Cold Blow is a name for a deserted farmstead located in Temple Ewell Civil Parish in Kent. The first element cold concerns “coldness” or “chilliness,” and the second element blow concerns “strong wind.” This paper aims to investigate the “wind strength” which is supposed to be meant by the second element of the place-name in question by analyzing the meteorological data obtained from the local weather forecast. Since Cold Blow is isolated on a rather inland hilltop, Folkestone was selected for the purpose of pursuing a contrastive comparison, because the city is situated on the coastal level plain in the vicinity. Consequently, it has been revealed that, in the summer season, the “wind strength” at Cold Blow is weaker than that at Folkestone, and that the directions of the prevalent winds and those of the stronger winds are fairly correlated at Folkestone but only partially at Cold Blow, despite the fact that the northeasterly and the southwesterly winds are prevalent at both places.