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If you were born in the most recent ice age, how different would your life be compared to how you live it today? Furthermore, if humans currently lived in an ice age, how would it affect life today?

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    $\begingroup$ people had moved closer to equator,and the changes had probably been a lot less than you might think.the water level in the oceans had been lower creating more dry land close to equator. $\endgroup$ – trond hansen Jan 24 '18 at 18:49
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    $\begingroup$ Technically we live in an ice age right now, an ice age is just defined as a time period when a significant portion of the earth's surface is covered in ice year round, thanks to Greenland and Antarctica the current earth easily qualifies. You might want to look into the terms glacial and inter-glacial periods, they may get you closer to what I think you want to ask. $\endgroup$ – John Jan 31 '18 at 21:52
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It depends where, the continental landmasses at higher latitudes would be covered by massive ice sheets. Therefore the life in the sections of the US and Europe that are close to the Ice sheets would have conditions similar to what is life in Greenland today. The map would look like this: enter image description here

(Image taken from planetaryvisions.com)

And the summers would be more mellow than what you are used to. Mean global temperatures would be much lower but at tropical latitudes there would still be warm weather. That means that the temperature gradient between the equator and the poles would be larger, leading to quicker climatic transitions as you travel North or South, and also leading to stronger winds and probably more powerful storms.

Also the sea level would be about 120 meters lower than today, exposing many areas that are now underwater, some of them massive, like the Sunda land bridge (see map in the Indonesia area), many islands would be connected to the continents, like Tasmania to Australia and Sirilanka to India. England would be connected to Europe and the Persian gulf would be dry, as well as the Yellow sea. New Zealand would be just one big island, and hundreds of islands that are now underwater would poke the oceans. Using ETOPO1 I've put together a fairly high resolution image of the world showing all the land that would be exposed if the sea level today drops 120m (as it did on the last ice age). You can see it here.

Furthermore, the Pacific and the Atlantic would be completely isolated from each other for navigation proposes, as the Magellan strait and Drake passage would be blocked by ice and the Panama canal would be a nearly impossible feat, with the sea level ~120 m lower than today. So probably, train transport would be much more important to carry goods across the Americas.

The Suez cannal would not exist either, and navigation around the Good hope cape at the southern tip of Africa would be constantly threatened and perhaps blocked by icebers, so most transport between the Indian and Atlantic ocean would be by land too.

The sea ice would be in contact with the tropical gyros, meaning that massive floating ice islands would be seen even at the ecuador, and icebergs would be all around the oceans.

All that would mean that all the empires that rose from naval power (England, Portugal, Spain) would might not existed, then, maybe Asian powers would rule the world undisputed, and the colonization/invasion of many territories would have never happen or at least would have been delayed, leading to a completely different world distribution and organization.

Another interesting change, would be the scarcity of shallow seas compared to today. The drop in total surface area for a given elevation below current sea level becomes stepper once the sea level drops more than 60 m. Therefore, the sea depth would increase quicker as you go seaward from an "ice age seashore". This would lead also to a drop in coastal water productivity (oposite to what is believed to have happened in the Cretaceous, with high sea level and abundant shallow seas).

Also the day would be about one and a half minutes longer, meaning that the year would have only 364 days.

The change in day length would lead to calendar changes. Currently, a year have 365.2422 days, that is approximated in our calendar to 365.2425, with the fraction part divided as

0.2425 = 0.25-0.01+0.0025

  • The +0.25 is compensated by adding one day every four years, that is a leap year
  • The -0.01 is compensated by skipping one leap year every 100 years
  • And the +0.0025 is compensated by not skipping one leap year every 400 years.

That's how our calendar works today.

Now, if we assume that the figure of a day 1.5 minutes longer is precise, one year would have 364.8621 days, and the fractional part would probably be approximated to 0.8620, and perhaps divided as

0.8620 = 0.80 + 0.05 +0.02 -0.0080

So the calendar rule would perhaps be like

  • +0.80 compensated by adding one day every year except every 5 years
  • +0.05 compensated by skipping the above rule exception every 20 years and add a day anyways
  • +0.02 compensated by skipping the exception to the first rule once more every 50 years.
  • -0.0080 compensated by not adding an extra day every 125 years

Or something like that, many other arrangements could be imagined. But at the end, a typical year would still have 365 days, but the lap years would have one day less instead of one extra day.

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    $\begingroup$ What is the source for the map? $\endgroup$ – arkaia Jan 24 '18 at 21:20
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    $\begingroup$ @arkaia planetaryvisions.com/Project.php?pid=2226 I choose it because is nice, but there is many other maps from more reliable sources showing basically the same features. $\endgroup$ – Camilo Rada Jan 24 '18 at 21:25
  • $\begingroup$ What about leap years? $\endgroup$ – Eevee Jan 29 '18 at 19:09
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    $\begingroup$ @Imtherealsanic given your interest in the lap year detail I've added few paragraphs at the end of the answer about that. $\endgroup$ – Camilo Rada Jan 30 '18 at 16:46
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    $\begingroup$ @JeopardyTempest True, I think that's because that area would be too dry, so, despite of the cold there would be not enough accumulation to build ice sheets. $\endgroup$ – Camilo Rada Feb 17 '18 at 5:24

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