Tropical rainfall variability — The agroclimatic impact

S. Nieuwolt
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引用次数: 20

Abstract

In tropical lowlands, agriculture is largely controlled by rainfall conditions. In these areas, most elements of climate, and particularly temperatures, are very uniform both over place and time, but rainfall is much more variable. Lack of sufficient rainfall is the main limiting factor in agriculture in most tropical areas. Long-term predictions, expected from agroclimatologist, should be mainly concerned with rainfall, but the irregularity of this element makes this a difficult task.

Therefore an obvious need exists for methods to quantify rainfall variability in relation to agriculture. These methods should be simple, so that they can be used wherever necessary without the use of a computer. Peninsular Malaysia offers favourable conditions for the study and application of these methods.

Annual rainfall totals present a picture of endless variations, with no clear trend or cycles. The seasonal rainfall distribution is much more regular, as large-scale weather patterns are frequently controlled by the monsoonal wind systems. Agricultural conditions determined by seasonal rainfall can be described most conviniently by probability figures. When these are related to crop water needs, as is done in the Agricultural Rainfall Index, the risk of droughts can be indicated accurately enough for most agroclimatic purposes. The proper selection of crops and correct timing of planting can also be decided by this method.

The irregularity of rainfall from day to day affects the growth and yields of many crops, particularly those with shallow root systems. Even during seasons which are generally considered favourable for crop production, temporary shortages or surpluses of rainfall occur often. To obtain estimates of these effects a daily water-balance model is introduced. Risks are indicated by the number of days with severe moisture stress and by the amount of surplus rain water. A comparison with a more sophisticated computer programme shows the validity and accuracy of the model.

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热带降雨变率-农业气候影响
在热带低地,农业主要受降雨条件的控制。在这些地区,气候的大部分要素,尤其是温度,在时间和地点上都是非常均匀的,但降雨的变化要大得多。缺乏充足的降雨是大多数热带地区农业的主要限制因素。农业气候学家所期望的长期预测应该主要与降雨有关,但这一因素的不规律性使这一任务变得困难。因此,显然需要找到方法来量化与农业有关的降雨变异性。这些方法应该很简单,这样就可以在任何需要的地方使用,而不需要使用电脑。马来西亚半岛为这些方法的研究和应用提供了有利条件。年降雨量呈现出无穷变化的画面,没有明显的趋势或周期。由于大尺度的天气模式经常受到季风系统的控制,季节性降雨分布更加规律。由季节降雨决定的农业条件可以用概率图最方便地描述。当这些与作物需水量相关时,就像农业降雨指数所做的那样,干旱的风险可以足够准确地显示出来,用于大多数农业气候目的。正确的作物选择和正确的种植时间也可以通过这种方法来决定。每天降雨的不规律影响了许多作物的生长和产量,特别是那些根系较浅的作物。即使在通常被认为有利于作物生产的季节,也经常出现暂时的降雨短缺或过剩。为了估计这些影响,引入了日水平衡模型。风险由严重湿气胁迫的天数和剩余雨水的数量来表示。与更复杂的计算机程序的比较表明了该模型的有效性和准确性。
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