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Changes in rainfall interception along a secondary forest succession gradient in lowland Panama

机译:巴拿马低地次生林演替梯度中降雨截留量的变化

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Secondary forests are rapidly expanding in tropical regions. Yet, despite the importance of understanding the hydrological consequences of land-cover dynamics, the relationship between forest succession and canopy interception is poorly understood. This lack of knowledge is unfortunate because rainfall interception plays an important role in regional water cycles and needs to be quantified for many modeling purposes. To help close this knowledge gap, we designed a throughfall monitoring study along a secondary succession gradient in a tropical forest region of Panama. The investigated gradient comprised 20 forest patches 3 to 130 yr old. We sampled each patch with a minimum of 20 funnel-type throughfall collectors over a continuous 2- month period that had nearly 900mm of rain. During the same period, we acquired forest inventory data and derived several forest structural attributes. We then applied simple and multiple regression models (Bayesian model averaging, BMA) and identified those vegetation parameters that had the strongest influence on the variation of canopy interception. Our analyses yielded three main findings. First, canopy interception changed rapidly during forest succession. After only a decade, throughfall volumes approached levels that are typical for mature forests. Second, a parsimonious (simple linear regression) model based on the ratio of the basal area of small stems to the total basal area outperformed more complex multivariate models (BMA approach). Third, based on complementary forest inventory data, we show that the influence of young secondary forests on interception in realworld fragmented landscapes might be detectable only in regions with a substantial fraction of young forests. Our results suggest that where entire catchments undergo forest regrowth, initial stages of succession may be associated with a substantial decrease of streamflow generation. Our results further highlight the need to study hydrological processes in all forest succession stages, including early ones.
机译:热带地区的次生林正在迅速扩大。然而,尽管重要的是要了解土地覆盖动力学的水文后果,但对森林演替和林冠截留之间的关系知之甚少。缺乏知识是不幸的,因为降雨截获在区域水循环中起着重要作用,并且需要为许多建模目的进行量化。为了帮助弥合这一知识鸿沟,我们在巴拿马热带森林地区中,根据次生演替梯度设计了一项贯穿监测研究。所调查的坡度包括20个3至130岁的森林斑块。在连续2个月的降雨期间,我们用至少20个漏斗型穿透收集器对每个斑块进行了采样,降雨量接近900mm。在同一时期,我们获取了森林清单数据并得出了几种森林结构属性。然后,我们应用了简单的多元回归模型(贝叶斯模型平均,BMA),并确定了对冠层截留变化影响最大的植被参数。我们的分析得出了三个主要发现。首先,在森林演替过程中,林冠截留变化迅速。仅仅十年之后,穿透量就达到了成熟森林的典型水平。其次,基于小茎基面积与总基面积之比的简约(简单线性回归)模型优于更复杂的多元模型(BMA方法)。第三,基于补充的森林清单数据,我们表明,仅在具有大量未成年森林的区域中,才可以检测到次生年轻森林对现实世界零散景观中的截留的影响。我们的结果表明,在整个集水区都经历森林再生的情况下,演替的初始阶段可能与溪流产生的大量减少有关。我们的结果进一步强调了需要研究所有森林演替阶段(包括早期)的水文过程。

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