The area on the topic of the discussion is where the labrador current meets the gulf stream.
This is or can be caused by atlantic thermohaline circulation.
As for example. The gulf stream will form A warm core eddy from winds and upwelling.
This eddy will blow into the continental shelf. As the breeze passes by this warm core
eddy. You will now feel pockets of warm air pass by.
We have placed cookies on your device to help make this website better. You can adjust your cookie settings, otherwise we'll assume you're okay to continue.