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Yoshida - 1981 - Fundamentals of Rice Crop Science

Yoshida - 1981 - Fundamentals of Rice Crop Science

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CLIMATIC ENVIRONMENT AND ITS INFLUENCE 69<br />

2.2. Effect <strong>of</strong> technical improvement on average brown-rice yields in Hokkaido, Japan, during<br />

the past 90 years (Satake 1976).<br />

managed, the dry season crop usually produces higher yields than the wet season<br />

crop because it receives more sunlight.<br />

Stability <strong>of</strong> crop yields is affected by several factors. In Hokkaido, which is the<br />

northern limit <strong>of</strong> rice cultivation in Japan, low temperatures frequently cause crop<br />

failure. Between 1880 and 1970, 22 crops were affected by cool summer temperatures<br />

(Fig. 2.2). In addition, low sunlight associated with excessive rainfall during<br />

ripening causes low yields. Too little or too much rainfall at any stage <strong>of</strong> rice<br />

growth can cause partial or total crop failure. In Thailand, more than 15% <strong>of</strong> the<br />

cropped area totally failed because <strong>of</strong> either drought or flood during 8 <strong>of</strong> the 58<br />

years from 1907 to 1965 (Table 2.3). In 24 <strong>of</strong> the 58 years, more than 10% <strong>of</strong> the<br />

cropped area was not harvested at all.<br />

In both the tropics and the temperate region, typhoons are unavoidable hazards.<br />

One way to minimize crop damage by typhoons is to shift crop seasons so that<br />

ripening proceeds when typhoons are least frequent.<br />

2.3. TEMPERATURE<br />

2.3.1. Physical aspects<br />

Average temperatures for a month or a year are computed from daily mean<br />

temperatures, which are usually calculated by averaging the daily maximum<br />

temperature plus the daily minimum temperature.

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