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Canopy temperature and heat stress are increased by compound high air temperature and water stress and reduced by irrigation – a modeling analysis

机译:通过化合物高空气温度和水胁迫增加了冠层温度和热应激,并通过灌溉减少 - 一种建模分析

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摘要

Crop yield is reduced by heat and water stress and even more when these conditions co-occur. Yet, compound effects of air temperature and water availability on crop heat stress are poorly quantified. Existing crop models, by relying at least partially on empirical functions, cannot account for the feedbacks of plant traits and response to heat and water stress on canopy temperature. We developed a fully mechanistic model, coupling crop energy and water balances, to determine canopy temperature as a function of plant traits, stochastic environmental conditions, and irrigation applications. While general, the model was parameterized for wheat. Canopy temperature largely followed air temperature under well-watered conditions. But, when soil water potential was more negative than ?0.14 ? MPa , further reductions in soil water availability led to a rapid rise in canopy temperature – up to 10? ° C warmer than air at soil water potential of ?0.62 ? MPa . More intermittent precipitation led to higher canopy temperatures and longer periods of potentially damaging crop canopy temperatures. Irrigation applications aimed at keeping crops under well-watered conditions could reduce canopy temperature but in most cases were unable to maintain it below the threshold temperature for potential heat damage; the benefits of irrigation in terms of reduction of canopy temperature decreased as average air temperature increased. Hence, irrigation is only a partial solution to adapt to warmer and drier climates.
机译:当这些条件共同发生时,通过热量和水分胁迫减少了作物产量。然而,空气温度和水可用性对作物热应激的复合效应量很差。通过至少部分地依赖于经验职能来依赖于现有的作物模型,不能考虑植物性状的反馈和对冠层温度的热量和水胁迫的反馈。我们开发了一种全部机械模型,耦合作物能量和水平,以确定冠层温度作为植物特征,随机环境条件和灌溉应用的功能。虽然一般来说,该模型是针对小麦的参数化。冠层温度在很大程度上在含水良好的条件下遵循空气温度。但是,当土壤水潜力比0.14更负的时候? MPA,进一步减少土壤水可用性导致冠层温度快速上升 - 最多10? °C比空气温暖在土壤水潜力的空气中?0.62? MPA。更多间歇降水导致冠层温度较高,更长的潜在破坏性作物冠层温度。旨在在含水良好的条件下保持作物的灌溉应用可能降低冠层温度,但在大多数情况下,在大多数情况下无法将其维持在阈值温度以下,以进行潜在的热量损伤;随着平均空气温度的增加,灌溉的灌溉益处降低了。因此,灌溉只是适应温暖和干燥气候的部分解决方案。

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