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Comparison of tree transpiration under wet and dry canopy conditions in a Costa Rican premontane tropical forest

机译:潮汐干燥冠覆条件下树蒸腾对哥斯达黎加的热带热带森林的比较

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Spatial and temporal variation in wet canopy conditions following precipitation events can influence processes such as transpiration and photosynthesis, which can be further enhanced as upper canopy leaves dry more rapidly than the understory following each event. As part of a larger study aimed at improving land surface modelling of evapotranspiration processes in wet tropical forests, we compared transpiration among trees with exposed and shaded crowns under both wet and dry canopy conditions in central Costa Rica, which has an average 4200mm annual rainfall. Transpiration was estimated for 5months using 43 sap flux sensors in eight dominant, ten midstory and eight suppressed trees in a mature forest stand surrounding a 40-m tower equipped with micrometeorological sensors. Dominant trees were 13% of the plot's trees and contributed around 76% to total transpiration at this site, whereas midstory and suppressed trees contributed 18 and 5%, respectively. After accounting for vapour pressure deficit and solar radiation, leaf wetness was a significant driver of sap flux, reducing it by as much as 28%. Under dry conditions, sap flux rates (J(s)) of dominant trees were similar to midstory trees and were almost double that of suppressed trees. On wet days, all trees had similarly low J(s). As expected, semi-dry conditions (dry upper canopy) led to higher J(s) in dominant trees than midstory, which had wetter leaves, but semi-dry conditions only reduced total stand transpiration slightly and did not change the relative proportion of transpiration from dominant and midstory. Therefore, models that better capture forest stand wet-dry canopy dynamics and individual tree water use strategies are needed to improve accuracy of predictions of water recycling over tropical forests. Copyright (c) 2016 John Wiley & Sons, Ltd.
机译:沉淀事件后湿冠覆条件的空间和时间变化可以影响蒸腾和光合作用的过程,这可以进一步增强,因为上层冠层比每个事件的林林更快地烘干。作为旨在改善湿热带森林中蒸发过程的蒸发过程的土地表面建模的较大研究的一部分,我们在哥斯达黎加中部潮湿和干燥的树冠条件下与暴露和阴影冠的树木进行比较,平均每年降雨量为4200毫米。在一座成熟的森林站在一个配备微气象传感器的40米塔的成熟森林站中,使用43个SAP通量传感器估计蒸腾率为5个月。主导树木是13%的地块树木,贡献了这个网站的总蒸腾率约为76%,而中间和抑制的树木分别贡献了18%和5%。在蒸汽压力缺陷和太阳辐射核算后,叶片湿度是SAP通量的重要驱动器,将其降低到28%。在干燥条件下,显性树木的SAP助熔剂速率(J(S))类似于中立树,几乎是抑制树木的两倍。在潮湿的日子里,所有树木都有类似地低J(s)。正如预期的那样,半干燥条件(干燥的上层)导致较高的j(干燥的上层)比中立的j更高,它具有湿润的叶子,但半干燥条件仅减少了总支架蒸腾,并没有改变蒸腾的相对比例来自主导和中立。因此,需要更好地捕获森林湿干燥机动力学和单独的树用水策略的模型,以提高热带森林的水回收预测的准确性。版权所有(c)2016 John Wiley&Sons,Ltd。

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