Talk:Cold-core low

Upper-level low?
Is this the same as an upper-level low? If so that should be mentioned. --♫ Hurricanehink ( talk ) 18:49, 16 February 2011 (UTC)
 * It's mentioned a couple times that cold-core lows strengthen with height, but not explicitly since they can have a related low level circulation. You think it should be made more obvious?  Is there a way it could be worded more clearly without being incorrect?  Thegreatdr (talk) 23:39, 16 February 2011 (UTC)
 * Oh, just that you see all the time references to upper-level lows. If ULL and cold-core low are one in the same, that would be great, as I'm often looking for a place to link for that. ♫ Hurricanehink ( talk ) 00:33, 17 February 2011 (UTC)

I still think there should be a mention in the lede that the "upper-level lows" so often read about in tropical cyclone literature refer to this. ♫ Hurricanehink ( talk ) 19:10, 30 June 2011 (UTC)

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Do all high level lows have a cold core
Equating upper-level low with cold-core low seems to imply all high level lows have a cold core. Could we clarify if this is true, and why ? What causes them to form ? eg is it just a high level eddy that coincidentally contains colder air, or does the cold core cause the formation/rotation, or does the rotation cool the core ? - Rod57 (talk) 13:14, 5 November 2017 (UTC)