Very basically, see that high over Scandinavia, with the H (= "hoch"/high, it's in German)? Now imagine that expanding, particularly westwards. The low over the UK, with the T (= "tief"/deep, i.e. low), would be forced beneath it (or "undercut" it in the jargon on here).
Now picture that scenario and follow the resulting isobars (the lines around the T), bearing in mind the direction of wind is anti-clockwise around areas of low pressure. You'd find the consequent airflow would be coming off cool land to the east rather than mild water to the west.
The other noteworthy point is that the high over Scandinavia is coloured green and yellow, indicating warmth and consequently strength in the high. What coldies are looking for is warm air advection (WAA) northwards to promote areas of high pressure to our north (so-called northern blocking). This forces the areas of low pressure southwards and, if everything falls in the right places, a visit from colder Arctic of Continental air rather than mild sea air.
It really is that simple.
Originally Posted by: some faraway beach