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Ice Ages

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Mars Shapes Earth's Ice-Age Rhythm, New Simulations Show
science26 days ago

Mars Shapes Earth's Ice-Age Rhythm, New Simulations Show

UC Riverside planetary astrophysicist Stephen Kane’s simulations show Mars exerts a measurable influence on Earth’s orbital variations and tilt, helping to drive Milankovitch cycles that govern ice-age timing. Removing Mars erases two long cycles (about 100,000 and 2.3 million years), while increasing Mars’ mass shortens them, suggesting outer planets can affect climates on Earth-like worlds.

Mars’s gravity may pace Earth’s ice-age clock
science1 month ago

Mars’s gravity may pace Earth’s ice-age clock

New simulations show Mars helps set a 2.4-million-year rhythm in Earth’s orbit that paces Milankovitch cycles and influences ice-age timing. By running the solar system with and without Mars, researchers found the red planet’s gravity shapes orbital frequencies and Earth’s tilt; removing Mars erased a key cycle, tying these climate rhythms to planetary dynamics. While greenhouse gases and ocean circulation remain primary drivers of temperature swings, the study connects orbital science to rock records and suggests broader implications for understanding climates on other worlds.

Mars’ Gravity May Have Shaped Earth's Ice Ages and Evolution
science2 months ago

Mars’ Gravity May Have Shaped Earth's Ice Ages and Evolution

New simulations suggest Mars’ gravity subtly steers Earth’s orbit and tilt, influencing Milankovitch climate cycles that drive Ice Ages. When Mars is removed from the model, 100,000-year and 2.3-million-year cycles disappear; increasing Mars’ mass shortens these cycles and stabilizes Earth’s tilt. The findings imply Earth’s climate—and potentially its evolution—could have been very different without Mars, with broader implications for studying exoplanet climates.

Potential Climate Feedbacks That Could Trigger a New Ice Age
science5 months ago

Potential Climate Feedbacks That Could Trigger a New Ice Age

A new study uncovers a feedback mechanism in Earth's carbon cycle that could cause global warming to overshoot and trigger an ice age, suggesting Earth's climate system can overreact and potentially plunge the planet into deep freeze, especially under past conditions of low atmospheric oxygen. However, current higher oxygen levels may dampen this effect, but the risk remains if warming continues. The findings highlight the importance of limiting ongoing climate change.