Rainfall averages about per year, higher in the hills and lower on the coast.

Rainfall can be quite variable, but the wettest months on average are September to November and the driest months on average are February and March.

Rainfall averages about per year, higher in the hills and lower on the coast.

Rainfall can be quite variable, but the wettest months on average are September to November and the driest months on average are February and March.

Rainfall is generally plentiful, and Pohnpei reputedly is one of the wettest places on earth, with up to 330 inches ( 8. 4 m ) of rain per year.

* John B. Ford ( born 1963 ), English horror writer and publisher whose fiction focuses on death and madness ; launched magazine, Terror Tales, in 1996 and Rainfall Records and Books in 2001

Rainfall also varies regionally, with the highest amounts -- annually — recorded on the Bolovens Plateau in Champasak Province.

Rainfall amounts vary from a low of in the lee of the Ngorongoro Highlands to a high of on the shores of Lake Victoria.

Rainfall can be quite variable, but the wettest months on average are September to November and the driest months on average are February and March.

Rainfall is below average with the heaviest precipitation on the South Downs with 950mm ( 37 in ) of rainfall per year.

Rainfall is moderate on the foothills and in some sheltered valleys, measuring 700 to 1, 000 mm per year, but increases significantly in the higher valleys with levels between 1, 000 mm and 1, 800 mm.

Rainfall averages 21. 2 inches annually and falls on an average of 59 days annually.

Rainfall is abundant with the yearly average approaching 67 inches and occurring on 127 days.

Rainfall during summer is, on average, less than half an inch each month with July receving the lowest monthly average precipitation of the year at. 07 inches.

Rainfall average's 576. 9 mm a year, with daily totals of over 1 mm falling on 105. 1 days of the year.

Rainfall on land that is not protected by a layer of mulch is left open to the elements of being impacted directly by the rain.

* Rainfall collected on roofs, yards, hard-standings, etc.

Rainfall shortages resulted in worst drought on record for Maryland, Delaware, New Jersey, and Rhode Island.

Rainfall in October 1960 was even heavier, when fell on the Somerset Levels, representing 249 per cent of the normal levels.

Rainfall on the mountain averages 4, 489 mm yearly with August being the wettest month with an average rainfall of 1, 135 mm.

* HPC Rainfall Page on Connie

Rainfall is higher in the winter months, and varies with elevation and exposure ; elevations above 500 meters experience almost daily rainfall, while the western, leeward side of Robinson Crusoe and Santa Clara are quite dry.

Rainfall was fairly light due to the fast movement and dry air on the southern side of the storm.

Rainfall is however less heavy than in most parts of mainland Japan since the island is too far south to be influenced by the Aleutian Low and too far from Asia to receive monsoonal rainfall or orographic precipitation on the equatorward side of the Siberian High.

Rainfall distribution variation ( Figure 1 ) is influenced by rain shadow effect of the mountainous belt on the eastern side of Bukidnon and by the presence of adjoining hills and mountain ranges.

Rainfall on the western side of the peak ( after several creeks ) enters the Middle Fork of the Flathead River, which in turn enters the Clark Fork River, Pend Oreille River, and the Columbia River which empties into the Pacific Ocean at Astoria, Oregon.

With the Intertropical Convergence Zone ( ITCZ ) swinging northward over West Africa from the Southern Hemisphere in April, heavy showers coming from pre-monsoonal convective clouds mainly in the form of squall lines also known as the north easterlies formed mainly as a result of the interactions of the two dominant airmasses in Nigeria known as the Maritime tropical ( south westerlies ) and the Continental tropical ( north easterlies ), begins in central Nigeria while the Monsoons from the south atlantic ocean arrives in central Nigeria in July bringing with it high humidity, heavy cloud cover and heavy rainfall which can be daily occurrence lasting till September when the monsoons gradually begin retreating southward to the southern part of Nigeria. Rainfall totals in central Nigeria varies from in the lowlands of the river Niger Benue trough to over along the south western escarpment of the Jos Plateau.

Rainfall in the Guinea zone, located in Chad's southwestern tip, ranges between.

Rainfall may average per year in the higher central area as compared with in the coastal zone.

Rainfall patterns vary widely throughout the subtropics including hot deserts, savannas, monsoon forests, humid forests and the warmer parts of the Mediterranean climate zone.

Rainfall is less than 300 millimeters per annum as the region falls outside the monsoon zone.

Rainfall, especially during the summer monsoon, percolates into the bhabar, then is forced to the surface by finer alluvial layers below it in a zone of springs and marshes along the northern edge of the Terai or plains.

Rainfall and snowfall increase on the mountains as these rise, perhaps at a rate of a few millimeters per year ( at a growth rate of 1 mm / year, a 5, 000 m tall mountain can form in 5 million years, a time period that is less than 10 % of the life of a typical collision zone ).

Rainfall absorbs this salt on the surface, and carries it down into the subsoil where it is stored in unsaturated soil profiles, until it is once again mobilised by ground water and rising water tables.

Rainfall is infrequent – 63 days a year, but can be torrential, particularly in September, when storms and rain are caused by the difference between the colder air inland and the warm Mediterranean water temperature ( 20 – 24 degrees C .).

Rainfall is concentrated from September to May, while the rest of the year the mass of dry air over the center of Brazil rainy inhibit the formations.

Rainfall is usually only produced by the most vigorous frontal systems or by occasional penetration of tropical air in the summer.

Rainfall around the basin increases with elevation.

Rainfall intensity is the primary determinant of erosivity, with higher intensity rainfall generally resulting in more erosion.

Rainfall in summer is convectional, while relief rainfall dominates in the winter, with some snow.

Rainfall is light to moderate throughout the year with 169 wet days.

Rainfall is mainly orographic and increases in amount and frequency with the altitude.

* Rainfall of around 250 cm evenly distributed without any marked dry season and with at least 100 rainy days per year.

Rainfall is rare in this season, and a typical July month only records one or two days with measurable rainfall.

Rainfall averages around a year, with the wettest months being June through September.

Rainfall tends to be associated with Atlantic depressions or with convection.

Rainfall below per annum needs be complemented with, for example, a drip irrigation system.

Rainfall occurs primarily between July and December and varies considerably with elevation.

Rainfall, although scanty everywhere, is greater in the northern half, where the land is covered with scrub vegetation.

Rainfall is generally spread throughout the year, with eight to twelve wet days per month, at an average annual rate of.

Rainfall decreases from east to west, resulting in different types of prairies, with the tallgrass prairie in the wetter eastern region, mixed-grass prairie in the central Great Plains, and shortgrass prairie towards the rain shadow of the Rockies.