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Then things changed. Since 2015, Antarctic sea ice<\/a> has dropped sharply. By 2023, it reached the lowest level ever recorded. <\/p>\n A new study explains why. The answer is not one single cause. It is a chain of events that built up over time.<\/p>\n A sudden drop in sea ice<\/p>\n For years, Antarctic sea ice behaved differently from Arctic ice. While Arctic ice shrank, Antarctic ice<\/a> slightly increased between 1979 and 2015.<\/p>\n Then the trend flipped. Ice began to shrink and did not recover. The loss kept growing each year.<\/p>\n \u201cAntarctic sea ice in the Southern Ocean helps drive the planet\u2019s ocean<\/a> overturning circulation,\u201d explains Dr. Aditya Narayanan, lead author of the study. <\/p>\n \u201cHowever, since 2015, the region has undergone a huge transformation, with extreme ice loss around the continent.\u201d<\/p>\n Winds start the process<\/p>\n The story begins with strong winds around Antarctica. These winds have grown stronger over the past few decades.<\/p>\n Stronger winds do more than move surface water. They pull water up from deeper layers<\/a>. This process slowly brings warm water closer to the surface.<\/p>\n The deep ocean holds warm and salty water. This water stores heat collected over long periods.<\/p>\n For years, this warm water stayed below the surface. But stronger winds pushed it upward bit by bit.<\/p>\n The surface still looked cold. Ice could still form. But hidden heat was building below.<\/p>\n When everything changed <\/p>\n Around 2015, everything changed. A burst of strong winds caused deep mixing in the ocean. Warm water broke through to the surface layer.<\/p>\n This warmed the upper ocean. It also made the water saltier.<\/p>\n Sea ice needs cold water to form. Once the surface warmed, ice started to melt and stopped forming as easily.<\/p>\n \u201cWhat started as a slow build-up of deep-sea heat under the Antarctic sea ice was followed by a violent mixing of water, ending in a vicious cycle where it\u2019s too warm to let ice recover,\u201d Dr. Narayanan said.<\/p>\n The role of warmer temperatures <\/p>\n In East Antarctica, the main cause came from the ocean.<\/p>\n Warm water rose from below and melted ice. As ice disappeared, more sunlight reached the ocean. The water absorbed this heat, which caused more melting.<\/p>\n This created a loop. Less ice led to more heat. More heat led to even less ice.<\/p>\n In West Antarctica, the atmosphere played a bigger role. Warm and moist air moved toward the region in certain years. This brought more clouds.<\/p>\n Clouds trap heat. In polar regions, this trapped heat can warm the surface more than sunlight would.<\/p>\n So here, the ice melted from above instead of below.<\/p>\n Ice loss feeds itself<\/p>\n After 2018, the system entered a new phase.<\/p>\n Normally, sea ice forms near Antarctica and moves outward. When it melts, it adds fresh water to the ocean surface. This fresh water helps keep the surface stable.<\/p>\n But with less ice forming, less fresh water entered the ocean.<\/p>\n The surface became saltier. Saltier water mixes more easily with deeper water. This allowed more warm water to rise.<\/p>\n This created another loop. Ice loss made it easier for more heat to reach the surface.<\/p>\n The change did not happen overnight.<\/p>\n Winds have been getting stronger since the 1980s. Warm water has been moving upward for years.<\/p>\n By 2015, the system reached a tipping point.<\/p>\n A possible new normal<\/p>\n Scientists now wonder if this change will last.<\/p>\n Some signs suggest the system has shifted. Ice now shows stronger year to year patterns. It may also be thinner.<\/p>\n If current wind patterns continue, warm water will keep rising. The cycles that prevent ice from recovering will remain.<\/p>\n \u201cIf the low sea-ice coverage prevails into 2030 and beyond, the ocean may transition from a stabilizer of the world\u2019s climate to a powerful new driver of global warming,\u201d said Professor Alberto Naveira Garabato from the University of Southampton<\/a>.<\/p>\n Why it matters<\/p>\n Antarctic sea ice is important for the whole planet. It reflects sunlight and helps keep Earth cool. When ice shrinks, the ocean absorbs more heat.<\/p>\n Sea ice also helps store carbon in the ocean. Less ice weakens this process.<\/p>\n \u201cThis isn\u2019t just a regional problem, Antarctic sea ice acts as Earth\u2019s mirror, reflecting solar radiation back into space,\u201d said study co-author Dr. Alessandro Silvano.<\/p>\n \u201cIts loss could destabilize the currents that store heat and carbon in the ocean, accelerating global warming, and also destabilize ice shelves that prevent glaciers from sliding into the sea, raising global sea levels.\u201d<\/p>\n Effects on marine life<\/p>\n Sea ice acts like the base of a food system.<\/p>\n Algae grow under the ice. Krill eat this algae and use the ice for shelter. Many animals depend on krill, including penguins, seals, and whales.<\/p>\n When sea ice shrinks, less algae grows. Krill get less food, so their numbers can drop. This affects all the animals that rely on them.<\/p>\n Ultimately, a change in sea ice spreads through the entire food chain.<\/p>\n A clear warning<\/p>\n The record low in 2023 is not just a one time event. It shows a deeper shift.<\/p>\n \u201cIt\u2019s concerning because massive loss of sea ice destabilizes the world\u2019s ocean current systems, warming our planet far quicker than expected,\u201d Dr. Narayanan adds.<\/p>\n What happens near Antarctica affects the entire planet. Understanding this change helps us prepare for what comes next.<\/p>\n The study is published in the journal Science Advances<\/a>.<\/p>\n \u2014\u2013<\/p>\n Like what you read? Subscribe to our newsletter<\/a> for engaging articles, exclusive content, and the latest updates.<\/p>\n Check us out on EarthSnap<\/a>, a free app brought to you by Eric Ralls<\/a> and Earth.com.<\/p>\n \u2014\u2013<\/p>\n","protected":false},"excerpt":{"rendered":"The edge of Antarctica once felt steady and predictable. Each winter, sea ice spread across the ocean. 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