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[–] 8 points 1 day ago* (14 children)

The mainland US is crazily far south. I thought Washington would be level with London

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  • [–] 19 points 1 day ago (6 children)

    I have always felt the opposite. Europe is way further north than I would have expected given their climate. I realize now it is kept warm by the gulf steam and North America get that in reverse, hence really cold eastern Canada and New England.

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  • [–] 4 points 1 day ago* (5 children)

    No reverse. New England and eastern Canada are warmed by the same currents too, albeit not as much. The heat generally comes from the Caribbean. North Korea and Hokkaido have far colder winters and milder summers at similar latitude.

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  • [–] 3 points 1 day ago (4 children)

    I believe you actually have it backwards. Europe is warmed by the gulf steam, it cools off on the way back to Canada and the US. If the Gulf Steam is disrupted as predicted, the UK is going to be in for a really cold time.

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  • [–] 3 points 1 day ago (3 children)

    the cold water returning to the tropics flows deep under the warmer surface waters and has much less effect on land temperatures.

    https://yaleclimateconnections.org/2024/12/atlantic-circulation-collapse-new-clues-on-the-fate-of-a-crucial-conveyor-belt/

    this is where i got the claim from, that NE USA and E Canada would also cool down with no AMOC. (the sea-level rise in that region would be an even bigger problem though)

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  • [–] 1 point 20 hours ago (2 children)

    I think you may be misreading the map from that link a bit because it is fairly low detail and doesn't point out the landmarks very well. The "gyre" as it is referred to in the linked page doesn't really reach the northeast US much at all, it mostly stops at around the area between NC and VA where the coast protrudes. If you want to see a cool image based on satellite data that shows it off, check this out (https://www.earthdata.nasa.gov/news/worldview-image-archive/gulf-stream). That being said, some of that warm water does still affect a the NE US a bit (not so much for Canada), so the gulf stream faltering will make it colder, just not as dramatically as places like the UK which based on latitude would likely have temperatures closer to Sweden and Norway.

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  • [–] 3 points 19 hours ago (1 child)

    Your comment six hours ago had a claim that eastern Canada and New England were cooled by the amoc. I think that was the only thing the other poster was going against. Your recent comment now agrees that eastern Canada and New England would be colder without the amoc.

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  • [–] 1 point 3 hours ago

    It wasn't clear at all that was all that other commenter disagreed with. Also Eastern Canada and New Edgland are cooled by it. It isn't as much of an effect because the cold water sink, but it most certainly affects it.

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  • [–] 7 points 1 day ago* (last edited 1 day ago) (3 children)

    Well, and it's crazy how cold the middle and eastern parts of North America get.

    Boston and Chicago are famously cold cities. Chicago is exactly parallel with Rome; Boston is only 50km north of Rome. Rome, Barcelona, even Tblisi - all about 10+ degrees C (so 20 degrees F) more mild in the winter than Chicago. The entirety of continental France, including its southern coast, is north of Boston. Paris is almost far enough north to be exactly at the long E-W US/Canada border. Yet rarely gets below freezing.

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  • [–] 4 points 1 day ago (1 child)

    The entirety of France, including its southern coast, is north of Boston.

    Acktyually, the southernmost point in France is 50°01′ South (Îles de Boynes in the southern Indian Ocean). 🤓

    Somewhat more legitimately, there are also inhabited French lands further south than Boston: Corsica, French Guiana, French Polynesia, Réunion, etc. Corsica even counts as "Metropolitan France" (as opposed to "Overseas France") while still -- barely -- beating Boston by about 1°.

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  • [–] 5 points 1 day ago (2 children)

    Latitude is crazy. London would sit in the Hudson Bay, and Atlanta is a similar latitude to Casablanca or Baghdad.

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