Mawsynram
Mawsynram is a town in the East [Khasi Hills district] of Meghalaya state in Northeastern India, from Shillong, the state capital. Mawsynram receives the highest rainfall in India. It is reportedly the wettest place on Earth, with an average annual rainfall of. According to the Guinness Book of World Records, Mawsynram received of rainfall in 1985.
Mawsynram received of rainfall on 19 August 2015. On 17 June 2022, Mawsynram set a new record by receiving in a span of 24 hours which has now become its highest single day record for the month of June and for its all-time single day record, beating its former record of on 7 June 1966.
Location
Mawsynram is located at 25° 18′ N, 91° 35′ E, at an altitude of about 1,400 meters, 15 km west of Cherrapunji, in the Khasi Hills in the state of Meghalaya.Climate and rainfall
Under the Köppen climate classification, Mawsynram features a subtropical highland climate with an extraordinarily showery, rainy and long monsoonal season and a short dry season. Based on the data of a recent few decades, it appears to be the wettest place in the world, or the place with the highest average annual rainfall. Mawsynram receives over of rain in an average year, and the vast majority of the rain it gets falls during the monsoon months. A comparison of rainfalls for Cherrapunji and Mawsynram for some years is given in Table 1.Mawsynram receives the highest rainfall in India. Although it is reportedly the wettest place on Earth, with an average annual rainfall of, this claim is disputed by Lloró, Colombia, which reported an average yearly rainfall of between 1952 and 1989 and López de Micay, also in Colombia, which reported per year between 1960 and 2012. According to the records observed by the Indian Meteorological Department, it was seen that while its neighbour, Cherrapunji is having a significant decreasing trend in rainfall, Mawsynram on the other hand is experiencing a slight increase in its rainfall pattern which put its average annual rainfall from 1950 to 2000 at and from 2000 to 2020 at. The precipitation table below shows the average monthly record from 1950 to 2000.
Primarily due to the high altitude, it seldom gets truly hot in Mawsynram. Average monthly temperatures range from around in January to just above in August. The village also experiences a brief but noticeably drier season from December until February, when monthly precipitation on average does not exceed. The little precipitation during the village's "low sun" season is something that is shared by many areas with this type of climate.
The following table is a comparison of rainfalls for Cherrapunji and Mawsynram between 1970 and 2010.
| Year | Cherrapunji Rainfall | Mawsynram Rainfall |
| 2010 | 13 472 | 14 234 |
| 2009 | 9 070 | 12 459 |
| 2008 | 11 415 | 12 670 |
| 2007 | 12 647 | 13 302 |
| 2006 | 8 734 | 8 082 |
| 2005 | 9 758 | 10 072 |
| 2004 | 14 791 | 14 026 |
| 2003 | 10 499 | 11 767 |
| 2002 | 12 262 | 11 118 |
| 2001 | 9 071 | 10 765 |
| 2000 | 11 221 | 13 561 |
| 1999 | 12 503 | 13 445 |
| 1998 | 14 536 | 16 720 |
| 1997 | 8 993 | 9 892 |
| 1996 | 12 989 | 12 850 |
| 1995 | 14 189 | 13 832 |
| 1994 | 11 194 | 10 940 |
| 1993 | 12 807 | 13 848 |
| 1992 | 8 537 | 10 450 |
| 1991 | 13 494 | 16 112 |
| 1990 | 11 598 | 12 934 |
| 1989 | 13 432 | 8 828 |
| 1988 | 17 948 | 16 750 |
| 1987 | 13 153 | NA |
| 1986 | 8 140 | NA |
| 1985 | 11 816 | 26 000 |
| 1984 | 16 761 | 25 613 |
| 1983 | 9 773 | 12 163 |
| 1982 | 10 468 | 9 246 |
| 1981 | 9 113 | 9 739 |
| 1980 | 9 133 | 9 739 |
| 1979 | 12 095 | NA |
| 1978 | 6 950 | NA |
| 1977 | 11 689 | 11 986 |
| 1976 | 11 012 | 6 134 |
| 1975 | 11 976 | 10 639 |
| 1974 | 24 554 | NA |
| 1973 | 10 911 | NA |
| 1972 | 11 095 | NA |
| 1971 | 16 915 | NA |
| 1970 | 15 318 | NA |
Source:
Three reasons can be cited for high rainfall at Mawsynram:
- The warm moist winds of the northward-moving air from the Bay of Bengal during the monsoon, which cover an extensive area but are forced to converge into the narrower zone over the Khasi Hills, thus concentrating their moisture.
- The alignment of the Khasi Hills places them directly in the path of the airflow from the Bay of Bengal, producing a significant uplift.
- Finally, 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 more or less continuous.