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Surface Levels.
The BBC leaves a lot to be desired when it comes to making use of the North Atlantic plots. The reason is that they ignore most of the Atlantic and concentrate only on the after effects of the systems portrayed on decent weather maps. To get the most out of a North Atlantic map, you need to consider the coming (real time US/Canadian) mesoscales and the situation extant on the west coast from Florida up to Greenland, as this is the deciding factor in most coastal European synopsis. The present dead-head regime in the BBC insists that technical stuff be left out of all presentations. And nowadays, apart from local regional forecasts (and not all of them too neither) it is uncommon to see the North Atlantic map. Well that's enough about the BBC. They can rot in hell as far as I am concerned. I can forget the good old days now I realise how not so good they might have been. The weather in the USA varies according to the tenets laid down by Weatherlawyer in work stated elsewhere. So I won't go into that yet. Just restate the obvious that generally the weather they get is like ours for the same reasons. It comes in from southern climes and crosses diagonally to the Canadian border where at Newfoundland it joins the Atlantic stream called the North Atlantic Drift. Sometimes (and erroneously called the Gulf Stream.) The drift is the result of tropical heating forcing brine the same way that it forces the atmosphere. In the ocean this is called the Thermo-Haline Column in the atmosphere it is called The Weather. As a mass is heated it builds up pressure. When contained -as in the top layer of the ocean or the bottom layer of the atmosphere it expands according to the laws of thermodynamics. And with the air this lifts the lid called The Tropopause. And takes with it a section from the thermo-haline column that can not escape any other way, water being infinitely less responsive to thermodynamics than air. Air from warm water surfaces, filling with moisture, rises to the top of the air column -because water laden air is much lighter than dry air. Complex, but relatively unimportant. |
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