the proliferation renewable energy, improving irrigation techniques to promote sustainable agriculture, increase public education efforts on sustainable measures, and lobbying internationally for the increased use of renewable energy sources.^[60]

United States

In the United States, there have been several initiatives taken to better prepare for the strengthening of hurricanes, such as preparing local emergency shelters, building sand dunes and levees, and reforestation initiatives.^[61] Despite better modeling capabilities of hurricanes, property damage has increased dramatically.^[62] The National Flood Insurance Program incentivizes people to re-build houses in flood-prone areas, and thereby hampers adaptation to increased risk from hurricanes and sea level rise.^[63] Due to the wind shear and storm surge, a building with a weak building envelope is subject to more damages. Risk assessment using climate models help determine the structural integrity of residential buildings in hurricane-prone areas.^[64]

Some ecosystems, such as marshes, mangroves, and coral reefs, can serve as a natural obstacle to coastal erosion, storm surges, and wind damage caused by hurricanes.^[65]^[66] These natural habitats are seen to be more cost-effective as they serve as a carbon sink and support biodiversity of a region.^[66] ^[67] Although there is substantial evidence of natural habitats being the more beneficial barrier for tropical cyclones, built defenses are often the primary solution for government agencies and decision makers.^[68] A study published in 2015, which assessed the feasibility of natural, engineered, and hybrid risk-mitigation to tropical cyclones in Freeport, Texas, found that incorporating natural ecosystems into risk-mitigation plans could reduce flood heights and ease the cost of built defenses in the future.^[68]

Media and public perception

The destruction from early 21st century Atlantic Ocean hurricanes, such as Hurricanes Katrina, Wilma, and Sandy, caused a substantial upsurge in interest in the subject of climate change and hurricanes by news media and the wider public, and concerns that global climatic change may have played a significant role in those events. In 2005 and 2017, related polling of populations affected by hurricanes concluded in 2005 that 39 percent of Americans believed climate change helped to fuel the intensity of hurricanes, rising to 55 percent in September 2017.^[69]

After Typhoon Meranti in 2016, risk perception in China was not measured to increase. However, there was a clear rise in support for personal and community action against climate change.^[70] In Taiwan, people that had lived through a typhoon did not express more anxiety about climate change. The survey did find a positive correlation between anxiety about typhoons and anxiety about climate change.^[71]

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^ James P. Kossin; Kerry A. Emanuel; Gabriel A. Vecchi (2014). "The poleward migration of the location of tropical cyclone maximum intensity". Nature. 509 (7500): 349–352. Bibcode:2014Natur.509..349K. doi:10.1038/nature13278. hdl:1721.1/91576. PMID 24828193. S2CID 4463311.
^ ^a ^b Collins, M.; Sutherland, M.; Bouwer, L.; Cheong, S.-M.; et al. (2019). "Chapter 6: Extremes, Abrupt Changes and Managing Risks" (PDF). IPCC Special Report on the Ocean and the Cryosphere in a Changing Climate, 2019. p. 603.
^ ^a ^b "Hurricane Harvey shows how we underestimate flooding risks in coastal cities, scientists say". The Washington Post. August 29, 2017.
^ Grinsted A, Moore JC, Jevrejeva S. Homogeneous record of Atlantic hurricane surge threat since 1923. Proc Natl Acad Sci USA 2012, 109:19601–19605.
^ Matthew, Richard A.; Sanders, Brett F.; Aghakouchak, Amir; Salvadori, Gianfausto; Moftakhari, Hamed R. (2017). "Compounding effects of sea level rise and fluvial flooding". Proceedings of the National Academy of Sciences. 114 (37): 9785–9790. Bibcode:2017PNAS..114.9785M. doi:10.1073/pnas.1620325114. PMC 5603992. PMID 28847932.
^ Knutson, Thomas; Camargo, Suzana J.; Chan, Johnny C. L.; Emanuel, Kerry; Ho, Chang-Hoi; Kossin, James; Mohapatra, Mrutyunjay; Satoh, Masaki; Sugi, Masato; Walsh, Kevin; Wu, Liguang (2019-10-01). "Tropical Cyclones and Climate Change Assessment: Part I: Detection and Attribution". Bulletin of the American Meteorological Society. 100 (10): 1987–2007. Bibcode:2019BAMS..100.1987K. doi:10.1175/BAMS-D-18-0189.1. hdl:1721.1/125577. ISSN 0003-0007. S2CID 191139413.
^ Jeff Masters (November 1, 2017). "November Atlantic Hurricane Outlook: The Season is Not Over Yet". Wunderground.
^ Wang; Gillies (2011). "Observed Change in Sahel Rainfall, Circulations, African Easterly Waves, and Atlantic Hurricanes Since 1979". International Journal of Geophysics. 2011: 1–14. doi:10.1155/2011/259529.
^ Christopher Bryan Skinner; Noah S. Diffenbaugh (2014). "Projected changes in African easterly wave intensity and track in response to greenhouse forcing". Proceedings of the National Academy of Sciences of the United States of America. 111 (19): 6882–6887. Bibcode:2014PNAS..111.6882S. doi:10.1073/pnas.1319597111. PMC 4024927. PMID 24778244.
^ Davidson, Jordan (July 12, 2019). "Study: Climate Change Linked to More Rain in Hurricanes". Ecowatch. Retrieved 14 July 2019.
^ Klotzbach, Philip J.; Bowen, Steven G.; Pielke, Roger; Bell, Michael (2018-07-01). "Continental U.S. Hurricane Landfall Frequency and Associated Damage: Observations and Future Risks". Bulletin of the American Meteorological Society. 99 (7): 1359–1376. Bibcode:2018BAMS...99.1359K. doi:10.1175/BAMS-D-17-0184.1. ISSN 0003-0007.
^ "Asian typhoons becoming more intense, study finds". The Guardian. 2016.
^ Liu, Lu; Wang, Yuqing; Zhan, Ruifen; Xu, Jing; Duan, Yihong (2020-05-01). "Increasing Destructive Potential of Landfalling Tropical Cyclones over China". Journal of Climate. 33 (9): 3731–3743. Bibcode:2020JCli...33.3731L. doi:10.1175/JCLI-D-19-0451.1. ISSN 0894-8755. S2CID 213900279.
^ Collins, M.; Sutherland, M.; Bouwer, L.; Cheong, S.-M.; et al. (2019). "Chapter 6: Extremes, Abrupt Changes and Managing Risks" (PDF). IPCC SROCC. p. 606.
^ ^a ^b ^c ^d Thomas, Adelle; Pringle, Patrick; Pfleiderer, Peter; Schleussner, Car-Friedrich (April 14, 2017). "Topical Cyclones: Impacts, the link to Climate Change and Adaptation" (PDF). IMPACT.
^ ^a ^b ^c "Prevention Web".
^ Moser, Susan (2005). "Impact assessments and policy responses to sea-level rise in three US states: An exploration of human-dimension uncertainties". Global Environmental Change. 15 (4): 353–369. doi:10.1016/j.gloenvcha.2005.08.002.
^ Sadowski, Nicole Cornell; Sutter, Daniel (2008-01-01). "Mitigation motivated by past experience: Prior hurricanes and damages". Ocean & Coastal Management. 51 (4): 303–313. doi:10.1016/j.ocecoaman.2007.09.003. ISSN 0964-5691.
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^ Li, Yue; Ellingwood, Bruce R. (2006-06-01). "Hurricane damage to residential construction in the US: Importance of uncertainty modeling in risk assessment". Engineering Structures. 28 (7): 1009–1018. doi:10.1016/j.engstruct.2005.11.005. ISSN 0141-0296.
^ Shepard, C. C., Crain, C. M., & Beck, M. W. (2011). The protective role of coastal marshes: a systematic review and meta-analysis. PLOS ONE, 6(11), e27374.
^ ^a ^b Ferrario, Filippo; Beck, Michael W.; Storlazzi, Curt D.; Micheli, Fiorenza; Shepard, Christine C.; Airoldi, Laura (September 2014). "The effectiveness of coral reefs for coastal hazard risk reduction and adaptation". Nature Communications. 5 (1): 3794. Bibcode:2014NatCo...5.3794F. doi:10.1038/ncomms4794. ISSN 2041-1723. PMC 4354160. PMID 24825660.
^ Barbier, Edward B., Sally D. Hacker, Chris Kennedy, Evamaria W. Koch, Adrian C. Stier, and Brian R. Silliman. "The value of estuarine and coastal ecosystem services." Ecological monographs 81, no. 2 (2011): 169–193.
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^ "Majority of Americans now say climate change makes hurricanes more intense". The Washington Post. 2017.
^ Wu, Wenhao; Zheng, Junjie; Fang, Qinhua (2020-07-10). "How a typhoon event transforms public risk perception of climate change: A study in China". Journal of Cleaner Production. 261: 121163. doi:10.1016/j.jclepro.2020.121163. ISSN 0959-6526. S2CID 216412671.
^ Sun, Yingying; Han, Ziqiang (2018). "Climate Change Risk Perception in Taiwan: Correlation with Individual and Societal Factors". International Journal of Environmental Research and Public Health. 15 (1): 91. doi:10.3390/ijerph15010091. PMC 5800190. PMID 29316685.

External links

Climate scientist describes physics behind expected increase in storm strength due to climate change (Video September 2017)

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[4] Collins, M.; Sutherland, M.; Bouwer, L.; Cheong, S.-M.; et al. (2019). "Chapter 6: Extremes, Abrupt Changes and Managing Risks" (PDF). IPCC Special Report on the Ocean and Cryosphere in a Changing Climate. p. 602. Archived (PDF) from the original on December 20, 2019. Retrieved October 6, 2020.

[5] Thomas R. Knutson; Joseph J. Sirutis; Ming Zhao (2015). "Global Projections of Intense Tropical Cyclone Activity for the Late Twenty-First Century from Dynamical Downscaling of CMIP5/RCP4.5 Scenarios". Journal of Climate. 28 (18): 7203–7224. Bibcode:2015JCli...28.7203K. doi:10.1175/JCLI-D-15-0129.1. Archived from the original on January 5, 2020. Retrieved October 6, 2020.

[knutson_20132-6] Knutson; et al. (2013). "Dynamical Downscaling Projections of Late 21st Century Atlantic Hurricane Activity: CMIP3 and CMIP5 Model-based Scenarios". Journal of Climate. 26 (17): 6591–6617. Bibcode:2013JCli...26.6591K. doi:10.1175/JCLI-D-12-00539.1. S2CID 129571840. Archived from the original on October 5, 2020. Retrieved October 6, 2020.

[:62-7] Collins, M.; Sutherland, M.; Bouwer, L.; Cheong, S.-M.; et al. (2019). "Chapter 6: Extremes, Abrupt Changes and Managing Risks" (PDF). IPCC Special Report on the Ocean and Cryosphere in a Changing Climate. p. 603. Archived (PDF) from the original on December 20, 2019. Retrieved October 6, 2020.

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[43] Held, Isaac M.; Zhao, Ming (2011-10-15). "The Response of Tropical Cyclone Statistics to an Increase in CO2 with Fixed Sea Surface Temperatures". Journal of Climate. 24 (20): 5353–5364. Bibcode:2011JCli...24.5353H. doi:10.1175/JCLI-D-11-00050.1. ISSN 0894-8755. OSTI 1564909.

[:8-44] Murakami, Hiroyuki; Vecchi, Gabriel A.; Delworth, Thomas L.; Wittenberg, Andrew T.; Underwood, Seth; Gudgel, Richard; Yang, Xiaosong; Jia, Liwei; Zeng, Fanrong; Paffendorf, Karen; Zhang, Wei (2017). "Dominant Role of Subtropical Pacific Warming in Extreme Eastern Pacific Hurricane Seasons: 2015 and the Future". Journal of Climate. 30 (1): 243–264. Bibcode:2017JCli...30..243M. doi:10.1175/JCLI-D-16-0424.1. ISSN 0894-8755.

[45] James P. Kossin; Kerry A. Emanuel; Gabriel A. Vecchi (2014). "The poleward migration of the location of tropical cyclone maximum intensity". Nature. 509 (7500): 349–352. Bibcode:2014Natur.509..349K. doi:10.1038/nature13278. hdl:1721.1/91576. PMID 24828193. S2CID 4463311.

[:6-46] Collins, M.; Sutherland, M.; Bouwer, L.; Cheong, S.-M.; et al. (2019). "Chapter 6: Extremes, Abrupt Changes and Managing Risks" (PDF). IPCC Special Report on the Ocean and the Cryosphere in a Changing Climate, 2019. p. 603.

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[48] Grinsted A, Moore JC, Jevrejeva S. Homogeneous record of Atlantic hurricane surge threat since 1923. Proc Natl Acad Sci USA 2012, 109:19601–19605.

[49] Matthew, Richard A.; Sanders, Brett F.; Aghakouchak, Amir; Salvadori, Gianfausto; Moftakhari, Hamed R. (2017). "Compounding effects of sea level rise and fluvial flooding". Proceedings of the National Academy of Sciences. 114 (37): 9785–9790. Bibcode:2017PNAS..114.9785M. doi:10.1073/pnas.1620325114. PMC 5603992. PMID 28847932.

[50] Knutson, Thomas; Camargo, Suzana J.; Chan, Johnny C. L.; Emanuel, Kerry; Ho, Chang-Hoi; Kossin, James; Mohapatra, Mrutyunjay; Satoh, Masaki; Sugi, Masato; Walsh, Kevin; Wu, Liguang (2019-10-01). "Tropical Cyclones and Climate Change Assessment: Part I: Detection and Attribution". Bulletin of the American Meteorological Society. 100 (10): 1987–2007. Bibcode:2019BAMS..100.1987K. doi:10.1175/BAMS-D-18-0189.1. hdl:1721.1/125577. ISSN 0003-0007. S2CID 191139413.

[51] Jeff Masters (November 1, 2017). "November Atlantic Hurricane Outlook: The Season is Not Over Yet". Wunderground.

[52] Wang; Gillies (2011). "Observed Change in Sahel Rainfall, Circulations, African Easterly Waves, and Atlantic Hurricanes Since 1979". International Journal of Geophysics. 2011: 1–14. doi:10.1155/2011/259529.

[53] Christopher Bryan Skinner; Noah S. Diffenbaugh (2014). "Projected changes in African easterly wave intensity and track in response to greenhouse forcing". Proceedings of the National Academy of Sciences of the United States of America. 111 (19): 6882–6887. Bibcode:2014PNAS..111.6882S. doi:10.1073/pnas.1319597111. PMC 4024927. PMID 24778244.

[54] Davidson, Jordan (July 12, 2019). "Study: Climate Change Linked to More Rain in Hurricanes". Ecowatch. Retrieved 14 July 2019.

[55] Klotzbach, Philip J.; Bowen, Steven G.; Pielke, Roger; Bell, Michael (2018-07-01). "Continental U.S. Hurricane Landfall Frequency and Associated Damage: Observations and Future Risks". Bulletin of the American Meteorological Society. 99 (7): 1359–1376. Bibcode:2018BAMS...99.1359K. doi:10.1175/BAMS-D-17-0184.1. ISSN 0003-0007.

[56] "Asian typhoons becoming more intense, study finds". The Guardian. 2016.

[57] Liu, Lu; Wang, Yuqing; Zhan, Ruifen; Xu, Jing; Duan, Yihong (2020-05-01). "Increasing Destructive Potential of Landfalling Tropical Cyclones over China". Journal of Climate. 33 (9): 3731–3743. Bibcode:2020JCli...33.3731L. doi:10.1175/JCLI-D-19-0451.1. ISSN 0894-8755. S2CID 213900279.

[58] Collins, M.; Sutherland, M.; Bouwer, L.; Cheong, S.-M.; et al. (2019). "Chapter 6: Extremes, Abrupt Changes and Managing Risks" (PDF). IPCC SROCC. p. 606.

[:0-59] Thomas, Adelle; Pringle, Patrick; Pfleiderer, Peter; Schleussner, Car-Friedrich (April 14, 2017). "Topical Cyclones: Impacts, the link to Climate Change and Adaptation" (PDF). IMPACT.

[:1-60] "Prevention Web".

[:2-61] Moser, Susan (2005). "Impact assessments and policy responses to sea-level rise in three US states: An exploration of human-dimension uncertainties". Global Environmental Change. 15 (4): 353–369. doi:10.1016/j.gloenvcha.2005.08.002.

[62] Sadowski, Nicole Cornell; Sutter, Daniel (2008-01-01). "Mitigation motivated by past experience: Prior hurricanes and damages". Ocean & Coastal Management. 51 (4): 303–313. doi:10.1016/j.ocecoaman.2007.09.003. ISSN 0964-5691.

[63] Craig, Robin Kundis (2019). "Coastal adaptation, government-subsidized insurance, and perverse incentives to stay". Climatic Change. 152 (2): 215–226. Bibcode:2019ClCh..152..215C. doi:10.1007/s10584-018-2203-5. ISSN 1573-1480. S2CID 158455505.

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@@ Line 2: / Line 2: @@
 <noinclude></noinclude>
 [[File:North Atlantic Tropical Cyclone Activity 1949–2015 Power Dissipation Index PDI NOAA EPA.png|thumb|upright=1.35|North Atlantic tropical cyclone activity according to the Power Dissipation Index, 1949–2015. Sea surface temperature has been plotted alongside the PDI to show how they compare. The lines have been smoothed using a five-year weighted average, plotted at the middle year.]]
-[[Climate change]] can affect [[Tropical cyclone|tropical cyclones]] in a variety of ways: an intensification of rainfall and wind speed, a decrease in overall frequency, an increase in the frequency of very intense storms and a poleward extension of where the cyclones reach maximum intensity are among the possible consequences of human-induced climate change.<ref name=":52">{{Cite journal |last1=Knutson |first1=Thomas |last2=Camargo |first2=Suzana J. |last3=Chan |first3=Johnny C. L. |last4=Emanuel |first4=Kerry |last5=Ho |first5=Chang-Hoi |last6=Kossin |first6=James |last7=Mohapatra |first7=Mrutyunjay |last8=Satoh |first8=Masaki |last9=Sugi |first9=Masato |last10=Walsh |first10=Kevin |last11=Wu |first11=Liguang |date=August 6, 2019 |title=Tropical Cyclones and Climate Change Assessment: Part II. Projected Response to Anthropogenic Warming |journal=Bulletin of the American Meteorological Society |language=en |volume=101 |issue=3 |pages=BAMS–D–18–0194.1 |doi=10.1175/BAMS-D-18-0194.1 |issn=0003-0007 |doi-access=free}}</ref> Tropical cyclones use warm, moist air as their source of energy or "fuel". As climate change is [[Ocean heat content|warming ocean temperatures]], there is potentially more of this fuel available.<ref>{{Cite web |date=May 18, 2020 |title=Major tropical cyclones have become '15% more likely' over past 40 years |url=https://www.carbonbrief.org/major-tropical-cyclones-have-become-15-more-likely-over-past-40-years |url-status=live |archive-url=https://web.archive.org/web/20200808212654/https://www.carbonbrief.org/major-tropical-cyclones-have-become-15-more-likely-over-past-40-years |archive-date=August 8, 2020 |access-date=August 31, 2020 |website=Carbon Brief |language=en}}</ref> Between 1979 and 2017, there was a global increase in the proportion of tropical cyclones of Category 3 and higher on the [[Saffir–Simpson scale]]. The trend was most clear in the North Atlantic and in the Southern Indian Ocean. In the North Pacific, tropical cyclones have been moving poleward into colder waters and there was no increase in intensity over this period.<ref>{{Cite journal |last1=Kossin |first1=James P. |last2=Knapp |first2=Kenneth R. |last3=Olander |first3=Timothy L. |last4=Velden |first4=Christopher S. |date=May 18, 2020 |title=Global increase in major tropical cyclone exceedance probability over the past four decades |url=https://www.pnas.org/content/pnas/117/22/11975.full.pdf |url-status=live |journal=Proceedings of the National Academy of Sciences |language=en |volume=117 |issue=22 |pages=11975–11980 |bibcode=2020PNAS..11711975K |doi=10.1073/pnas.1920849117 |issn=0027-8424 |pmc=7275711 |pmid=32424081 |archive-url=https://web.archive.org/web/20201119095015/https://www.pnas.org/content/pnas/117/22/11975.full.pdf |archive-date=November 19, 2020 |access-date=October 6, 2020 |doi-access=free}}</ref> With {{Convert|2|C-change|F-change}} warming, a greater percentage (+13%) of tropical cyclones are expected to reach Category 4 and 5 strength.<ref name=":52" /> A 2019 study indicates that climate change has been driving the observed trend of [[rapid intensification]] of tropical cyclones in the Atlantic basin. Rapidly intensifying cyclones are hard to forecast and therefore pose additional risk to coastal communities.<ref>{{Cite book |last1=Collins |first1=M. |title=IPCC Special Report on the Ocean and Cryosphere in a Changing Climate |last2=Sutherland |first2=M. |last3=Bouwer |first3=L. |last4=Cheong |first4=S.-M. |last5=Frölicher |first5=T. |last6=Jacot Des Combes |first6=H. |last7=Koll Roxy |first7=M. |last8=Losada |first8=I. J. |last9=McInnes |first9=K. |year=2019 |pages=602 |chapter=Chapter 6: Extremes, Abrupt Changes and Managing Risks <!-- ipcc:20200202 --> |display-authors=4 |access-date=October 6, 2020 |chapter-url=https://www.ipcc.ch/site/assets/uploads/sites/3/2019/11/10_SROCC_Ch06_FINAL.pdf |archive-url=https://web.archive.org/web/20191220151131/https://www.ipcc.ch/site/assets/uploads/sites/3/2019/11/10_SROCC_Ch06_FINAL.pdf |archive-date=December 20, 2019 |url-status=live |last12=Susanto |last10=Ratter |last11=Rivera-Arriaga |first12=R. D. |last14=Tibig |first11=E. |last13=Swingedouw |first14=L. |first13=D. |first10=B.}}</ref>
+[[Climate change]] can affect [[Tropical cyclone|tropical cyclones]] in a variety of ways: an intensification of rainfall and wind speed, a decrease in overall frequency, an increase in the frequency of very intense storms and a poleward extension of where the cyclones reach maximum [[Intensity mapping|intensity]] are among the possible consequences of human-induced climate change.<ref name=":52">{{Cite journal |last1=Knutson |first1=Thomas |last2=Camargo |first2=Suzana J. |last3=Chan |first3=Johnny C. L. |last4=Emanuel |first4=Kerry |last5=Ho |first5=Chang-Hoi |last6=Kossin |first6=James |last7=Mohapatra |first7=Mrutyunjay |last8=Satoh |first8=Masaki |last9=Sugi |first9=Masato |last10=Walsh |first10=Kevin |last11=Wu |first11=Liguang |date=August 6, 2019 |title=Tropical Cyclones and Climate Change Assessment: Part II. Projected Response to Anthropogenic Warming |journal=Bulletin of the American Meteorological Society |language=en |volume=101 |issue=3 |pages=BAMS–D–18–0194.1 |doi=10.1175/BAMS-D-18-0194.1 |issn=0003-0007 |doi-access=free}}</ref> Tropical cyclones use warm, moist air as their source of energy or "fuel". As climate change is [[Ocean heat content|warming ocean temperatures]], there is potentially more of this fuel available.<ref>{{Cite web |date=May 18, 2020 |title=Major tropical cyclones have become '15% more likely' over past 40 years |url=https://www.carbonbrief.org/major-tropical-cyclones-have-become-15-more-likely-over-past-40-years |url-status=live |archive-url=https://web.archive.org/web/20200808212654/https://www.carbonbrief.org/major-tropical-cyclones-have-become-15-more-likely-over-past-40-years |archive-date=August 8, 2020 |access-date=August 31, 2020 |website=Carbon Brief |language=en}}</ref> Between 1979 and 2017, there was a global increase in the proportion of tropical cyclones of Category 3 and higher on the [[Saffir–Simpson scale]]. The trend was most clear in the [[North Atlantic]] and in the [[Southern Indian Ocean Islands tundra|Southern Indian Ocean.]] In the [[North Pacific]], tropical cyclones have been moving poleward into colder waters and there was no increase in intensity over this period.<ref>{{Cite journal |last1=Kossin |first1=James P. |last2=Knapp |first2=Kenneth R. |last3=Olander |first3=Timothy L. |last4=Velden |first4=Christopher S. |date=May 18, 2020 |title=Global increase in major tropical cyclone exceedance probability over the past four decades |url=https://www.pnas.org/content/pnas/117/22/11975.full.pdf |url-status=live |journal=Proceedings of the National Academy of Sciences |language=en |volume=117 |issue=22 |pages=11975–11980 |bibcode=2020PNAS..11711975K |doi=10.1073/pnas.1920849117 |issn=0027-8424 |pmc=7275711 |pmid=32424081 |archive-url=https://web.archive.org/web/20201119095015/https://www.pnas.org/content/pnas/117/22/11975.full.pdf |archive-date=November 19, 2020 |access-date=October 6, 2020 |doi-access=free}}</ref> With {{Convert|2|C-change|F-change}} warming, a greater percentage (+13%) of tropical cyclones are expected to reach Category 4 and 5 strength.<ref name=":52" /> A 2019 study indicates that climate change has been driving the observed trend of [[rapid intensification]] of tropical cyclones in the Atlantic basin. Rapidly intensifying cyclones are hard to forecast and therefore pose additional risk to coastal communities.<ref>{{Cite book |last1=Collins |first1=M. |title=IPCC Special Report on the Ocean and Cryosphere in a Changing Climate |last2=Sutherland |first2=M. |last3=Bouwer |first3=L. |last4=Cheong |first4=S.-M. |last5=Frölicher |first5=T. |last6=Jacot Des Combes |first6=H. |last7=Koll Roxy |first7=M. |last8=Losada |first8=I. J. |last9=McInnes |first9=K. |year=2019 |pages=602 |chapter=Chapter 6: Extremes, Abrupt Changes and Managing Risks <!-- ipcc:20200202 --> |display-authors=4 |access-date=October 6, 2020 |chapter-url=https://www.ipcc.ch/site/assets/uploads/sites/3/2019/11/10_SROCC_Ch06_FINAL.pdf |archive-url=https://web.archive.org/web/20191220151131/https://www.ipcc.ch/site/assets/uploads/sites/3/2019/11/10_SROCC_Ch06_FINAL.pdf |archive-date=December 20, 2019 |url-status=live |last12=Susanto |last10=Ratter |last11=Rivera-Arriaga |first12=R. D. |last14=Tibig |first11=E. |last13=Swingedouw |first14=L. |first13=D. |first10=B.}}</ref>
 Warmer air can hold more water vapor: the theoretical maximum water vapor content is given by the [[Clausius–Clapeyron relation]], which yields ≈7% increase in water vapor in the atmosphere per {{Convert|1|C-change|F-change}} warming.<ref>{{cite journal |author1=Thomas R. Knutson |author2=Joseph J. Sirutis |author3=Ming Zhao |year=2015 |title=Global Projections of Intense Tropical Cyclone Activity for the Late Twenty-First Century from Dynamical Downscaling of CMIP5/RCP4.5 Scenarios |url=https://digitalcommons.odu.edu/cgi/viewcontent.cgi?article=1323&context=ccpo_pubs |url-status=live |journal=Journal of Climate |volume=28 |issue=18 |pages=7203–7224 |bibcode=2015JCli...28.7203K |doi=10.1175/JCLI-D-15-0129.1 |archive-url=https://web.archive.org/web/20200105210405/https://digitalcommons.odu.edu/cgi/viewcontent.cgi?article=1323&context=ccpo_pubs |archive-date=January 5, 2020 |access-date=October 6, 2020}}</ref><ref name="knutson 20132">{{cite journal |author=Knutson |display-authors=et al |year=2013 |title=Dynamical Downscaling Projections of Late 21st Century Atlantic Hurricane Activity: CMIP3 and CMIP5 Model-based Scenarios |url=https://www.gfdl.noaa.gov/research_highlight/dynamical-downscaling-projections-of-late-21st-century-atlantic-hurricane-activity-cmip3-and-cmip5-model-based-scenarios/ |url-status=live |journal=Journal of Climate |volume=26 |issue=17 |pages=6591–6617 |bibcode=2013JCli...26.6591K |doi=10.1175/JCLI-D-12-00539.1 |archive-url=https://web.archive.org/web/20201005005313/https://www.gfdl.noaa.gov/research_highlight/dynamical-downscaling-projections-of-late-21st-century-atlantic-hurricane-activity-cmip3-and-cmip5-model-based-scenarios/ |archive-date=October 5, 2020 |access-date=October 6, 2020 |s2cid=129571840}}</ref> All models that were assessed in a 2019 review paper show a future increase of rainfall rates.<ref name=":52" /> Additional [[sea level rise]] will increase storm surge levels.<ref name=":62">{{Cite book |last1=Collins |first1=M. |title=IPCC Special Report on the Ocean and Cryosphere in a Changing Climate |last2=Sutherland |first2=M. |last3=Bouwer |first3=L. |last4=Cheong |first4=S.-M. |last5=Frölicher |first5=T. |last6=Jacot Des Combes |first6=H. |last7=Koll Roxy |first7=M. |last8=Losada |first8=I. J. |last9=McInnes |first9=K. |year=2019 |pages=603 |chapter=Chapter 6: Extremes, Abrupt Changes and Managing Risks |ref={{harvid|IPCC SROCC Ch6|2019}} <!-- ipcc:20200202 --> |display-authors=4 |access-date=October 6, 2020 |chapter-url=https://www.ipcc.ch/site/assets/uploads/sites/3/2019/11/10_SROCC_Ch06_FINAL.pdf |archive-url=https://web.archive.org/web/20191220151131/https://www.ipcc.ch/site/assets/uploads/sites/3/2019/11/10_SROCC_Ch06_FINAL.pdf |archive-date=December 20, 2019 |url-status=live |last12=Susanto |last10=Ratter |last11=Rivera-Arriaga |first12=R. D. |last14=Tibig |first11=E. |last13=Swingedouw |first14=L. |first13=D. |first10=B.}}</ref><ref name=":42">{{cite news |date=August 29, 2017 |title=Hurricane Harvey shows how we underestimate flooding risks in coastal cities, scientists say |newspaper=The Washington Post |url=https://www.washingtonpost.com/news/energy-environment/wp/2017/08/29/hurricane-harvey-shows-how-we-underestimate-flooding-risks-in-coastal-cities-scientists-say |url-status=live |access-date=August 30, 2017 |archive-url=https://web.archive.org/web/20170830031541/https://www.washingtonpost.com/news/energy-environment/wp/2017/08/29/hurricane-harvey-shows-how-we-underestimate-flooding-risks-in-coastal-cities-scientists-say/ |archive-date=August 30, 2017}}</ref> It is plausible that extreme [[Wind wave|wind waves]] see an increase as a consequence of changes in tropical cyclones, further exacerbating storm surge dangers to coastal communities.<ref name=":72">{{Cite journal |last1=Walsh |first1=K. J. E. |last2=Camargo |first2=S. J. |last3=Knutson |first3=T. R. |last4=Kossin |first4=J. |last5=Lee |first5=T. -C. |last6=Murakami |first6=H. |last7=Patricola |first7=C. |date=December 1, 2019 |title=Tropical cyclones and climate change |journal=Tropical Cyclone Research and Review |language=en |volume=8 |issue=4 |pages=240–250 |doi=10.1016/j.tcrr.2020.01.004 |issn=2225-6032 |doi-access=free}}</ref> The compounding effects from floods, storm surge, and terrestrial flooding (rivers) are projected to increase [[Effects of global warming|due to global warming]].<ref name=":42" />
-There is currently no consensus on how climate change will affect the overall frequency of tropical cyclones.<ref name=":52" /> A majority of [[Climate model|climate models]] show a decreased frequency in future projections.<ref name=":72" /> For instance, a 2020 paper comparing nine high-resolution climate models found robust decreases in frequency in the Southern Indian Ocean and the Southern Hemisphere more generally, while finding mixed signals for Northern Hemisphere tropical cyclones.<ref>{{Cite journal |last1=Roberts |first1=Malcolm John |last2=Camp |first2=Joanne |last3=Seddon |first3=Jon |last4=Vidale |first4=Pier Luigi |last5=Hodges |first5=Kevin |last6=Vannière |first6=Benoît |last7=Mecking |first7=Jenny |last8=Haarsma |first8=Rein |last9=Bellucci |first9=Alessio |last10=Scoccimarro |first10=Enrico |last11=Caron |first11=Louis-Philippe |year=2020 |title=Projected Future Changes in Tropical Cyclones Using the CMIP6 HighResMIP Multimodel Ensemble |journal=Geophysical Research Letters |language=en |volume=47 |issue=14 |pages=e2020GL088662 |bibcode=2020GeoRL..4788662R |doi=10.1029/2020GL088662 |issn=1944-8007 |pmc=7507130 |pmid=32999514 |s2cid=221972087}}</ref> Observations have shown little change in the overall frequency of tropical cyclones worldwide,<ref>{{Cite web |title=Hurricanes and Climate Change |url=https://www.ucsusa.org/global-warming/science-and-impacts/impacts/hurricanes-and-climate-change.html |url-status=live |archive-url=https://web.archive.org/web/20190924043720/https://www.ucsusa.org/global-warming/science-and-impacts/impacts/hurricanes-and-climate-change.html |archive-date=September 24, 2019 |access-date=September 29, 2019 |website=Union of Concerned Scientists |language=en}}</ref> with increased frequency in the North Atlantic and central Pacific, and significant decreases in the southern Indian Ocean and western North Pacific.<ref>{{Cite journal |last1=Murakami |first1=Hiroyuki |last2=Delworth |first2=Thomas L. |last3=Cooke |first3=William F. |last4=Zhao |first4=Ming |last5=Xiang |first5=Baoqiang |last6=Hsu |first6=Pang-Chi |year=2020 |title=Detected climatic change in global distribution of tropical cyclones |journal=Proceedings of the National Academy of Sciences |language=en |volume=117 |issue=20 |pages=10706–10714 |bibcode=2020PNAS..11710706M |doi=10.1073/pnas.1922500117 |issn=0027-8424 |pmc=7245084 |pmid=32366651 |doi-access=free}}</ref> There has been a poleward expansion of the latitude at which the maximum intensity of tropical cyclones occurs, which may be associated with climate change.<ref>{{cite journal |author1=James P. Kossin |author2=Kerry A. Emanuel |author3=Gabriel A. Vecchi |year=2014 |title=The poleward migration of the location of tropical cyclone maximum intensity |journal=Nature |volume=509 |issue=7500 |pages=349–352 |bibcode=2014Natur.509..349K |doi=10.1038/nature13278 |pmid=24828193 |hdl-access=free |hdl=1721.1/91576 |s2cid=4463311}}</ref> In the North Pacific, there may also have been an eastward expansion.<ref name=":62" /> Between 1949 and 2016, there was a slowdown in tropical cyclone translation speeds. It is unclear still to what extent this can be attributed to climate change: climate models do not all show this feature.<ref name=":72" />
+There is currently no consensus on how climate change will affect the overall frequency of tropical cyclones.<ref name=":52" /> A majority of [[Climate model|climate models]] show a decreased frequency in future projections.<ref name=":72" /> For instance, a 2020 paper comparing nine high-resolution climate models found robust decreases in frequency in the Southern Indian Ocean and the Southern [[Hemispheres (Rush album)|Hemisphere]] more generally, while finding mixed signals for Northern Hemisphere tropical cyclones.<ref>{{Cite journal |last1=Roberts |first1=Malcolm John |last2=Camp |first2=Joanne |last3=Seddon |first3=Jon |last4=Vidale |first4=Pier Luigi |last5=Hodges |first5=Kevin |last6=Vannière |first6=Benoît |last7=Mecking |first7=Jenny |last8=Haarsma |first8=Rein |last9=Bellucci |first9=Alessio |last10=Scoccimarro |first10=Enrico |last11=Caron |first11=Louis-Philippe |year=2020 |title=Projected Future Changes in Tropical Cyclones Using the CMIP6 HighResMIP Multimodel Ensemble |journal=Geophysical Research Letters |language=en |volume=47 |issue=14 |pages=e2020GL088662 |bibcode=2020GeoRL..4788662R |doi=10.1029/2020GL088662 |issn=1944-8007 |pmc=7507130 |pmid=32999514 |s2cid=221972087}}</ref> Observations have shown little change in the overall frequency of tropical cyclones worldwide,<ref>{{Cite web |title=Hurricanes and Climate Change |url=https://www.ucsusa.org/global-warming/science-and-impacts/impacts/hurricanes-and-climate-change.html |url-status=live |archive-url=https://web.archive.org/web/20190924043720/https://www.ucsusa.org/global-warming/science-and-impacts/impacts/hurricanes-and-climate-change.html |archive-date=September 24, 2019 |access-date=September 29, 2019 |website=Union of Concerned Scientists |language=en}}</ref> with increased frequency in the North Atlantic and central Pacific, and significant decreases in the southern Indian Ocean and western North Pacific.<ref>{{Cite journal |last1=Murakami |first1=Hiroyuki |last2=Delworth |first2=Thomas L. |last3=Cooke |first3=William F. |last4=Zhao |first4=Ming |last5=Xiang |first5=Baoqiang |last6=Hsu |first6=Pang-Chi |year=2020 |title=Detected climatic change in global distribution of tropical cyclones |journal=Proceedings of the National Academy of Sciences |language=en |volume=117 |issue=20 |pages=10706–10714 |bibcode=2020PNAS..11710706M |doi=10.1073/pnas.1922500117 |issn=0027-8424 |pmc=7245084 |pmid=32366651 |doi-access=free}}</ref> There has been a poleward expansion of the latitude at which the maximum intensity of tropical cyclones occurs, which may be associated with climate change.<ref>{{cite journal |author1=James P. Kossin |author2=Kerry A. Emanuel |author3=Gabriel A. Vecchi |year=2014 |title=The poleward migration of the location of tropical cyclone maximum intensity |journal=Nature |volume=509 |issue=7500 |pages=349–352 |bibcode=2014Natur.509..349K |doi=10.1038/nature13278 |pmid=24828193 |hdl-access=free |hdl=1721.1/91576 |s2cid=4463311}}</ref> In the North Pacific, there may also have been an eastward expansion.<ref name=":62" /> Between 1949 and 2016, there was a slowdown in tropical cyclone translation speeds. It is unclear still to what extent this can be attributed to climate change: climate models do not all show this feature.<ref name=":72" />
 == Background ==