LONDON, ENGLAND
1952
T
he most unusual fact about the London Fog of 1952 was not that some four thousand people died from it-one of the largest num bers of people killed by any environmental disaster-but that no one seemed to recognize that it was happening. For four days the fog was so thick that traveling throughout the city was almost impossible, but few realized just how deadly it was. After all, London had been notorious for its fog for a long time-romantic notions were even attached to it. For the residents of London the fog was a frequent, if unwelcome, guest. In 1952 Londoners were relying heavily on soft, bituminous coal for
- fuel. The soft coal was cheap, in part because of the low cost of shipping
it by sea from Newcastle, but it had a higher sulfur and nitrogen oxide content than the harder anthracite coal used in Wales and Scotland. The smoke it emitted was tarry and full of hydrocarbons. When carbon particles of soot from coal-fire emissions combine with particles of water, fog becomes smog. The soot and water combination is not transparent to light, and as the fog thickens, light is prevented from penetrating the foggy air. No only does this cause limited visibility, but a breath of this air carries with it carbon particles and other dangerous substances. Certain weather conditions, particularly temperature inversions, aggra vate fog. Usually the air near the ground is warmer than the air higher up, and the warm air rises and mixes with the cooler air. Occasionally this relationship is inverted with the colder air remaining close to the ground
Reference: Hernan, R.E. (2010). This Borrowed Earth