Za

Za ba̱shekkwot ba a̱ bvwa nyyai a nu̱nyaan rot ryoi a tung a̱tantai ni. Za a̱mi yet ka̱hyok a̱kpak a̱zuzrak ba̱shekkwot ka̱sa nu.
Za nji yet duwwik ti wwut nyai a nunyaan na a a̱ shrim a su tyi akukwang bashekkwot ni kaya atantai wwon a bvwa rot cet kwak nkyang a sshi an tswa kabyen ni (gravity). Za nji ami yet agbadang kahyok u azuzrak bashekkwot kasa nu na n wut ni. Nji wwat bashekkwot kuyak bu kuyak syang bu ruk ring lantarki bu nkyang zaan kayat kasa ka.
Kyang a cong bu za ni nkpa yet rywoi a sshi an wun ni nyyi na naat n bvwot u nabvwa bagungang ní.

The major cause of rain production is moisture moving along three-dimensional zones of temperature and moisture contrasts known as weather fronts. If enough moisture and upward motion is present, precipitation falls from convective clouds (those with strong upward vertical motion) such as cumulonimbus (thunder clouds) which can organize into narrow rainbands. In mountainous areas, heavy precipitation is possible where upslope flow is maximized within windward sides of the terrain at elevation which forces moist air to condense and fall out as rainfall along the sides of mountains. On the leeward side of mountains, desert climates can exist due to the dry air caused by downslope flow which causes heating and drying of the air mass. The movement of the monsoon trough, or Intertropical Convergence Zone, brings rainy seasons to savannah climes.

The urban heat island effect leads to increased rainfall, both in amounts and intensity, downwind of cities. Global warming is also causing changes in the precipitation pattern, including wetter conditions across eastern North America and drier conditions in the tropics. Antarctica is the driest continent. The globally averaged annual precipitation over land is 715 mm (28.1 in), but over the whole Earth, it is much higher at 990 mm (39 in).[1] Climate classification systems such as the Köppen classification system use average annual rainfall to help differentiate between differing climate regimes. Rainfall is measured using rain gauges. Rainfall amounts can be estimated by weather radar.́́́́́́́

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