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Bergs wins Eastbourne final to clinch first ATP title
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Ravindra and Mitchell strengthen New Zealand's grip on England decider
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BIS warns 'pressure points' putting global economy at risk
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Ntamack aims to bring Toulouse Top 14 win 'energy' to Nations Championship campaign
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Cycling industry bets on smart bikes to boost sales
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'High-strung' camels race in Australian outback
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In Idaho, the next generation of US nuclear reactors nears reality
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Algeria and Austria reach World Cup knockouts after 3-3 thriller
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Africa the winner of expanded World Cup amid mixed fortunes for minnows
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DR Congo advance but Iran out as wild World Cup group stage wraps
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Asia's vendors grapple with rising costs of ever-present plastics
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Austria and Algeria reach World Cup knockouts after 3-3 thriller
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Messi scores again as Argentina head into World Cup last 32 on a high
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Where are they? Dogs disappear before South Korea meat ban
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Wissa proud to deliver World Cup joy to war-torn DR Congo
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China's bull wrestlers fight to keep tradition alive
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South Korea's 'dismal' World Cup ends in group phase
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England top group to set up DR Congo World Cup clash, Portugal held
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Colombia and Portugal through to World Cup last 32 after thrilling draw
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England moving on at World Cup but questions linger
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Wissa sends DR Congo into World Cup last 32 clash with England
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Venezuela quakes kill 1,400 as time running out to find survivors
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A painful wait by a pile of rubble in quake-hit Venezuela
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Australia World Cup goalkeeper Patrick Beach has beach named after him
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Tuchel delighted to have Bellingham in 'sweet spot' for England at World Cup
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Bellingham says 'job done' but England must improve at World Cup
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Australia boosts shark-spotting drone coverage at Sydney beaches
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Scotland boss Clarke resigns after World Cup exit confirmed: official
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Kane, Bellingham on target as England clinch top spot
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Croatia battle past Ghana to sew up World Cup Last 32 spot
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Bellingham, Kane score as England beat Panama to reach World Cup last 32
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Canada's Davies 'available' for historic knockout clash
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Ryu takes one-shot lead over Henderson at Women's PGA Championship
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Hovland seizes one-shot PGA Travelers lead over Scheffler
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Jangoo and Chase put West Indies in control against Sri Lanka
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Mauvaka double inspires Toulouse to fourth-straight Top 14 in storm-impacted final
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World Cup star Gakpo requests privacy after death of unborn son
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Solidarity, sadness among Venezuelans made destitute by quake
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Aid planes landing at partially reopened Venezuela airport after quakes
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Spain's Williams hits out at Uruguay over World Cup injury
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'We need help': Venezuelans furious at slow official response to quakes
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World's largest particle smasher halts for upgrade to boost hunt for dark matter
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Venus Williams relishes 'very special' Wimbledon reunion with sister Serena
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Ex-Olympic medallist Canderloro elected French Ice Sports chief
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Ravindra leads New Zealand rally in England finale after Archer's double strike
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Prince Harry and family to stay at royal residences on UK visit
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Wimbledon 'towel thief' Swiatek back on the trophy hunt
Study reveals how Earth's orbit controls ice ages
The Earth's next ice age is expected to begin in about 11,000 years -- unless human-caused global warming disrupts natural cycles.
That's according to a new study published Thursday in Science, which analyzed how subtle shifts in Earth's orbit around the Sun have historically triggered massive climate changes.
A research team examined a million-year record of climate change, focusing on land-based ice sheets across the Northern Hemisphere and deep ocean temperatures.
They then paired this data with small but cyclical variations in Earth's orbital patterns.
"For many years, the difficulty in answering how small changes in Earth's orbit around the Sun translate to large shifts between glacial and interglacial states has been a central theme in paleoclimate research," lead author Stephen Barker, a professor at Cardiff University, told AFP.
Earth has long alternated between ice ages and warmer interglacial periods, with the last glaciation ending approximately 11,700 years ago. This transition marked the beginning of the Holocene epoch, an era of relative climate stability that enabled early human societies to shift from nomadic hunting and gathering to settled agriculture.
Scientists have long recognized a connection between Earth's orbit and ice ages. However, due to challenges in accurately dating climate changes that occurred so far in the past, they struggled to pinpoint which orbital parameters were responsible for starting and ending these glacial cycles.
According to Barker, the key breakthrough came from analyzing the "shape" of the ancient climate record -- the curves showing how temperatures rose and fell over time -- rather than just the timing of ice age transitions.
This approach allowed the team to determine how the three orbital factors -- tilt, wobble, and the shape of Earth's orbit around the Sun -- interact to drive ice age cycles over the past 900,000 years.
Barker said that without the Industrial Revolution, assuming fossil fuels had never been burned, "we would expect a glaciation to occur within the next 11,000 years, and it would end in 66,000 years' time."
Co-author Lorraine Lisiecki, a professor at the University of California, Santa Barbara, emphasized the significance of the study, stating that it "confirms the natural climate change cycles we observe on Earth over tens of thousands of years are largely predictable and not random or chaotic."
However, Barker strongly cautioned against interpreting the findings to suggest that human-caused climate change is beneficial.
Carbon dioxide levels have nearly doubled since the Industrial Revolution, and if emissions remain unchecked, "then in around 8,000 years' time, Antarctica would have melted, leading to around 70 meters of sea-level rise," said Barker.
"Instead of there being glaciers, you'll be underwater," he warned.
Looking ahead, the research team aims to expand on their findings by investigating the long-term impact of human-driven climate change and how it may reshape the planet's natural climate cycles.
V.Dantas--PC