climate change will shift every aspect, such as temperature, rainfall, and storm patterns, as well as bringing fundamental changes in the physical environment, such as rising sea levels and changes in ocean chemistry.

Average rainfall in winter to 115 mm.

Leaving crop residues on the soil changes the surface characteristics. It increases rainfall efficiency, as water gets caught by and then percolates through the residues and soil.

Rainfall in the upland mountain ranges is heavier.

The maximum rainfall in one year was in 1983.

This rainfall cycle, this rainfall factory, effectively feeds an agricultural economy of the order of 240 billion dollars worth in Latin America.

The most rainfall in one month was in March 1991.

Rainfall in Canada peaked at 4.27 inches (108 mm) in Quebec.

Shifts in rainfall patterns will certainly affect crops, particularly rice.

The average annual rainfall is around .

However, there are large variations in depth depending on the rainfall.

at the rainfall , though before that they had been in despair .

at the rainfall , though before that they had been in despair .

Rainfall in Dammam is generally sparse, and usually occurs in small amounts in December.

It receives about 520 millimeters of rainfall annually.

During the monsoon, rainfall averages 40 mm day.

and execute the great task of apportioning ( rainfall )

Rainfall is however highly variable, and droughts are common.

Rainfall is about 49 inches per year (120 cm).

Rainfall in most of the rest of the country runs between these two extremes.

Other Parties expected an increase in rainfall and flooding, thus affecting hydroelectric power generation.

The continent suffers from one of the most unstable rainfall regimes in the world.

After March, the rainfall rapidly diminishes and from May to September wet mists float from the highlands into the plateaus, with almost no rainfall during these months.

The average rainfall is 500 600 mm per square meter.

There is a general deficiency of rainfall. Rains are monsoonic in origin and fall late in summer.

Rainfall patterns are changing. Deserts and dry regions are becoming drier.

The bad rainy season with rainfall far below the annual average occurred in summer 2006 07.

Average rainfall reaches 100 200 mm in the northeastern areas and 200 300 mm in the northwestern areas.

Gunung Leuser, receives 3000 mm of rainfall, in the north, and collects 4657 mm in the lowland south.

Rainfall patterns will vary, and the Asian monsoon will become less reliable.

The climate is equatorial, with little rainfall, constant wind, and strong sunshine.

(a) the climate of the region, and its influence on rainfall patterns

Water In some areas sufficient rainfall is available for crop growth, but many other areas require irrigation.

These changes are also triggering changes in human consciousness.

In such cases, rainfall is the most important meteorological factor in determining the food security situation locally and nationally.

Rainfall at Coleraine typically peaks at over 100mm during the month of October.

(b) rainfall patterns, and their influence on surface hydrology, and related hydro geology

Considerable variations occur because of local conditions that affect wind currents, however, and areas on the leeward side of the Guajira Peninsula receive generally light rainfall the annual rainfall of recorded at the Uribia station there is the lowest in Colombia.

Climate in this area has mild differences between highs and lows, and there is adequate rainfall year round.

The average annual temperature in La Rinconada is 1.2 C and the average annual rainfall is 707 mm.

Surface water is scarce in Botswana and less than 5 of the agriculture in the country is sustainable by rainfall.

On average, the region receives less than 15 inches (381mm) of rainfall per year.

Precipitation is moderate to heavy in most parts of the country the heavier rainfall occurs in the low lying hot zone.

Small changes in inputs can result in large changes in the value of a company.

But countries like Ethiopia have virtually no water storage facilities, great variability in rainfall, and attractive sites for hydroelectric generation.