Fuvahmulah Monthly Rainfall & Precipitation
This page shows both the average monthly rainfall and the number of rainy days in Fuvahmulah, Gnaviyani Atoll, Maldives. Long-term data from 1990 to 2020 was used to calculate these averages. Now, let's break down all the details for a clearer picture.
Fuvahmulah experiences significant rainfall throughout the year, averaging 1854 mm (73 in) of precipitation annually. However, this abundant rainfall is not evenly distributed, with a distinct rainy season during certain months. You can clearly see this in our monthly precipitation graphs below.
Monthly Precipitation Levels
The average number of days each month with precipitation (> 0.2 mm (0.01 in))
Fuvahmulah can be quite wet during November, receiving approximately 213 mm (8.4 in) of precipitation over 13 rainy days.
In contrast February, experiences much drier conditions, with 81 mm (3.2 in) of rainfall, spread across 7 rainy days.
November, the wettest month, has a maximum daytime temperature of 29°C (84°F). During the driest month February you can expect a temperature of 29°C (84°F). For more detailed insights into the city's temperatures, visit our Fuvahmulah Temperature page.
Daily Historical Precipitation
33-year average (1985-2025)
Average daily rainfall for each day of the month based on long-term records.
Average precipitation in June
Explore Fuvahmulah's Historical Precipitation: 1981-2026
Browse day-by-day precipitation records for Fuvahmulah spanning 46 years. Select any month and year to see actual rainfall and snowfall recorded on each day.
Annual Rainfall in the Maldives: City Comparison
The map below shows the annual precipitation across the Maldives. You can also select the different months in case you are interested in a specific month.
heavy rainfall
high
moderate
low
almost none
Fuvahmulah vs World: Rainfall Compared
Fuvahmulah's average annual precipitation is 1854 mm (73 in). Let's compare this to some popular worldwide tourist destinations:
The city of Rome, Italy, has an average annual precipitation of 832 mm (33 in), spread fairly evenly throughout the year.
Osaka, Japan, experiences 1507 mm (59 in) of rainfall annually, spread across the year with wetter summers.
In Tokyo, Japan, the average annual precipitation is 1528 mm (60 in), with significant summer rains due to typhoon season.
Singapore, situated near the equator, gets 2581 mm (102 in) of rainfall annually, with no distinct dry season and consistent monthly precipitation.
Precipitation amounts are measured using specific gauges installed at weather stations, collecting both rain and snow and any other type of precipitation. Rainfall is measured directly in millimeters, while that from snow and ice is obtained by melting it. Automated systems often incorporate heaters to make this easier.
Information from these stations is transmitted via Wi-Fi, satellite, GPS, or telephone connections to central monitoring networks. This information is immediately updated and integrated into weather models and forecasts.
The proximity of a location to a large body of water can significantly affect its rainfall patterns:
- Ocean Influence: Coastal regions typically receive more rainfall due to the presence of moisture-laden winds from the ocean. These regions tend to have more humid climates and experience more frequent precipitation, especially in winter.
- Continental Climates: Areas further from the sea, such as inland or continental regions, experience less frequent rainfall and more extreme seasonal variations in precipitation.
- Mawsynram in India is noted as being the wettest place on earth, with over 11 meters (36 feet) of rain falling every year.
- In contrast, Antofagasta in Chile is among the driest places on the planet, getting less than 0.1mm (0.004 inches) per year, with some years recording virtually no rainfall.
- Nearly 1,650 thunderstorm cells are estimated over the planet at any given time.
For more detailed information about Fuvahmulah's weather, including sunshine hours, humidity levels, and temperature data, visit our Fuvahmulah Climate page.
