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Rainfall and amounts
Rainfall also varies regionally, with the highest amounts -- annually — recorded on the Bolovens Plateau in Champasak Province.
Rainfall is fairly evenly distributed throughout the year, and annual amounts increase from southeast to northwest.
Rainfall tends to be heavily concentrated in summer, and the area receives extensive amounts of sunshine.
Rainfall in Jeddah is generally sparse, and usually occurs in small amounts in December.
Rainfall amounts of over in the area west of where Connie made landfall.
Rainfall in Dammam is generally sparse, and usually occurs in small amounts in December.
Rainfall amounts amounted to a maximum of 8. 41 inches ( 210 mm ) in Tavernier, while other locations reported lesser amounts.
Rainfall is incredulously low ; the average annual rainfall total amounts to a mere.
Rainfall was moderate across Louisiana, including amounts of over 8 inches ( 200 mm ) in the southwestern portion of the state.
Rainfall in this humid tropical climate amounts to around 850 mm ( 33 inches ) annually, largely concentrated in the months December to March.

Rainfall and vary
* Rainfall: Rainfall should vary between 1, 500 mm to 1, 800 mm.
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 in Colmar is 500 mm, but can vary greatly between sites.
The northernmost point at which crops had not failed was marked as " Goyder's Line of Rainfall " and corresponds approximately to the 300-millimetre ( 12 inch ) annual isohyet ( figures vary from 250 to 350 millimetres in different publications ).
Rainfall patterns throughout the municipality vary with elevation, with the upper areas having a relatively greater amount of rainfall than the lower areas.

Rainfall and from
Rainfall from April to September in the Tonle Sap Basin-Mekong Lowlands area averages annually, but the amount varies considerably from year to year.
Rainfall is negligible from May to September, but for the rest of the year it is adequate for rain-fed farming.
Rainfall during this season generally comes from low pressure over the Pacific and usually falls in heavy afternoon thunderstorms.
Rainfall shifts from the western Pacific toward the Americas, while Indonesia and India become drier.
Rainfall is less pronounced from December through May, when the equatorial low-pressure system moves south.
Rainfall varies from a year across the country ; actual rainfall has ranged from a year to as much as.
Rainfall changes from in the south to elsewhere.
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 varies from as little as less than 10 inches a year to over 150 inches a year, in various parts of the nation.
Rainfall is light, varying from per year, except in the higher land to the northwest where it is somewhat greater.
Rainfall varies from per year.
Rainfall varies from per year.
Rainfall, although adequate throughout the country, decreases from west to east and from mountains to plains.
Rainfall pattern of the country is influenced by Monsoon winds from the Indian Ocean and Bay of Bengal.
Rainfall ranges from over ( temperate rainforest ) conditions at the west end to as little as at the east end.
Rainfall during the summer months is mainly from thunderstorms and thundery showers ; from January to March the heavier rainfall is due to prevailing south-westerly frontal systems.

Rainfall and low
Rainfall is low and highly variable, and much of Jordan's available ground water is not renewable.
Rainfall, at around 620 mm is typical for low lying areas of central and eastern England.
Rainfall is greatest in winter months ( between November and March ) and very low in summer ( between June and August ).
Rainfall is generally low, at under 600mm, and spread fairly evenly throughout the year.
Rainfall is primarily produced by the monsoonal low during summer ; in winter, when the vast Siberian High dominates due to radiative cooling from further north, the area receives little precipitation.
Rainfall is quite low as it is in the rain shadow of mountains to the west and southwest.
Rainfall is extremely low ; the entire region receives fewer than of rainfall annually, and the western part receives as little as.
Rainfall is extremely low at less than 75 millimetres ( 3 inches ) per year.
Rainfall is very low, and the evaporation rate classifies the area as desert, even though the rainfall just barely exceeds 10 inches.
The top photo shows the lake with low water levels, exposing large tracts of salt flat | salt and mud flat s. Rainfall afterwards resulted in flooding of Poopó with muddy waters from the Desaguadero River ( Bolivia ) | Desaguadero River.
Rainfall is low ; Barletta receives 500 mm of rain annually, with most of the rain in autumn and winter day-long deluges and minimal rain between the second half of June and the first half of August.
Rainfall averages about 1, 500 mm yearly on the Loyalty Islands, 2, 000 mm at low elevations on eastern Grand Terre, and 2, 000-4, 000 mm at high elevations on Grand Terre.
Rainfall was also reported in California, but that was mostly due to an upper-level low.
Rainfall per month on the coast typically ranges from around in February and March to around in September ; it can average as low as between May and September inland, where exposed areas sometimes suffer bushfires after droughts, as occurred in 1915 and 2000.

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