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Antarctic ice sheets may have changed the planet's heartbeat
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Sam Wormley
Aug 24, 2012, 1:36:02 AM8/24/12
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Antarctic ice sheets may have changed the planet's heartbeat
> http://arstechnica.com/science/2012/08/antarctic-ice-sheets-may-have-changed-the-planets-heartbeat/
> You may have seen them before—the graphs from Antarctic ice cores showing the heartbeat of “ice ages” (or glaciations). If so, you probably noted a cyclical pattern, with each glaciation lasting about 100,000 years before being abruptly interrupted by a relatively brief warm period—the interglacial. Soon, the slow freeze inexorably gripped the planet again. There's a reason for this rhythmic pattern—cycles in Earth’s orbit that subtly alter the sunlight reaching the Earth.
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> But the graphs have long contained a couple head-scratching mysteries to climate scientists, though. First, why is the 100,000 year cycle dominant? There are several orbital cycles—some around 20,000 years long, another about 41,000 years long, and then the 100,000 year cycle. By itself, the 100,000 year cycle changes things the least, yet it drives the glacial heartbeat.
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kensi
Aug 24, 2012, 6:08:48 AM8/24/12
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On Aug 24, 12:36 am, Sam Wormley <sworml...@gmail.com> wrote:
> Antarctic ice sheets may have changed the planet's heartbeat
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> >http://arstechnica.com/science/2012/08/antarctic-ice-sheets-may-have-...
> Antarctic ice sheets may have changed the planet's heartbeat
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> > You may have seen them before—the graphs from Antarctic ice cores showing the heartbeat of “ice ages” (or glaciations). If so, you probably noted a cyclical pattern, with each glaciation lasting about 100,000 years before being abruptly interrupted by a relatively brief warm period—the interglacial. Soon, the slow freeze inexorably gripped the planet again. There's a reason for this rhythmic pattern—cycles in Earth’s orbit that subtly alter the sunlight reaching the Earth.
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> > But the graphs have long contained a couple head-scratching mysteries to climate scientists, though. First, why is the 100,000 year cycle dominant? There are several orbital cycles—some around 20,000 years long, another about 41,000 years long, and then the 100,000 year cycle. By itself, the 100,000 year cycle changes things the least, yet it drives the glacial heartbeat.
Bullshit.
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> > But the graphs have long contained a couple head-scratching mysteries to climate scientists, though. First, why is the 100,000 year cycle dominant? There are several orbital cycles—some around 20,000 years long, another about 41,000 years long, and then the 100,000 year cycle. By itself, the 100,000 year cycle changes things the least, yet it drives the glacial heartbeat.
Wally W.
Aug 25, 2012, 2:22:57 PM8/25/12
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On Fri, 24 Aug 2012 00:36:02 -0500, Sam Wormley wrote:
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>Antarctic ice sheets may have changed the planet's heartbeat
Or they may not have.
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>Antarctic ice sheets may have changed the planet's heartbeat
Sam Wormley
Aug 25, 2012, 6:00:40 PM8/25/12
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bja...@iwaynet.net
Aug 26, 2012, 1:36:19 AM8/26/12
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