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Rainfed rice - IRRI books - International Rice Research Institute

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Influence of Agro-Ecosystem Components on <strong>Rice</strong> Production<br />

Table 1. Influence of rainfall and landform/physiography on the hydrology of rainfed <strong>rice</strong> lands<br />

Landform/physiography<br />

Rainfall<br />

(amount/intensity) 1 Plains Gently sloping Low-lying<br />

High amount<br />

High intensity Abrupt accumulation Abrupt accumulation but fast Abrupt accumulation<br />

but slow recession recession (flood: shorter but slow recession (flood:<br />

(flood: intermediate duration and shallow). longer duration and deep).<br />

duration, and depth).<br />

Low intensity Gradual accumulation Gradual accumulation but fast Gradual accumulation and<br />

but fast recession recession (flood: shorter slow recession (flood: longer<br />

(flood: intermediate duration and shallow). duration and deep).<br />

duration and depth).<br />

Normal amount<br />

High intensity No accumulation Gradual accumulation but fast<br />

(no flood and no recession (no flood and no<br />

drought). drought).<br />

Abrupt accumulation but<br />

slow recession (flood: longer<br />

duration and deep).<br />

Low intensity No accumulation No accumulation (no flood Gradual accumulation and<br />

(no flood and no and no drought). slow recession (flood:<br />

drought). shorter duration and<br />

intermediate depth).<br />

Low amount<br />

High intensity No accumulation No accumulation (no flood, Abrupt accumulation (also<br />

(flood, but may have but drought occurs). because of drainage from<br />

drought)'. catchment) but slow<br />

recession (flood: longer<br />

duration and intermediate/<br />

shorter depths).<br />

Low intensity No accumulation (no No accumulation (no flood, Gradual accumulation, slow<br />

flood, but drought but drought occurs). recession (flood: shorter<br />

occurs). duration and shallow).<br />

1 Amount refers to total annual rainfall and intensity refers to one occurrence.<br />

Rainfall and water depth<br />

The rainfall in June-October during<br />

1984-92 and peak water depth<br />

accumulation in Ghaghraghat,<br />

Bahraich District, show that<br />

accumulation of water depends not<br />

only on total rainfall in an area, but<br />

also on the duration, intensity and<br />

period of rainfall as well as drainage<br />

from the catchment area.<br />

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