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首页> 外文期刊>Agricultural and Forest Meteorology >Seasonal patterns of Mediterranean evergreen woodlands (Montado) are explained by long-term precipitation
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Seasonal patterns of Mediterranean evergreen woodlands (Montado) are explained by long-term precipitation

机译:地中海常绿林地(蒙塔多)的季节性模式可以通过长期降水来解释

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In temperate areas, vegetation seasonality and phenology have been mostly associated with temperature changes both in space and time. In drylands, where water is the most limiting factor, we expect that they strongly respond to water availability. The degree to what that response depends more on precipitation that occurred when vegetation seasonality and phenology were measured, or on the long-term precipitation, is not fully known. We hypothesize that in drylands, long-term precipitation better explains the patterns of seasonality and phenology metrics than concurrent one, due to constrains imposed by ecosystem legacy. We correlated long-term precipitation (30 years normal) and concurrent precipitation (12 years) to several seasonal metrics (MODIS, average of 12 years) measured in a savannah-like system, Mediterranean evergreen woodlands, located in southwest Europe (Portugal). We observed that seasonal metrics of productivity and phenology were more significantly related with long-term precipitation than with concurrent precipitation. Comparing the extremes of our gradient we found that drier areas (c. 496 mm long-term annual precipitation) showed average growth cycles of annual plants 25 days shorter and ended 16 days sooner than more rainy regions (c. 739 mm). Evergreen vegetation productivity was shown to be c. 30% lower in drier areas. Moreover, productivity and phenology metrics were non-linearly related to the long-term precipitation, suggesting both are particularly constrained below 600-650 mm. These results suggest a memory effect in the response of vegetation to climate, most probably associated to legacies on soil characteristics and on plant community. It also indicates the existence of ecosystem response thresholds in vegetation's response to precipitation along ecosystem transitions. Overall, this method can be used to track ecosystem services over space in drylands and for managing ecosystems for both mitigation and adaptation to climate change. (C) 2014 Elsevier B.V. All rights reserved.
机译:在温带地区,植被的季节性和物候学大多与时空的温度变化有关。在缺水最严重的旱地,我们希望它们对水的供应有强烈的反应。这种响应的程度更多地取决于测量植被季节性和物候学时发生的降水量,或者取决于长期降水量。我们假设在干旱地区,由于生态系统遗留因素的限制,长期降水比季节性降水和物候指标更好地解释了季节性和物候指标的模式。我们将长期降水(正常30年)和同期降水(12年)与几个季节指标(MODIS,平均12年)相关联,这些指标是在类似大草原的系统(位于欧洲西南部(葡萄牙)的地中海常绿林地)中测得的。我们观察到,生产力和物候的季节性指标与长期降水比与同期降水更相关。比较我们的极端梯度,我们发现较干燥的地区(约496毫米的长期年降水量)显示,一年生植物的平均生长周期比多雨的地区(约739毫米)短25天,并提前16天结束。常绿植被生产力显示为c。较干燥的地区降低30%。此外,生产力和物候指标与长期降水呈非线性关系,这表明两者都特别受限制在600-650 mm以下。这些结果表明,在植被对气候的响应中存在记忆效应,这很可能与土壤特征和植物群落的遗留力有关。这也表明生态系统响应阈值在植被对沿生态系统转变的降水响应中存在。总体而言,该方法可用于追踪干旱地区整个空间的生态系统服务,以及管理生态系统以缓解和适应气候变化。 (C)2014 Elsevier B.V.保留所有权利。

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