This is the second installment of impressive weather records. Last time I covered temperature and this time it is the turn of our old foe: rain. I hate rain. It’s my least favourite type of weather and I don’t think I’m alone in that. It often feels like England is the rainiest country in the world, but of course it isn’t. We just complain about it the most.
Here are some of the most impressive rain records that planet earth has to offer.
Barot, Guadeloupe – 26th November 1970
I couldn’t find much else out about Barot, Guadeloupe, other than the fact that they had this record breaking deluge. They received 3.8 cm (1.5 in) of rain in just a single minute.
Guadeloupe is generally a pretty wet country, in September they normally get about 9 cm over the 30 day period. So to receive well over a week’s worth of rain in just a single 60 second period is pretty impressive.
Holt, Missouri – 22nd June 1947
Holt has the distinction of holding the world record for the fastest accumulation of rainfall in one hour. On June 22, 1947, they took 12 inches (300 mm) of rain in just 42 minutes. BOOM.
According to their Wikipedia page, there is literally nothing else of interest going on in Holt. It has a population of around 450 people. The end.
Foc-Foc, Réunion – 8 January 1966
Foc-Foc, Réunion – 7/8 January 1966
Back in Reunion – 1,825 mm (71.9 in). Nearly 2 metres! That’s almost double the UK’s yearly precipitation budget.
Cherrapunji, Meghalaya, India – 15/16 June 1995
In June 1995 they managed to welcome in 2,493 mm (98.1 in) in just 2 days.
Mawsynram, Meghalaya, India
Damp doesn’t even touch the sides. This place is sopping. On average they get 11,872 mm (467.4 in) per year. The poor gits. In 1998 they had a mega 16,720 mm in total.
Why’s it so wet? Well, its position in the Khasi Hills (pictured above) is at the route of the problem:
1. The warm moist winds drifting in from the Bay of Bengal during the monsoon are forced to converge into the narrower zone over the Khasi Hills, thus concentrating their moisture.
2. The Khasi Hills run east to west placing them directly in the path of the airflow from the Bay of Bengal, producing a significant uplift (plus cooling, further condensation and thus more rain).
3. Uplift over the Khasi Hills is virtually continuous in the monsoon period because the lifted air is constantly being pulled up by vigorous winds in the upper atmosphere, hence the rainfall is pretty much constant.
It sounds rubbish there doesn’t it? So next time you’re trapped in a shower thank your lucky stars you don’t live anywhere listed above.
Quit your whining.
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