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Climate change caused by greenhouse gas emissions from human activities occurs everywhere on Earth, and while Antarctica is less vulnerable to it than any other continent, climate change in Antarctica has been observed. Since 1959, there has been an average temperature increase of >0.05 °C/decade since 1957 across the continent, although it had been uneven. West Antarctica warmed by over 0.1 °C/decade from the 1950s to the 2000s, and the exposed Antarctic Peninsula has warmed by 3 °C (5.4 °F) since the mid-20th century. The colder, stabler East Antarctica had been experiencing cooling until the 2000s. Around Antarctica, the Southern Ocean has absorbed more oceanic heat than any other ocean, and has seen strong warming at depths below 2,000 m (6,600 ft). Around the West Antarctic, the ocean has warmed by 1 °C (1.8 °F) since 1955.

The warming of the Southern Ocean around Antarctica has caused the weakening or collapse of ice shelves, which float just offshore of glaciers and stabilize them. Many coastal glaciers have been losing mass and retreating, causing net-annual ice loss across Antarctica, although the East Antarctic ice sheet continues to gain ice inland. By 2100, net ice loss from Antarctica is expected to add about 11 cm (5 in) to global sea level rise. Marine ice sheet instability may cause West Antarctica to contribute tens of centimeters more if it is triggered before 2100. With higher warming, instability would be much more likely, and could double global, 21st-century sea-level rise.

The fresh, 1100-1500 billion tons (GT) per year of meltwater from the ice dilutes the saline Antarctic bottom water, weakening the lower cell of the Southern Ocean overturning circulation (SOOC). According to some research, a full collapse of the SOOC may occur a between 1.7 °C (3.1 °F) and 3 °C (5.4 °F) of global warming, although the full effects are expected to occur over multiple centuries; these include less precipitation in the Southern Hemisphere but more in the Northern Hemisphere, an eventual decline of fisheries in the Southern Ocean and a potential collapse of certain marine ecosystems. While many Antarctic species remain undiscovered, there are documented increases in Antarctic flora, and large fauna such as penguins are already having difficulty retaining suitable habitat. On ice-free land, permafrost thaws release greenhouse gases and formerly frozen pollution.

The West Antarctic ice sheet is likely to completely melt unless temperatures are reduced by 2 °C (3.6 °F) below 2020 levels. The loss of this ice sheet would take between 2,000 and 13,000 years, although several centuries of high greenhouse emissions could shorten this time to 500 years. A sea-level rise of 3.3 m (10 ft 10 in) would occur if the ice sheet collapses, leaving ice caps on the mountains, and 4.3 m (14 ft 1 in) if those ice caps also melt. Isostatic rebound may contribute an additional 1 m (3 ft 3 in) to global sea levels over another 1,000 years. The far-stabler East Antarctic ice sheet may only cause a sea-level rise of 0.5 m (1 ft 8 in) – 0.9 m (2 ft 11 in) from the current level of warming, a small fraction of the 53.3 m (175 ft) contained in the full ice sheet. With global warming of around 3 °C (5.4 °F), vulnerable areas like Wilkes Basin and Aurora Basin may collapse over around 2,000 years, potentially adding up to 6.4 m (21 ft 0 in) to sea levels. The complete melting and disappearance of the East Antarctic ice sheet would require at least 10,000 years and would only occur if global warming reaches 5 °C (9.0 °F) to 10 °C (18 °F).

Temperature and weather changes

Antarctica is the coldest, driest continent on Earth, and has the highest average elevation. Antarctica's dryness means the air contains little water vapor and conducts heat poorly. The Southern Ocean surrounding the continent is far more effective at absorbing heat than any other ocean. The presence of extensive, year-around sea ice, which has a high albedo (reflectivity), adds to the albedo of the ice sheets' own bright, white surface. Antarctica's coldness means it is the only place on Earth where an atmospheric temperature inversion occurs every winter; elsewhere on Earth, the atmosphere is at its warmest near the surface and becomes cooler as elevation increases. During the Antarctic winter, the surface of central Antarctica becomes cooler than middle layers of the atmosphere; this means greenhouse gases trap heat in the middle atmosphere, and reduce its flow toward the surface and toward space, rather than preventing the flow of heat from the lower atmosphere to the upper layers. This effect lasts until the end of the Antarctic winter. Early climate models predicted temperature trends over Antarctica would emerge more slowly and be more subtle than those elsewhere.

There were fewer than twenty permanent weather stations across the continent and only two in the continent's interior. Automatic weather stations were deployed relatively late, and their observational record was brief for much of the 20th century satellite temperature measurements began in 1981 and are typically limited to cloud-free conditions. Thus, datasets representing the entire continent only began to appear by the very end of the 20th century. The exception was the Antarctic Peninsula, where warming was pronounced and well-documented; it was eventually found to have warmed by 3 °C (5.4 °F) since the mid 20th century. Based on this limited data, several papers published in the early 2000s said there had been an overall cooling over continental Antarctica outside the Peninsula.

A 2002 analysis led by Peter Doran received widespread media coverage after it also indicated stronger cooling than warming between 1966 and 2000, and found the McMurdo Dry Valleys in East Antarctica had experienced cooling of 0.7 °C per decade, a local trend that was confirmed by subsequent research at McMurdo. Multiple journalists said these findings were "contradictory" to global warming, even though the paper noted the limited data and found warming over 42% of the continent. What became known as the Antarctic Cooling Controversy received further attention in 2004, when Michael Crichton wrote that novel State of Fear, which said a conspiracy among climate scientists to make up global warming, and said Doran's study definitively proved there was no warming in Antarctica outside of the Peninsula. Relatively few scientists responded to the book at the time, but it was mentioned in a 2006 US Senate hearing in support of climate change denial. Peter Doran published a statement in The New York Times decrying the misinterpretation of his work. The British Antarctic Survey and NASA also issued statements affirming the strength of climate science after the hearing.

By 2009, researchers were able to combine historical weather-station data with satellite measurements to create consistent temperature records going back to 1957 that demonstrated warming of >0.05 °C/decade since 1957 across the continent, with cooling in East Antarctica offset by the average temperature increase of at least 0.176 ± 0.06 °C per decade in West Antarctica. Subsequent research confirmed clear warming over West Antarctica in the 20th century, with the only uncertainty being the magnitude. During 2012-2013, estimates based on WAIS Divide ice cores and revised temperature records from Byrd Station suggested a much-larger West-Antarctica warming of 2.4 °C (4.3 °F) since 1958, or around 0.46 °C (0.83 °F) per decade, although there has been uncertainty about it. In 2022, a study narrowed the warming of the Central area of the West Antarctic Ice Sheet between 1959 and 2000 to 0.31 °C (0.56 °F) per decade, and conclusively attributed it to increases in greenhouse gas concentrations caused by human activity.

Between 2000 and 2020, local changes in atmospheric circulation patterns like the Interdecadal Pacific Oscillation (IPO) and the Southern Annular Mode (SAM) slowed or partially reversed the warming of West Antarctica , with the Antarctic Peninsula experiencing cooling from 2002.

While a variability in those patterns is natural, ozone depletion had also led the SAM to be stronger than it had been in the past 600 years of observations. Studies predicted a reversal in the SAM once the ozone layer began to recover following the Montreal Protocol, starting from 2002, and these changes are consistent with their predictions. As these patterns reversed, the East Antarctica interior demonstrated clear warming over those two decades. In particular, the South Pole warmed by 0.61 ± 0.34 °C per decade between 1990 and 2020, which is three times the global average. The Antarctica-wide warming trend continued after 2000, and in February 2020, the continent recorded its highest temperature of 18.3 °C, which is one degree higher than the previous record of 17.5 °C in March 2015.

Models predict under the most intense climate change scenario, known as RCP8.5, Antarctic temperatures will rise by 4 °C (7.2 °F) on average by 2100; this rise will be accompanied by a 30% increase in precipitation and a 30% decrease in sea ice. RCPs were developed in the late 2000s, and early 2020s research considers RCP8.5 much less likely than the more-moderate scenarios like RCP 4.5, which lie in between the worst-case scenario and the Paris Agreement goals.

Effects on ocean currents

Between 1971 and 2018, over 90% of thermal energy from global heating entered the oceans. The Southern Ocean absorbs the most heat; after 2005, it accounted for between 67% and 98% of all heat entering the oceans. The temperature in the ocean's upper layer in West Antarctica has warmed by 1 °C (1.8 °F) since 1955, and the Antarctic Circumpolar Current (ACC) is also warming faster than the average. It is also a highly important carbon sink. These properties are connected to the Southern Ocean overturning circulation (SOOC), one half of the global thermohaline circulation. It is important estimates on when global warming will reach 2 °C (3.6 °F) – inevitable in all scenarios where greenhouse gas emissions have not been significantly lowered – depend on the strength of the circulation more than any factor other than the overall emissions.

The overturning circulation has two parts; the smaller upper cell, which is most-strongly affected by winds and precipitation, and the larger lower cell that is defined by the temperature and salinity of Antarctic bottom water. Since the 1970s, the upper cell has strengthened by 50-60% while the lower cell has weakened by 10-20%. Some of this was due to the natural cycle of Interdecadal Pacific Oscillation (IPO) but there is a clear effect of climate change, because it alters winds and precipitation through shifts in the Southern Annular Mode (SAM) pattern. Fresh meltwater from the erosion of the West Antarctic ice sheet dilutes the more-saline Antarctic bottom water, which flows at a rate of 1100-1500 billion tons (GT) per year. During the 2010s, a temporary reduction in ice-shelf melting in West Antarctica allowed for the partial recovery of Antarctic bottom water and the lower cell of the circulation. Greater melting and further decline of the circulation is expected in the future.

As bottom water weakens while the flow of warmer, fresher waters strengthens near the surface, the surface waters become more buoyant, and less likely to sink and mix with the lower layers, increasing ocean stratification. One study says the strength of the circulation would halve by 2050 under the worst climate-change scenario, with greater losses occurring afterwards. Paleoclimate evidence shows the entire circulation has significantly weakened or completely collapsed in the past; preliminary research says such a collapse may become likely once global warming reaches between 1.7 °C (3.1 °F) and 3 °C (5.4 °F), but this estimate is much-less certain than for the majority of tipping points in the climate system. Such a collapse would be prolonged; one estimate says it would occur before 2300. As with the better-studied Atlantic meridional overturning circulation (AMOC), a major slowing or collapse of the SOOC would have substantial regional and global effects. Some likely effects include a decline in precipitation in Southern Hemisphere countries like Australia, a corresponding increase in precipitation in the Northern Hemisphere, and an eventual decline of fisheries in the Southern Ocean, which could lead to a potential collapse of some marine ecosystems. These effects are expected to occur over centuries, but there has been limited research to date and few specifics are currently known.

Effects on the cryosphere

Observed changes in ice mass

Contrasting temperature trends across parts of Antarctica mean some locations, particularly at the coasts, lose mass while locations further inland continue to gain mass. These contrasting trends and the remoteness of the region make estimating an average trend difficult. In 2018, a systematic review of all previous studies and data by the Ice Sheet Mass Balance Inter-comparison Exercise (IMBIE) estimated an increase in the West Antarctic ice sheet from 53 ± 29 Gt (gigatonnes) in 1992 to 159 ± 26 Gt in the final five years of the study. On the Antarctic Peninsula, the study estimated a loss of 20 ± 15 Gt per year with an increase in loss of roughly 15 Gt per year after 2000, a significant quantity of which was the loss of ice shelves. The review's overall estimate was that Antarctica lost 2,720 ± 1,390 gigatons of ice from 1992 to 2017, averaging 109 ± 56 Gt per year. This would amount to 7.6 mm (0.30 in) of sea-level rise. A 2021 analysis of data from four research satellite systems – Envisat, European Remote-Sensing Satellite, GRACE and GRACE-FO, and ICESat – indicated an annual mass loss of about 12 Gt from 2012 to 2016 due to much-greater ice gain in East Antarctica than earlier estimated, which offset most of the losses from West Antarctica. The East Antarctic ice sheet can still gain mass despite warming because effects of climate change on the water cycle increase precipitation over its surface, which then freezes and helps to accrete more ice.

Black carbon pollution

Black carbon from incomplete fuel combustion is carried long distances by wind. If it reaches Antarctica, black carbon accumulates on snow and ice, reducing the reflectivity and causing it to absorb more energy. This accelerates melting and can create an ice-albedo feedback loop in which meltwater itself absorbs more heat from sunlight. Due to its remoteness, Antarctica has the cleanest snow in the world, and some research says the effects of black carbon across West and East Antarctica is minimal with an albedo reduction of about 0.5% in one 47-year ice core.

The highest concentrations of black carbon are found on the Antarctic Peninsula, where human activity is higher than elsewhere. Black carbon deposits near common tourist sites and research stations increase summer seasonal melting by between about 5 to 23 kg (11 to 51 lb) of snow per m.

21st-century ice loss and sea-level rise

By 2100, net ice loss from Antarctica is expected to add about 11 cm (4.3 in) to global sea-level rise. Other processes may cause West Antarctica to contribute more to sea-level rise. Marine ice-sheet instability is the potential for warm water currents to enter between the seafloor and the base of the ice sheet once the sheet is no longer heavy enough to displace such flows. Marine ice-cliff instability may cause ice cliffs taller than 100 m (330 ft) to collapse under their own weight once they are no longer buttressed by ice shelves. This process has never been observed and it only occurs in some models. By 2100, these processes may increase sea-level rise caused by Antarctica to 41 cm (16 in) under the low-emission scenario and by 57 cm (22 in) under the high-emission scenario.

Some scientists have given greater estimates but all agree melting in Antarctica would have a greater impact and would be much more likely to occur under higher warming scenarios, where it may double the overall 21st-century sea-level rise to 2 m (7 ft) or more. According to one study, if the Paris Agreement is followed and global warming is limited to 2 °C (3.6 °F), the loss of ice in Antarctica will continue at the 2020 rate for the rest of the 21st century, but if a trajectory leading to 3 °C (5.4 °F) is followed, Antarctica ice loss will accelerate after 2060 and start adding 0.5 cm (0.20 in) per year to global sea levels by 2100.

Long-term sea level rise

Sea levels will continue to rise long after 2100 but potentially at very different rates. According to the most-recent reports of the Intergovernmental Panel on Climate Change (SROCC and the IPCC Sixth Assessment Report), there will be a median rise of 16 cm (6.3 in) and maximum rise of 37 cm (15 in) under the low-emission scenario. The highest-emission scenario results in a median rise of 1.46 m (5 ft) with a minimum of 60 cm (2 ft) and a maximum of 2.89 m (9+1⁄2 ft).

Over longer timescales, the West Antarctic ice sheet, which is much smaller than the East Antarctic ice sheet and is grounded deep below sea level, is considered highly vulnerable. The melting of all of the ice in West Antarctica would increase global sea-level rise to 4.3 m (14 ft 1 in). Mountain ice caps that are not in contact with water are less vulnerable than the majority of the ice sheet, which is located below sea level. The collapse of the West Antarctic ice sheet would cause around 3.3 m (10 ft 10 in) of sea-level rise. This kind of collapse is now considered almost inevitable because it appears to have occurred during the Eemian period 125,000 years ago, when temperatures were similar to those in the early 21st century. The Amundsen Sea also appears to be warming at rates that, if continued, make the ice sheet's collapse inevitable.

The only way to reverse ice loss from West Antarctica once triggered is to lower the global temperature to 1 °C (1.8 °F) below the pre-industrial level, to 2 °C (3.6 °F) below the temperature of 2020. Other researchers said a climate engineering intervention to stabilize the ice sheet's glaciers may delay its loss by centuries and give the environment more time to adapt. This is an uncertain proposal and would be one of the most-expensive projects ever attempted. Otherwise, the disappearance of the West Antarctic ice sheet would take an estimated 2,000 years. The loss of West Antarctica ice would take at least 500 years and possibly as long as 13,000 years. Once the ice sheet is lost, the isostatic rebound of the land previously covered by the ice sheet would result in an additional 1 m (3 ft 3 in) of sea-level rise over the following 1,000 years.

The East Antarctic ice sheet is far more stable than the West Antarctic ice sheet. The loss of the entire East Antarctic ice sheet would require global warming of between 5 °C (9.0 °F) and 10 °C (18 °F), and a minimum of 10,000 years. Some of its parts, such as Totten Glacier and Wilkes Basin, are in vulnerable subglacial basins that lie below sea level. Estimates suggest the irreversible loss of those basins would begin once global warming reaches 3 °C (5.4 °F), although this loss may become irreversible at warming of between 2 °C (3.6 °F) and 6 °C (11 °F). After global warming reaches the critical threshold for the collapse of these subglacial basins, their loss will likely occur over around 2,000 years, although the loss may be as fast as 500 years or as slow as 10,000 years.

The loss of all of this ice would add between 1.4 m (4 ft 7 in) and 6.4 m (21 ft 0 in) to sea levels, depending on the ice sheet model used. Isostatic rebound of the newly ice-free land would add between 8 cm (3.1 in) and 57 cm (1 ft 10 in). Evidence from the Pleistocene shows partial loss can occur at lower warming levels; Wilkes Basin is estimated to have lost enough ice to add 0.5 m (1 ft 8 in) to sea levels between 115,000 and 129,000 years ago during the Eemian, and about 0.9 m (2 ft 11 in) between 318,000 and 339,000 years ago during Marine Isotope Stage 9.

Permafrost thaw

Antarctica has much less permafrost than the Arctic. Antarctic permafrost is subject to thaw. The permafrost in Antarctica traps various compounds, including persistent organic pollutants (POPs) like polycyclic aromatic hydrocarbons, many of which are known carcinogens or can cause liver damage; and polychlorinated biphenyls such as hexachlorobenzene (HCB) and DDT, which are associated with decreased reproductive success and immunohematological disorders. Antarctic soils also contain heavy metals, including mercury, lead and cadmium, all of which can cause endocrine disruption, DNA damage, immunotoxicity and reproductive toxicity. These compounds are released when contaminated permafrost thaws; this can change the chemistry of surface water. Bioaccumulation and biomagnification spread these compounds throughout the food web. Permafrost thaw also results in greenhouse gas emissions, though the limited volume of Antarctic permafrost relative to Arctic permafrost means Antarctic permafrost is not considered a significant cause of climate change.

Ecological effects

Marine ecosystems

Nearly all of the species in Antarctic are marine; by 2015, 8,354 species had been discovered in Antarctica and taxonomically accepted; of these species, only 57 were not marine. Antarctica may have up to 17,000 species; while 90% of the ocean around Antarctica is deeper than 1,000 m (3,281 ft), only 30% of the benthic-sample locations were taken at that depth. On the Antarctic continental shelves, bethnic-zone biomass may increase due to oceanic warming, which is likely to be of most benefit to seaweed. Around 12% of the native benthic species may be outcompeted and go extinct. These estimates are preliminary; the vulnerabilities of most Antarctic species have yet to be assessed.

Unlike the Arctic, there has been little change in marine primary production across the Southern Ocean in the available observations. Estimates say an increase in Southern Ocean primary production could occur after 2100; this increase would block many nutrients from travelling to other oceans, leading to decreased production elsewhere. Some microbial communities appear to have been negatively affected by ocean acidification and there is a risk future acidification would threaten the eggs of pteropods, a type of zooplankton.

Antarctic krill are a key species in the Antarctic food web; they feed on phytoplankton, and are the main food for fish and penguins. Krill are likely to abandon the fastest-warming areas, such as the Weddell Sea, while icefish may find shelf waters around Antarctic islands unsuitable. The shifts or declines in krill and copepod numbers are known to prevent the recovery in numbers of baleen whale following the declines caused by historical whaling. Without a reversal in temperature increases, baleen whales are likely to be forced to adapt their migratory patterns or face local extinction. Many other marine species are expected to move into Antarctic waters as the oceans continue to warm, forcing native species to compete with them. Some research says at 3 °C (5.4 °F) of warming, the diversity of Antarctic species would decline by nearly 17% and the suitable climate area would shrink by 50%.

Penguins

Penguins are the highest species in the Antarctic food web and are already being substantially affected by climate change. Numbers of Adélie penguins, chinstrap penguins, emperor penguin and king penguins have already been declining, while the number of gentoo penguins has increased. Gentoo penguins, which are ice intolerant and use mosses as nesting material, have been able to spread into previously inaccessible territories and substantially increase in number. The vulnerable penguin species can respond through acclimatization, adaptation, or range shift. Range shift through dispersal leads to colonization elsewhere but results in local extinction.

Climate change is particularly threatening to penguins. As early as 2008, it was estimated every Southern Ocean temperature increase of 0.26 °C (0.47 °F) reduces king penguin populations by nine percent. Under the worst-case warming scenario, king penguins will permanently lose at least two of their current eight breeding sites, and 70% of the species (1.1 million pairs) will have to relocate to avoid extinction. Emperor penguin populations may be at a similar risk; with no climate mitigation, 80% of populations are at risk of extinction by 2100. With Paris-Agreement temperature goals in place, that number may fall to 31% under the 2 °C (3.6 °F) goal, and to 19% under the 1.5 °C (2.7 °F) goal.

A 27-year study of the largest colony of Magellanic penguins that was published in 2014 found extreme weather caused by climate change kills seven percent of penguin chicks in an average year, accounting for up to 50% of all chick deaths in some years. Since 1987, the number of breeding pairs in the colony has fallen by 24%. Chinstrap penguins are also in decline, mainly due to a corresponding decline of Antarctic krill. It is estimated while Adélie penguins will retain some habitat past 2099, one-third of colonies along the West Antarctic Peninsula – around 20% of the species – will be in decline by 2060.

Terrestrial ecosystems

On the Antarctic continent, plants are mainly found in coastal areas; the commonest plants are lichens, followed by mosses and ice algae. In the Antarctic Peninsula, green snow algae have a combined biomass of around 1,300 t (2,900,000 lb). As glaciers retreat, they expose areas that often become colonized by pioneer lichen species. The reduction in precipitation in East Antarctica had turned many green mosses from green to red or brown as they respond to this drought. Schistidium antarctici had declined, while the desiccation-tolerant species Bryum pseudotriquetrum and Ceratodon purpureus have increased. The Antarctic ozone hole has led to an increase in UV-B radiation, which also causes observed damage to plant cells and photosynthesis.

The only vascular plants on continental Antarctica are Deschampsia antarctica and Colobanthus quitensis, which are found on the Antarctic Peninsula. Increased temperatures have boosted photosynthesis and allowed these species to increase their population and range. Other plant species are increasingly likely to spread to Antarctica as the climate continues to warm and as human activity on the continent increases.

Effects of human development

Tourism in Antarctica has significantly increased since 2020; 74,400 tourists arrived there in late 2019 and early 2020. The development of Antarctica for the purposes of industry, tourism, and an increase in research facilities may put pressure on the continent and threaten its status as largely untouched land. Regulated tourism in Antarctica brings about awareness, and encourages the investment and public support needed to preserve Antarctica's distinctive environment. An unmitigated loss of ice on land and sea could greatly reduce its attractiveness.

Policy can be used to increase climate-change resilience through the protection of ecosystems. Ships that operate in Antarctic waters adhere to the international Polar Code, which includes regulations and safety measures such as operational training and assessments, the control of oil discharge, appropriate sewage disposal, and the prevention of pollution by toxic liquids. Antarctic Specially Protected Areas (ASPA) and Antarctic Specially Managed Areas (ASMA) are designated by the Antarctic Treaty to protect flora and fauna. Both ASPAs and ASMAs restrict entry but to different extents, with ASPAs being the highest level of protection. Designation of ASPAs has decreased 84% since the 1980s despite a rapid increase in tourism, which may bring additional stressors to the natural environment and ecosystems. To alleviate stress on Antarctic ecosystems posed by climate change and the rapid increase in tourism, much of the scientific community advocates for an increase in protected areas like ASPAs to improve Antarctica's resilience to rising temperatures.

See also

• 2024 Antarctica heat wave
• ANDEEP
• Climate of Antarctica
• Climate change in the Arctic
• Register of Antarctic Marine Species

References

1. ^ Singh, Hansi A.; Polvani, Lorenzo M. (10 January 2020). "Low Antarctic continental climate sensitivity due to high ice sheet orography". npj Climate and Atmospheric Science. 3 (1): 39. Bibcode:2020npCAS...3...39S. doi:10.1038/s41612-020-00143-w. S2CID 222179485.
2. ^ Steig, Eric; Schneider, David; Rutherford, Scott; Mann, Michael E.; Comiso, Josefino; Shindell, Drew (1 January 2009). "Warming of the Antarctic ice-sheet surface since the 1957 International Geophysical Year". Arts & Sciences Faculty Publications.
3. ^ "Impacts of climate change". Discovering Antarctica. Retrieved 15 May 2022.
4. ^ Clem, Kyle R.; Fogt, Ryan L.; Turner, John; Lintner, Benjamin R.; Marshall, Gareth J.; Miller, James R.; Renwick, James A. (August 2020). "Record warming at the South Pole during the past three decades". Nature Climate Change. 10 (8): 762–770. Bibcode:2020NatCC..10..762C. doi:10.1038/s41558-020-0815-z. ISSN 1758-6798. S2CID 220261150.
5. ^ Xin, Meijiao; Clem, Kyle R; Turner, John; Stammerjohn, Sharon E; Zhu, Jiang; Cai, Wenju; Li, Xichen (2 June 2023). "West-warming East-cooling trend over Antarctica reversed since early 21st century driven by large-scale circulation variation". Environmental Research Letters. 18 (6): 064034. doi:10.1088/1748-9326/acd8d4.
6. ^ Bourgeois, Timothée; Goris, Nadine; Schwinger, Jörg; Tjiputra, Jerry F. (17 January 2022). "Stratification constrains future heat and carbon uptake in the Southern Ocean between 30°S and 55°S". Nature Communications. 13 (1): 340. Bibcode:2022NatCo..13..340B. doi:10.1038/s41467-022-27979-5. PMC 8764023. PMID 35039511.
7. ^ Fox-Kemper, B.; Hewitt, H.T.; Xiao, C.; Aðalgeirsdóttir, G.; Drijfhout, S.S.; Edwards, T.L.; Golledge, N.R.; Hemer, M.; Kopp, R.E.; Krinner, G.; Mix, A. (2021). Masson-Delmotte, V.; Zhai, P.; Pirani, A.; Connors, S.L.; Péan, C.; Berger, S.; Caud, N.; Chen, Y.; Goldfarb, L. (eds.). "Chapter 9: Ocean, Cryosphere and Sea Level Change" (PDF). Climate Change 2021: The Physical Science Basis. Contribution of Working Group I to the Sixth Assessment Report of the Intergovernmental Panel on Climate Change. Cambridge University Press, Cambridge, UK and New York, NY, USA: 1270–1272.
8. ^ Nauels, Alexander; Rogelj, Joeri; Schleussner, Carl-Friedrich; Meinshausen, Malte; Mengel, Matthias (1 November 2017). "Linking sea level rise and socioeconomic indicators under the Shared Socioeconomic Pathways". Environmental Research Letters. 12 (11): 114002. Bibcode:2017ERL....12k4002N. doi:10.1088/1748-9326/aa92b6. hdl:20.500.11850/230713.
9. ^ L. Bamber, Jonathan; Oppenheimer, Michael; E. Kopp, Robert; P. Aspinall, Willy; M. Cooke, Roger (May 2019). "Ice sheet contributions to future sea-level rise from structured expert judgment". Proceedings of the National Academy of Sciences. 116 (23): 11195–11200. Bibcode:2019PNAS..11611195B. doi:10.1073/pnas.1817205116. PMC 6561295. PMID 31110015.
10. ^ Horton, Benjamin P.; Khan, Nicole S.; Cahill, Niamh; Lee, Janice S. H.; Shaw, Timothy A.; Garner, Andra J.; Kemp, Andrew C.; Engelhart, Simon E.; Rahmstorf, Stefan (8 May 2020). "Estimating global mean sea-level rise and its uncertainties by 2100 and 2300 from an expert survey". npj Climate and Atmospheric Science. 3 (1): 18. Bibcode:2020npCAS...3...18H. doi:10.1038/s41612-020-0121-5. hdl:10356/143900. S2CID 218541055.
11. ^ Silvano, Alessandro; Rintoul, Stephen Rich; Peña-Molino, Beatriz; Hobbs, William Richard; van Wijk, Esmee; Aoki, Shigeru; Tamura, Takeshi; Williams, Guy Darvall (18 April 2018). "Freshening by glacial meltwater enhances the melting of ice shelves and reduces the formation of Antarctic Bottom Water". Science Advances. 4 (4): eaap9467. doi:10.1126/sciadv.aap9467. PMC 5906079. PMID 29675467.
12. ^ Pan, Xianliang L.; Li, Bofeng F.; Watanabe, Yutaka W. (10 January 2022). "Intense ocean freshening from melting glacier around the Antarctica during early twenty-first century". Scientific Reports. 12 (1): 383. Bibcode:2022NatSR..12..383P. doi:10.1038/s41598-021-04231-6. ISSN 2045-2322. PMC 8748732. PMID 35013425.
13. ^ Lenton, T. M.; Armstrong McKay, D.I.; Loriani, S.; Abrams, J.F.; Lade, S.J.; Donges, J.F.; Milkoreit, M.; Powell, T.; Smith, S.R.; Zimm, C.; Buxton, J.E.; Daube, Bruce C.; Krummel, Paul B.; Loh, Zoë; Luijkx, Ingrid T. (2023). The Global Tipping Points Report 2023 (Report). University of Exeter.
14. ^ Logan, Tyne (29 March 2023). "Landmark study projects 'dramatic' changes to Southern Ocean by 2050". ABC News.
15. Roland, Thomas P.; Bartlett, Oliver T.; Charman, Dan J.; Anderson, Karen; Hodgson, Dominic A.; Amesbury, Matthew J.; Maclean, Ilya; Fretwell, Peter T.; Fleming, Andrew (4 October 2024). "Sustained greening of the Antarctic Peninsula observed from satellites". Nature Geoscience: 1–6. doi:10.1038/s41561-024-01564-5. ISSN 1752-0908.
16. ^ Potapowicz, Joanna; Szumińska, Danuta; Szopińska, Małgorzata; Polkowska, Żaneta (15 February 2019). "The influence of global climate change on the environmental fate of anthropogenic pollution released from the permafrost: Part I. Case study of Antarctica". Science of the Total Environment. 651 (Pt 1): 1534–1548. doi:10.1016/j.scitotenv.2018.09.168. ISSN 0048-9697. PMID 30360282. S2CID 53093132.
17. ^ Carlson, Anders E; Walczak, Maureen H; Beard, Brian L; Laffin, Matthew K; Stoner, Joseph S; Hatfield, Robert G (10 December 2018). Absence of the West Antarctic ice sheet during the last interglaciation. American Geophysical Union Fall Meeting.
18. ^ Lau, Sally C. Y.; Wilson, Nerida G.; Golledge, Nicholas R.; Naish, Tim R.; Watts, Phillip C.; Silva, Catarina N. S.; Cooke, Ira R.; Allcock, A. Louise; Mark, Felix C.; Linse, Katrin (21 December 2023). "Genomic evidence for West Antarctic Ice Sheet collapse during the Last Interglacial" (PDF). Science. 382 (6677): 1384–1389. Bibcode:2023Sci...382.1384L. doi:10.1126/science.ade0664. PMID 38127761. S2CID 266436146.
19. ^ A. Naughten, Kaitlin; R. Holland, Paul; De Rydt, Jan (23 October 2023). "Unavoidable future increase in West Antarctic ice-shelf melting over the twenty-first century". Nature Climate Change. 13 (11): 1222–1228. Bibcode:2023NatCC..13.1222N. doi:10.1038/s41558-023-01818-x. S2CID 264476246.
20. ^ Garbe, Julius; Albrecht, Torsten; Levermann, Anders; Donges, Jonathan F.; Winkelmann, Ricarda (2020). "The hysteresis of the Antarctic Ice Sheet". Nature. 585 (7826): 538–544. Bibcode:2020Natur.585..538G. doi:10.1038/s41586-020-2727-5. PMID 32968257. S2CID 221885420.
21. ^ Armstrong McKay, David; Abrams, Jesse; Winkelmann, Ricarda; Sakschewski, Boris; Loriani, Sina; Fetzer, Ingo; Cornell, Sarah; Rockström, Johan; Staal, Arie; Lenton, Timothy (9 September 2022). "Exceeding 1.5 °C global warming could trigger multiple climate tipping points". Science. 377 (6611): eabn7950. doi:10.1126/science.abn7950. hdl:10871/131584. ISSN 0036-8075. PMID 36074831. S2CID 252161375.
22. ^ Armstrong McKay, David (9 September 2022). "Exceeding 1.5 °C global warming could trigger multiple climate tipping points – paper explainer". climatetippingpoints.info. Retrieved 2 October 2022.
23. ^ Pan, Linda; Powell, Evelyn M.; Latychev, Konstantin; Mitrovica, Jerry X.; Creveling, Jessica R.; Gomez, Natalya; Hoggard, Mark J.; Clark, Peter U. (30 April 2021). "Rapid postglacial rebound amplifies global sea level rise following West Antarctic Ice Sheet collapse". Science Advances. 7 (18). Bibcode:2021SciA....7.7787P. doi:10.1126/sciadv.abf7787. PMC 8087405. PMID 33931453.
24. ^ Fretwell, P.; et al. (28 February 2013). "Bedmap2: improved ice bed, surface and thickness datasets for Antarctica" (PDF). The Cryosphere. 7 (1): 390. Bibcode:2013TCry....7..375F. doi:10.5194/tc-7-375-2013. S2CID 13129041. Archived (PDF) from the original on 16 February 2020. Retrieved 6 January 2014.
25. ^ Crotti, Ilaria; Quiquet, Aurélien; Landais, Amaelle; Stenni, Barbara; Wilson, David J.; Severi, Mirko; Mulvaney, Robert; Wilhelms, Frank; Barbante, Carlo; Frezzotti, Massimo (10 September 2022). "Wilkes subglacial basin ice sheet response to Southern Ocean warming during late Pleistocene interglacials". Nature Communications. 13 (1): 5328. Bibcode:2022NatCo..13.5328C. doi:10.1038/s41467-022-32847-3. PMC 9464198. PMID 36088458.
26. ^ Sejas, Sergio A.; Taylor, Patrick C.; Cai, Ming (11 July 2018). "Unmasking the negative greenhouse effect over the Antarctic Plateau". npj Climate and Atmospheric Science. 1 (1): 17. Bibcode:2018npCAS...1...17S. doi:10.1038/s41612-018-0031-y. PMC 7580794. PMID 33102742.
27. ^ Stewart, K. D.; Hogg, A. McC.; England, M. H.; Waugh, D. W. (2 November 2020). "Response of the Southern Ocean Overturning Circulation to Extreme Southern Annular Mode Conditions". Geophysical Research Letters. 47 (22): e2020GL091103. Bibcode:2020GeoRL..4791103S. doi:10.1029/2020GL091103. hdl:1885/274441. S2CID 229063736.
28. John Theodore, Houghton, ed. (2001). "Figure 9.8: Multi-model annual mean zonal temperature change (top), zonal mean temperature change range (middle) and the zonal mean change divided by the multi-model standard deviation of the mean change (bottom) for the CMIP2 simulations". Climate change 2001: the scientific basis: contribution of Working Group I to the Third Assessment Report of the Intergovernmental Panel on Climate Change. Cambridge, UK: Cambridge University Press. ISBN 978-0-521-80767-8. Archived from the original on 30 March 2016. Retrieved 18 December 2019.
29. J. H. Christensen; B. Hewitson; A. Busuioc; A. Chen; X. Gao; I. Held; R. Jones; R.K. Kolli; W.-T. Kwon; R. Laprise; V. Magaña Rueda; L. Mearns; C. G. Menéndez; J. Räisänen; A. Rinke; A. Sarr; P. Whetton (2007). Regional Climate Projections (In: Climate Change 2007: The Physical Science Basis. Contribution of Working Group I to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change) (PDF) (Report). Archived from the original (PDF) on 15 December 2007. Retrieved 5 November 2007.
30. Chapman, William L.; Walsh, John E. (2007). "A Synthesis of Antarctic Temperatures". Journal of Climate. 20 (16): 4096–4117. Bibcode:2007JCli...20.4096C. doi:10.1175/JCLI4236.1.
31. Comiso, Josefino C. (2000). "Variability and Trends in Antarctic Surface Temperatures from In Situ and Satellite Infrared Measurements". Journal of Climate. 13 (10): 1674–1696. Bibcode:2000JCli...13.1674C. doi:10.1175/1520-0442(2000)013<1674:vatias>2.0.co;2. PDF available at AMS Online
32. Thompson, David W. J.; Solomon, Susan (2002). "Interpretation of Recent Southern Hemisphere Climate Change" (PDF). Science. 296 (5569): 895–899. Bibcode:2002Sci...296..895T. doi:10.1126/science.1069270. PMID 11988571. S2CID 7732719. Archived from the original (PDF) on 11 August 2011. Retrieved 14 August 2008. PDF available at Annular Modes Website
33. ^ Doran, Peter T.; Priscu, JC; Lyons, WB; et al. (January 2002). "Antarctic climate cooling and terrestrial ecosystem response" (PDF). Nature. 415 (6871): 517–20. doi:10.1038/nature710. PMID 11793010. S2CID 387284. Archived from the original (PDF) on 11 December 2004.
34. Obryk, M. K.; Doran, P. T.; Fountain, A. G.; Myers, M.; McKay, C. P. (16 July 2020). "Climate From the McMurdo Dry Valleys, Antarctica, 1986–2017: Surface Air Temperature Trends and Redefined Summer Season". Journal of Geophysical Research: Atmospheres. 125 (13). Bibcode:2020JGRD..12532180O. doi:10.1029/2019JD032180. ISSN 2169-897X. S2CID 219738421.
35. "Scientific winds blow hot and cold in Antarctica". CNN. 25 January 2002. Retrieved 13 April 2013.
36. Chang, Kenneth (2 April 2002). "The Melting (Freezing) of Antarctica; Deciphering Contradictory Climate Patterns Is Largely a Matter of Ice". The New York Times. Retrieved 13 April 2013.
37. Derbyshire, David (14 January 2002). "Antarctic cools in warmer world". The Daily Telegraph. London. Archived from the original on 2 June 2014. Retrieved 13 April 2013.
38. Peter N. Spotts (18 January 2002). "Guess what? Antarctica's getting colder, not warmer". The Christian Science Monitor. Retrieved 13 April 2013.
39. Bijal P. Trivedi (25 January 2002). "Antarctica Gives Mixed Signals on Warming". National Geographic. Archived from the original on 28 January 2002. Retrieved 13 April 2013.
40. "Antarctic cooling pushing life closer to the edge". USA Today. 16 January 2002. Retrieved 13 April 2013.
41. ^ Peter Doran (27 July 2006). "Cold, Hard Facts". The New York Times. Archived from the original on 11 April 2009. Retrieved 14 August 2008.
42. Davidson, Keay (4 February 2002). "Media goofed on Antarctic data / Global warming interpretation irks scientists". San Francisco Chronicle. Retrieved 13 April 2013.
43. Crichton, Michael (2004). State of Fear. HarperCollins, New York. p. 109. ISBN 978-0-06-621413-9. The data show that one relatively small area called the Antarctic Peninsula is melting and calving huge icebergs. That's what gets reported year after year. But the continent as a whole is getting colder, and the ice is getting thicker. First Edition
44. Eric Steig; Gavin Schmidt (3 December 2004). "Antarctic cooling, global warming?". Real Climate. Retrieved 14 August 2008. At first glance this seems to contradict the idea of 'global' warming, but one needs to be careful before jumping to this conclusion. A rise in the global mean temperature does not imply universal warming. Dynamical effects (changes in the winds and ocean circulation) can have just as large an impact, locally as the radiative forcing from greenhouse gases. The temperature change in any particular region will in fact be a combination of radiation-related changes (through greenhouse gases, aerosols, ozone and the like) and dynamical effects. Since the winds tend to only move heat from one place to another, their impact will tend to cancel out in the global mean.
45. "America Reacts To Speech Debunking Media Global Warming Alarmism". U.S. Senate Committee on Environment and Public Works. 28 September 2006. Archived from the original on 5 March 2013. Retrieved 13 April 2013.
46. "Climate Change—Our Research". British Antarctic Survey. Archived from the original on 7 February 2006.
47. NASA (2007). "Two Decades of Temperature Change in Antarctica". Earth Observatory Newsroom. Archived from the original on 20 September 2008. Retrieved 14 August 2008. NASA image by Robert Simmon, based on data from Joey Comiso, GSFC.
48. Kenneth Chang (21 January 2009). "Warming in Antarctica Looks Certain". The New York Times. Archived from the original on 13 November 2014. Retrieved 13 April 2013.
49. Ding, Qinghua; Eric J. Steig; David S. Battisti; Marcel Küttel (10 April 2011). "Winter warming in West Antarctica caused by central tropical Pacific warming". Nature Geoscience. 4 (6): 398–403. Bibcode:2011NatGe...4..398D. CiteSeerX 10.1.1.459.8689. doi:10.1038/ngeo1129.
50. A. Orsi; Bruce D. Cornuelle; J. Severinghaus (2012). "Little Ice Age cold interval in West Antarctica: Evidence from borehole temperature at the West Antarctic Ice Sheet (WAIS) Divide". Geophysical Research Letters. 39 (9): L09710. Bibcode:2012GeoRL..39.9710O. doi:10.1029/2012GL051260.
51. Bromwich, D. H.; Nicolas, J. P.; Monaghan, A. J.; Lazzara, M. A.; Keller, L. M.; Weidner, G. A.; Wilson, A. B. (2012). "Central West Antarctica among the most rapidly warming regions on Earth". Nature Geoscience. 6 (2): 139. Bibcode:2013NatGe...6..139B. CiteSeerX 10.1.1.394.1974. doi:10.1038/ngeo1671.
    Steig, Eric (23 December 2012). "The heat is on in West Antarctica". RealClimate. Retrieved 20 January 2013.
52. J P. Nicolas; J. P.; D. H. Bromwich (2014). "New reconstruction of Antarctic near-surface temperatures: Multidecadal trends and reliability of global reanalyses". Journal of Climate. 27 (21): 8070–8093. Bibcode:2014JCli...27.8070N. CiteSeerX 10.1.1.668.6627. doi:10.1175/JCLI-D-13-00733.1. S2CID 21537289.
53. McGrath, Matt (23 December 2012). "West Antarctic Ice Sheet warming twice earlier estimate". BBC News. Retrieved 16 February 2013.
54. Ludescher, Josef; Bunde, Armin; Franzke, Christian L. E.; Schellnhuber, Hans Joachim (16 April 2015). "Long-term persistence enhances uncertainty about anthropogenic warming of Antarctica". Climate Dynamics. 46 (1–2): 263–271. Bibcode:2016ClDy...46..263L. doi:10.1007/s00382-015-2582-5. S2CID 131723421.
55. Dalaiden, Quentin; Schurer, Andrew P.; Kirchmeier-Young, Megan C.; Goosse, Hugues; Hegerl, Gabriele C. (24 August 2022). "West Antarctic Surface Climate Changes Since the Mid-20th Century Driven by Anthropogenic Forcing" (PDF). Geophysical Research Letters. 49 (16). Bibcode:2022GeoRL..4999543D. doi:10.1029/2022GL099543. hdl:20.500.11820/64ecd5a1-af19-43e8-9d34-da7274cc4ae0. S2CID 251854055.
56. Turner, John; Lu, Hua; White, Ian; King, John C.; Phillips, Tony; Hosking, J. Scott; Bracegirdle, Thomas J.; Marshall, Gareth J.; Mulvaney, Robert; Deb, Pranab (2016). "Absence of 21st century warming on Antarctic Peninsula consistent with natural variability" (PDF). Nature. 535 (7612): 411–415. Bibcode:2016Natur.535..411T. doi:10.1038/nature18645. PMID 27443743. S2CID 205249862.
57. Steig, Eric J. (2016). "Cooling in the Antarctic". Nature. 535 (7612): 358–359. doi:10.1038/535358a. PMID 27443735.
58. Trenberth, Kevin E.; Fasullo, John T.; Branstator, Grant; Phillips, Adam S. (2014). "Seasonal aspects of the recent pause in surface warming". Nature Climate Change. 4 (10): 911–916. Bibcode:2014NatCC...4..911T. doi:10.1038/NCLIMATE2341.
59. Chang, Kenneth (3 May 2002). "Ozone Hole Is Now Seen as a Cause for Antarctic Cooling". The New York Times. Retrieved 13 April 2013.
60. Shindell, Drew T.; Schmidt, Gavin A. (2004). "Southern Hemisphere climate response to ozone changes and greenhouse gas increases". Geophys. Res. Lett. 31 (18): L18209. Bibcode:2004GeoRL..3118209S. doi:10.1029/2004GL020724.
61. Thompson, David W. J.; Solomon, Susan; Kushner, Paul J.; England, Matthew H.; Grise, Kevin M.; Karoly, David J. (23 October 2011). "Signatures of the Antarctic ozone hole in Southern Hemisphere surface climate change". Nature Geoscience. 4 (11): 741–749. Bibcode:2011NatGe...4..741T. doi:10.1038/ngeo1296. S2CID 40243634.
62. Meredith, M.; Sommerkorn, M.; Cassotta, S; Derksen, C.; et al. (2019). "Chapter 3: Polar Regions" (PDF). IPCC Special Report on the Ocean and Cryosphere in a Changing Climate. p. 212.
63. Xin, Meijiao; Li, Xichen; Stammerjohn, Sharon E; Cai, Wenju; Zhu, Jiang; Turner, John; Clem, Kyle R; Song, Chentao; Wang, Wenzhu; Hou, Yurong (17 May 2023). "A broadscale shift in antarctic temperature trends". Climate Dynamics. 61 (9–10): 4623–4641. Bibcode:2023ClDy...61.4623X. doi:10.1007/s00382-023-06825-4. S2CID 258777741.
64. Stammerjohn, Sharon E.; Scambos, Ted A. (August 2020). "Warming reaches the South Pole". Nature Climate Change. 10 (8): 710–711. Bibcode:2020NatCC..10..710S. doi:10.1038/s41558-020-0827-8. ISSN 1758-6798. S2CID 220260051.
65. Larson, Christina (8 February 2020). "Antarctica appears to have broken a heat record". phys.org.
66. Hughes, Kevin A.; Convey, Peter; Turner, John (1 October 2021). "Developing resilience to climate change impacts in Antarctica: An evaluation of Antarctic Treaty System protected area policy". Environmental Science & Policy. 124: 12–22. Bibcode:2021ESPol.124...12H. doi:10.1016/j.envsci.2021.05.023. ISSN 1462-9011. S2CID 236282417.
67. ^ Hausfather, Zeke; Peters, Glen (29 January 2020). "Emissions – the 'business as usual' story is misleading". Nature. 577 (7792): 618–20. Bibcode:2020Natur.577..618H. doi:10.1038/d41586-020-00177-3. PMID 31996825.
68. ^ Schuur, Edward A.G.; Abbott, Benjamin W.; Commane, Roisin; Ernakovich, Jessica; Euskirchen, Eugenie; Hugelius, Gustaf; Grosse, Guido; Jones, Miriam; Koven, Charlie; Leshyk, Victor; Lawrence, David; Loranty, Michael M.; Mauritz, Marguerite; Olefeldt, David; Natali, Susan; Rodenhizer, Heidi; Salmon, Verity; Schädel, Christina; Strauss, Jens; Treat, Claire; Turetsky, Merritt (2022). "Permafrost and Climate Change: Carbon Cycle Feedbacks From the Warming Arctic". Annual Review of Environment and Resources. 47: 343–371. Bibcode:2022ARER...47..343S. doi:10.1146/annurev-environ-012220-011847. Medium-range estimates of Arctic carbon emissions could result from moderate climate emission mitigation policies that keep global warming below 3 °C (e.g., RCP4.5). This global warming level most closely matches country emissions reduction pledges made for the Paris Climate Agreement...
69. ^ Phiddian, Ellen (5 April 2022). "Explainer: IPCC Scenarios". Cosmos. Retrieved 30 September 2023. The IPCC doesn't make projections about which of these scenarios is more likely, but other researchers and modellers can. The Australian Academy of Science, for instance, released a report last year stating that our current emissions trajectory had us headed for a 3 °C warmer world, roughly in line with the middle scenario. Climate Action Tracker predicts 2.5 to 2.9 °C of warming based on current policies and action, with pledges and government agreements taking this to 2.13 °C.
70. IPCC, 2021: Summary for Policymakers. In: Climate Change 2021: The Physical Science Basis. Contribution of Working Group I to the Sixth Assessment Report of the Intergovernmental Panel on Climate Change . Cambridge University Press, Cambridge, United Kingdom and New York, New York, US, pp. 3−32, doi:10.1017/9781009157896.001.
71. von Schuckmann, K.; Cheng, L.; Palmer, M. D.; Hansen, J.; et al. (7 September 2020). "Heat stored in the Earth system: where does the energy go?". Earth System Science Data. 12 (3): 2013–2041. Bibcode:2020ESSD...12.2013V. doi:10.5194/essd-12-2013-2020. hdl:20.500.11850/443809. Text was copied from this source, which is available under a Creative Commons Attribution 4.0 International License
72. Long, Matthew C.; Stephens, Britton B.; McKain, Kathryn; Sweeney, Colm; Keeling, Ralph F.; Kort, Eric A.; Morgan, Eric J.; Bent, Jonathan D.; Chandra, Naveen; Chevallier, Frederic; Commane, Róisín; Daube, Bruce C.; Krummel, Paul B.; Loh, Zoë; Luijkx, Ingrid T.; Munro, David; Patra, Prabir; Peters, Wouter; Ramonet, Michel; Rödenbeck, Christian; Stavert, Ann; Tans, Pieter; Wofsy, Steven C. (2 December 2021). "Strong Southern Ocean carbon uptake evident in airborne observations". Science. 374 (6572): 1275–1280. Bibcode:2021Sci...374.1275L. doi:10.1126/science.abi4355. PMID 34855495. S2CID 244841359.
73. Terhaar, Jens; Frölicher, Thomas L.; Joos, Fortunat (28 April 2021). "Southern Ocean anthropogenic carbon sink constrained by sea surface salinity" (PDF). Science Advances. 7 (18): 1275–1280. Bibcode:2021Sci...374.1275L. doi:10.1126/science.abi4355. PMID 34855495. S2CID 244841359.
74. ^ "NOAA Scientists Detect a Reshaping of the Meridional Overturning Circulation in the Southern Ocean". NOAA. 29 March 2023.
75. Pellichero, Violaine; Sallée, Jean-Baptiste; Chapman, Christopher C.; Downes, Stephanie M. (3 May 2018). "The southern ocean meridional overturning in the sea-ice sector is driven by freshwater fluxes". Nature Communications. 9 (1): 1789. Bibcode:2018NatCo...9.1789P. doi:10.1038/s41467-018-04101-2. PMC 5934442. PMID 29724994.
76. ^ Lee, Sang-Ki; Lumpkin, Rick; Gomez, Fabian; Yeager, Stephen; Lopez, Hosmay; Takglis, Filippos; Dong, Shenfu; Aguiar, Wilton; Kim, Dongmin; Baringer, Molly (13 March 2023). "Human-induced changes in the global meridional overturning circulation are emerging from the Southern Ocean". Communications Earth & Environment. 4 (1): 69. Bibcode:2023ComEE...4...69L. doi:10.1038/s43247-023-00727-3.
77. Zhou, Shenjie; Meijers, Andrew J. S.; Meredith, Michael P.; Abrahamsen, E. Povl; Holland, Paul R.; Silvano, Alessandro; Sallée, Jean-Baptiste; Østerhus, Svein (12 June 2023). "Slowdown of Antarctic Bottom Water export driven by climatic wind and sea-ice changes". Nature Climate Change. 13 (6): 701–709. Bibcode:2023NatCC..13..537G. doi:10.1038/s41558-023-01667-8.
78. Silvano, Alessandro; Meijers, Andrew J. S.; Zhou, Shenjie (17 June 2023). "Slowing deep Southern Ocean current may be linked to natural climate cycle—but melting Antarctic ice is still a concern". The Conversation.
79. Aoki, S.; Yamazaki, K.; Hirano, D.; Katsumata, K.; Shimada, K.; Kitade, Y.; Sasaki, H.; Murase, H. (15 September 2020). "Reversal of freshening trend of Antarctic Bottom Water in the Australian-Antarctic Basin during 2010s". Scientific Reports. 10 (1): 14415. doi:10.1038/s41598-020-71290-6. PMC 7492216. PMID 32934273.
80. ^ Li, Qian; England, Matthew H.; Hogg, Andrew McC.; Rintoul, Stephen R.; Morrison, Adele K. (29 March 2023). "Abyssal ocean overturning slowdown and warming driven by Antarctic meltwater". Nature. 615 (7954): 841–847. Bibcode:2023Natur.615..841L. doi:10.1038/s41586-023-05762-w. PMID 36991191. S2CID 257807573.
81. Haumann, F. Alexander; Gruber, Nicolas; Münnich, Matthias; Frenger, Ivy; Kern, Stefan (September 2016). "Sea-ice transport driving Southern Ocean salinity and its recent trends". Nature. 537 (7618): 89–92. Bibcode:2016Natur.537...89H. doi:10.1038/nature19101. hdl:20.500.11850/120143. ISSN 1476-4687. PMID 27582222. S2CID 205250191.
82. Liu, Y.; Moore, J. K.; Primeau, F.; Wang, W. L. (22 December 2022). "Reduced CO2 uptake and growing nutrient sequestration from slowing overturning circulation". Nature Climate Change. 13: 83–90. doi:10.1038/s41558-022-01555-7. OSTI 2242376. S2CID 255028552.
83. King, M. A.; Bingham, R. J.; Moore, P.; Whitehouse, P. L.; Bentley, M. J.; Milne, G. A. (2012). "Lower satellite-gravimetry estimates of Antarctic sea-level contribution". Nature. 491 (7425): 586–589. Bibcode:2012Natur.491..586K. doi:10.1038/nature11621. PMID 23086145. S2CID 4414976.
84. ^ IMBIE team (13 June 2018). "Mass balance of the Antarctic Ice Sheet from 1992 to 2017". Nature. 558 (7709): 219–222. Bibcode:2018Natur.558..219I. doi:10.1038/s41586-018-0179-y. hdl:2268/225208. PMID 29899482. S2CID 49188002.
85. Zwally, H. Jay; Robbins, John W.; Luthcke, Scott B.; Loomis, Bryant D.; Rémy, Frédérique (29 March 2021). "Mass balance of the Antarctic ice sheet 1992–2016: reconciling results from GRACE gravimetry with ICESat, ERS1/2 and Envisat altimetry". Journal of Glaciology. 67 (263): 533–559. Bibcode:2021JGlac..67..533Z. doi:10.1017/jog.2021.8. Although their methods of interpolation or extrapolation for areas with unobserved output velocities have an insufficient description for the evaluation of associated errors, such errors in previous results (Rignot and others, 2008) caused large overestimates of the mass losses as detailed in Zwally and Giovinetto (Zwally and Giovinetto, 2011).
86. ^ Cordero, Raúl R.; Sepúlveda, Edgardo; Feron, Sarah; Damiani, Alessandro; Fernandoy, Francisco; Neshyba, Steven; Rowe, Penny M.; Asencio, Valentina; Carrasco, Jorge; Alfonso, Juan A.; Llanillo, Pedro (22 February 2022). "Black carbon footprint of human presence in Antarctica". Nature Communications. 13 (1): 984. Bibcode:2022NatCo..13..984C. doi:10.1038/s41467-022-28560-w. ISSN 2041-1723. PMC 8863810. PMID 35194040.
87. Thackeray, Chad W.; Fletcher, Christopher G. (June 2016). "Snow albedo feedback: Current knowledge, importance, outstanding issues and future directions". Progress in Physical Geography: Earth and Environment. 40 (3): 392–408. doi:10.1177/0309133315620999. ISSN 0309-1333. S2CID 130252885.
88. Kinase, T.; Adachi, K.; Oshima, N.; Goto-Azuma, K.; Ogawa-Tsukagawa, Y.; Kondo, Y.; Moteki, N.; Ohata, S.; Mori, T.; Hayashi, M.; Hara, K.; Kawashima, H.; Kita, K. (17 December 2019). "Concentrations and Size Distributions of Black Carbon in the Surface Snow of Eastern Antarctica in 2011". Journal of Geophysical Research: Atmospheres. 125 (1): e2019JD030737. doi:10.1029/2019JD030737.
89. Marquetto, Luciano; Kaspari, Susan; Simões, Jefferson Cardia (15 September 2020). "Refractory black carbon (rBC) variability in a 47-year West Antarctic snow and firn core". The Cryosphere. 14 (5): 1537–1554. Bibcode:2020TCry...14.1537M. doi:10.5194/tc-14-1537-2020.
90. Cereceda-Balic, Francisco; Vidal, Víctor; Ruggeri, María Florencia; González, Humberto E. (15 November 2020). "Black carbon pollution in snow and its impact on albedo near the Chilean stations on the Antarctic peninsula: First results". Science of the Total Environment. 743: 140801. Bibcode:2020ScTEn.74340801C. doi:10.1016/j.scitotenv.2020.140801. ISSN 0048-9697. PMID 32673927. S2CID 220608494.
91. Pattyn, Frank (16 July 2018). "The paradigm shift in Antarctic ice sheet modelling". Nature Communications. 9 (1): 2728. Bibcode:2018NatCo...9.2728P. doi:10.1038/s41467-018-05003-z. PMC 6048022. PMID 30013142.
92. Robel, Alexander A.; Seroussi, Hélène; Roe, Gerard H. (23 July 2019). "Marine ice sheet instability amplifies and skews uncertainty in projections of future sea-level rise". Proceedings of the National Academy of Sciences. 116 (30): 14887–14892. Bibcode:2019PNAS..11614887R. doi:10.1073/pnas.1904822116. PMC 6660720. PMID 31285345.
93. Perkins, Sid (17 June 2021). "Collapse may not always be inevitable for marine ice cliffs". Science News. Retrieved 9 January 2023.
94. DeConto, Robert M.; Pollard, David; Alley, Richard B.; Velicogna, Isabella; Gasson, Edward; Gomez, Natalya; Sadai, Shaina; Condron, Alan; Gilford, Daniel M.; Ashe, Erica L.; Kopp, Robert E. (May 2021). "The Paris Climate Agreement and future sea-level rise from Antarctica". Nature. 593 (7857): 83–89. Bibcode:2021Natur.593...83D. doi:10.1038/s41586-021-03427-0. hdl:10871/125843. ISSN 1476-4687. PMID 33953408. S2CID 233868268.
95. ^ "Anticipating Future Sea Levels". EarthObservatory.NASA.gov. National Aeronautics and Space Administration (NASA). 2021. Archived from the original on 7 July 2021.
96. Bamber, J.L.; Riva, R.E.M.; Vermeersen, B.L.A.; LeBrocq, A.M. (14 May 2009). "Reassessment of the Potential Sea-Level Rise from a Collapse of the West Antarctic Ice Sheet". Science. 324 (5929): 901–903. Bibcode:2009Sci...324..901B. doi:10.1126/science.1169335. PMID 19443778. S2CID 11083712.
97. Voosen, Paul (18 December 2018). "Discovery of recent Antarctic ice sheet collapse raises fears of a new global flood". Science. Retrieved 28 December 2018.
98. Turney, Chris S. M.; Fogwill, Christopher J.; Golledge, Nicholas R.; McKay, Nicholas P.; Sebille, Erik van; Jones, Richard T.; Etheridge, David; Rubino, Mauro; Thornton, David P.; Davies, Siwan M.; Ramsey, Christopher Bronk (11 February 2020). "Early Last Interglacial ocean warming drove substantial ice mass loss from Antarctica". Proceedings of the National Academy of Sciences. 117 (8): 3996–4006. Bibcode:2020PNAS..117.3996T. doi:10.1073/pnas.1902469117. ISSN 0027-8424. PMC 7049167. PMID 32047039.
99. AHMED, Issam. "Antarctic octopus DNA reveals ice sheet collapse closer than thought". phys.org. Retrieved 23 December 2023.
100. Poynting, Mark (24 October 2023). "Sea-level rise: West Antarctic ice shelf melt 'unavoidable'". BBC News. Retrieved 26 October 2023.
101. Wolovick, Michael; Moore, John; Keefer, Bowie (27 March 2023). "Feasibility of ice sheet conservation using seabed anchored curtains". PNAS Nexus. 2 (3): pgad053. doi:10.1093/pnasnexus/pgad053. PMC 10062297. PMID 37007716.
102. Wolovick, Michael; Moore, John; Keefer, Bowie (27 March 2023). "The potential for stabilizing Amundsen Sea glaciers via underwater curtains". PNAS Nexus. 2 (4): pgad103. doi:10.1093/pnasnexus/pgad103. PMC 10118300. PMID 37091546.
103. Curtosi, Antonio; Pelletier, Emilien; Vodopivez, Cristian L.; Cormack, Walter P. Mac (August 2009). "Distribution of PAHs in the water column, sediments and biota of Potter Cove, South Shetland Islands, Antarctica". Antarctic Science. 21 (4): 329–339. Bibcode:2009AntSc..21..329C. doi:10.1017/S0954102009002004. ISSN 1365-2079. S2CID 130818024.
104. Jara-Carrasco, S.; González, M.; González-Acuña, D.; Chiang, G.; Celis, J.; Espejo, W.; Mattatall, P.; Barra, R. (August 2015). "Potential immunohaematological effects of persistent organic pollutants on chinstrap penguin". Antarctic Science. 27 (4): 373–381. Bibcode:2015AntSc..27..373J. doi:10.1017/S0954102015000012. ISSN 0954-1020. S2CID 53415356.
105. Goutte, Aurélie; Cherel, Yves; Churlaud, Carine; Ponthus, Jean-Pierre; Massé, Guillaume; Bustamante, Paco (15 December 2015). "Trace elements in Antarctic fish species and the influence of foraging habitats and dietary habits on mercury levels". Science of the Total Environment. 538: 743–749. Bibcode:2015ScTEn.538..743G. doi:10.1016/j.scitotenv.2015.08.103. ISSN 0048-9697. PMID 26327642.
106. Jossart, Quentin; Moreau, Camille; Agüera, Antonio; Broyer, Claude De; Danis, Bruno (30 September 2015). "The Register of Antarctic Marine Species (RAMS): a ten-year appraisal". ZooKeys (524): 137–145. Bibcode:2015ZooK..524..137J. doi:10.3897/zookeys.524.6091. ISSN 1313-2989. PMC 4602294. PMID 26478709.
107. Gutt, Julian; Sirenko, Boris I.; Smirnov, Igor S.; Arntz, Wolf E. (March 2004). "How many macrozoobenthic species might inhabit the Antarctic shelf?". Antarctic Science. 16 (1): 11–16. Bibcode:2004AntSc..16...11G. doi:10.1017/S0954102004001750. ISSN 1365-2079. S2CID 86092653.
108. Griffiths, Huw J. (2 August 2010). "Antarctic Marine Biodiversity – What Do We Know About the Distribution of Life in the Southern Ocean?". PLOS ONE. 5 (8): e11683. Bibcode:2010PLoSO...511683G. doi:10.1371/journal.pone.0011683. ISSN 1932-6203. PMC 2914006. PMID 20689841.
109. ^ Constable, A.J.; Harper, S.; Dawson, J.; Holsman, K.; Mustonen, T.; Piepenburg, D.; Rost, B. (2022). "Cross-Chapter Paper 6: Polar Regions". Climate Change 2022: Impacts, Adaptation and Vulnerability. 2021: 2319–2367. Bibcode:2021AGUFM.U13B..05K. doi:10.1017/9781009325844.023.
110. Constable, Andrew J.; Melbourne-Thomas, Jessica; Corney, Stuart P.; Arrigo, Kevin R.; Barbraud, Christophe; Barnes, David K. A.; Bindoff, Nathaniel L.; Boyd, Philip W.; Brandt, Angelika; Costa, Daniel P.; Davidson, Andrew T. (2014). "Climate change and Southern Ocean ecosystems I: how changes in physical habitats directly affect marine biota". Global Change Biology. 20 (10): 3004–3025. Bibcode:2014GCBio..20.3004C. doi:10.1111/gcb.12623. ISSN 1365-2486. PMID 24802817. S2CID 7584865.
111. Smetacek, Victor; Nicol, Stephen (September 2005). "Polar ocean ecosystems in a changing world". Nature. 437 (7057): 362–368. Bibcode:2005Natur.437..362S. doi:10.1038/nature04161. ISSN 0028-0836. PMID 16163347. S2CID 4388240.
112. Tulloch, Vivitskaia J. D.; Plagányi, Éva E.; Brown, Christopher; Richardson, Anthony J.; Matear, Richard (April 2019). "Future recovery of baleen whales is imperiled by climate change". Global Change Biology. 25 (4): 1263–1281. Bibcode:2019GCBio..25.1263T. doi:10.1111/gcb.14573. PMC 6850638. PMID 30807685.
113. ^ McCarthy, Arlie H.; Peck, Lloyd S.; Hughes, Kevin A.; Aldridge, David C. (July 2019). "Antarctica: The final frontier for marine biological invasions". Global Change Biology. 25 (7): 2221–2241. Bibcode:2019GCBio..25.2221M. doi:10.1111/gcb.14600. ISSN 1354-1013. PMC 6849521. PMID 31016829.
114. Nunez, Sarahi; Arets, Eric; Alkemade, Rob; Verwer, Caspar; Leemans, Rik (2019). "Assessing the impacts of climate change on biodiversity: Is below 2 °C enough?". Climatic Change. 154 (3–4): 351–365. Bibcode:2019ClCh..154..351N. doi:10.1007/s10584-019-02420-x. S2CID 181651307.
115. Dykyy, Ihor; Bedernichek, Tymur (January 2022). "Gentoo Penguins (Pygoscelis papua) started using mosses as nesting material in the southernmost colony on the Antarctic Peninsula (Cape Tuxen, Graham Land)". Polar Biology. 45 (1): 149–152. Bibcode:2022PoBio..45..149D. doi:10.1007/s00300-021-02968-4. ISSN 0722-4060. S2CID 244363982.
116. Davis, Margaret B.; Shaw, Ruth G.; Etterson, Julie R. (July 2005). "Evolutionary Responses to Changing Climate". Ecology. 86 (7): 1704–1714. Bibcode:2005Ecol...86.1704D. doi:10.1890/03-0788. hdl:11299/178230. ISSN 0012-9658.
117. Pickett, Erin P.; Fraser, William R.; Patterson-Fraser, Donna L.; Cimino, Megan A.; Torres, Leigh G.; Friedlaender, Ari S. (October 2018). "Spatial niche partitioning may promote coexistence of Pygoscelis penguins as climate-induced sympatry occurs". Ecology and Evolution. 8 (19): 9764–9778. Bibcode:2018EcoEv...8.9764P. doi:10.1002/ece3.4445. ISSN 2045-7758. PMC 6202752. PMID 30386573.
118. Le Bohec, C.; Durant, J. M.; Gauthier-Clerc, M.; Stenseth, N. C.; Park, Y.-H.; Pradel, R.; Gremillet, D.; Gendner, J.-P.; Le Maho, Y. (11 February 2008). "King penguin population threatened by Southern Ocean warming". Proceedings of the National Academy of Sciences. 105 (7): 2493–2497. Bibcode:2008PNAS..105.2493L. doi:10.1073/pnas.0712031105. PMC 2268164. PMID 18268328.
119. Cristofari, Robin; Liu, Xiaoming; Bonadonna, Francesco; Cherel, Yves; Pistorius, Pierre; Maho, Yvon Le; Raybaud, Virginie; Stenseth, Nils Christian; Le Bohec, Céline; Trucchi, Emiliano (26 February 2018). "Climate-driven range shifts of the king penguin in a fragmented ecosystem". Nature Climate Change. 8 (3): 245–251. Bibcode:2018NatCC...8..245C. doi:10.1038/s41558-018-0084-2. S2CID 53793443.
120. "Antarctica's king penguins 'could disappear' by the end of the century". the Guardian. 26 February 2018. Retrieved 18 May 2022.
121. Jenouvrier, Stéphanie; Holland, Marika; Iles, David; Labrousse, Sara; Landrum, Laura; Garnier, Jimmy; Caswell, Hal; Weimerskirch, Henri; LaRue, Michelle; Ji, Rubao; Barbraud, Christophe (March 2020). "The Paris Agreement objectives will likely halt future declines of emperor penguins" (PDF). Global Change Biology. 26 (3): 1170–1184. Bibcode:2020GCBio..26.1170J. doi:10.1111/gcb.14864. PMID 31696584. S2CID 207964725.
122. "Penguins suffering from climate change, scientists say". The Guardian. 30 January 2014. Retrieved 30 January 2014.
123. ^ Fountain, Henry (29 January 2014). "For Already Vulnerable Penguins, Study Finds Climate Change Is Another Danger". The New York Times. Retrieved 30 January 2014.
124. Strycker, Noah; Wethington, Michael; Borowicz, Alex; Forrest, Steve; Witharana, Chandi; Hart, Tom; Lynch, Heather J. (10 November 2020). "A global population assessment of the Chinstrap penguin (Pygoscelis antarctica)". Scientific Reports. 10 (1): 19474. Bibcode:2020NatSR..1019474S. doi:10.1038/s41598-020-76479-3. PMC 7655846. PMID 33173126. S2CID 226304009.
125. Cimino MA, Lynch HJ, Saba VS, Oliver MJ (June 2016). "Projected asymmetric response of Adélie penguins to Antarctic climate change". Scientific Reports. 6: 28785. Bibcode:2016NatSR...628785C. doi:10.1038/srep28785. PMC 4926113. PMID 27352849.
126. Gray, Andrew; Krolikowski, Monika; Fretwell, Peter; Convey, Peter; Peck, Lloyd S.; Mendelova, Monika; Smith, Alison G.; Davey, Matthew P. (20 May 2020). "Remote sensing reveals Antarctic green snow algae as important terrestrial carbon sink". Nature Communications. 11 (1): 2527. Bibcode:2020NatCo..11.2527G. doi:10.1038/s41467-020-16018-w. PMC 7239900. PMID 32433543.
127. Olech, Maria; Słaby, Agnieszka (August 2016). "Changes in the lichen biota of the Lions Rump area, King George Island, Antarctica, over the last 20 years". Polar Biology. 39 (8): 1499–1503. Bibcode:2016PoBio..39.1499O. doi:10.1007/s00300-015-1863-0. ISSN 0722-4060. S2CID 16099068.
128. Robinson, Sharon A.; King, Diana H.; Bramley-Alves, Jessica; Waterman, Melinda J.; Ashcroft, Michael B.; Wasley, Jane; Turnbull, Johanna D.; Miller, Rebecca E.; Ryan-Colton, Ellen; Benny, Taylor; Mullany, Kathryn (October 2018). "Rapid change in East Antarctic terrestrial vegetation in response to regional drying". Nature Climate Change. 8 (10): 879–884. Bibcode:2018NatCC...8..879R. doi:10.1038/s41558-018-0280-0. ISSN 1758-678X. S2CID 92381608.
129. ^ Singh, Jaswant; Singh, Rudra P.; Khare, Rajni (December 2018). "Influence of climate change on Antarctic flora". Polar Science. 18: 94–101. Bibcode:2018PolSc..18...94S. doi:10.1016/j.polar.2018.05.006. S2CID 133659933.
130. Cavieres, Lohengrin A.; Sáez, Patricia; Sanhueza, Carolina; Sierra-Almeida, Angela; Rabert, Claudia; Corcuera, Luis J.; Alberdi, Miren; Bravo, León A. (March 2016). "Ecophysiological traits of Antarctic vascular plants: their importance in the responses to climate change". Plant Ecology. 217 (3): 343–358. Bibcode:2016PlEco.217..343C. doi:10.1007/s11258-016-0585-x. ISSN 1385-0237. S2CID 8030745.
131. IAATO Overview of Antarctic Tourism: 2018–19 Season and Preliminary Estimates for 2019–20 Season (Report). IAATO. 4 June 2019.
132. Liggett, Daniela; Frame, Bob; Gilbert, Neil; Morgan, Fraser (September 2017). "Is it all going south? Four future scenarios for Antarctica". Polar Record. 53 (5): 459–478. Bibcode:2017PoRec..53..459L. doi:10.1017/S0032247417000390.
133. "Impacts of tourism in Antarctica". www.iucn.org. Retrieved 1 December 2023.
134. "How to save Antarctica (and the rest of Earth too) | Imperial News | Imperial College London". Imperial News. 13 June 2018. Retrieved 1 December 2023.
135. "Polar Code". ww2.eagle.org. Retrieved 1 December 2023.
136. "Area Protection and Management / Monuments | Antarctic Treaty". www.ats.aq. Retrieved 27 April 2022.

• Climate change

v t e Antarctica
Geography	Antarctic sea ice Climate Climate change Heat waves Ice shelves Geology Glaciers Mountains Tundra Volcanoes Regions Biogeographic realm Antarctic Peninsula East Antarctica ice sheet shield Extreme points Floristic Kingdom Islands South Pole South magnetic pole West Antarctica ice sheet Bodies of Water Antarctic/Southern Ocean Lake CECs Lake Mercer Lake Vostok List of rivers McMurdo Sound Ross Sea Weddell Sea Life Flora Microorganisms Wildlife Birds Mammals Krill
History	Expeditions Heroic Age World War II Colonization COVID-19 pandemic Years
Politics	Council of Managers of National Antarctic Programs Military activity National programs Territorial claims Treaty System
Society	Antarctica Day Antarctic English Crime Demographics Economy Field camps Firefighting Flags Gateway cities Midwinter Day Protected areas Religion Research stations Telecommunications Time Tourism Transport Women
Famous explorers	Roald Amundsen Richard E. Byrd Douglas Mawson Ui-te-Rangiora (legendary) James Clark Ross Robert Falcon Scott Ernest Shackleton
Category Commons Index

• Environment of Antarctica
• Climate of Antarctica
• Climate change by continent
• Effects of climate change