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首页> 外文期刊>Remote Sensing of Environment: An Interdisciplinary Journal >Analysis of plant colonization on an arctic moraine since the end of the Little Ice Age using remotely sensed data and a Bayesian approach
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Analysis of plant colonization on an arctic moraine since the end of the Little Ice Age using remotely sensed data and a Bayesian approach

机译:自小冰期结束以来,北极冰m上的植物定植利用遥感数据和贝叶斯方法进行分析

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摘要

Young moraines less than 100 years old are considered as key areas for monitoring the effects of climate change since the end of the Little Ice Age. One way of documenting this change is by recognizing and characterizing the different plant colonization stages and trends that occur on these relatively new environments. Previous studies have shown that remotely sensed data alone are not sufficient to map the vegetation over these types of landscapes because the most significant part of the radiometric information is related to mineral landscape components. Therefore, the authors used an indirect approach which consisted in the following steps. 1. An optimized sampling procedure was used to collect georeferenced vegetation plot data. A multivariate analysis was then used to define vegetation types that could be related to different colonization stages and environmental contexts. 2. Color infrared aerial photographs were then used to produce a baseline vegetation map. This map was then integrated into a data base along with other environment factors known to control,plant colonization processes, such as climate (wind, temperature), physical landscape components (habitat characteristics) and morphodynamic processes (runoff). 3. A Bayesian model using conditional probabilities was used to identify the primary environmental habitats corresponding to the different vegetation types. This protocol was tested on the fore field of the Midre Lovenbreen (Svalbard) glacier where several vegetation belts correspond to well defined stages of deglaciation and corresponding local conditions such as microtopography, microclimate and runoff dynamics.
机译:自小冰河时代结束以来,年龄不到100岁的年轻mo子被视为监测气候变化影响的关键地区。记录这种变化的一种方法是识别并表征在这些相对较新的环境中发生的不同植物定殖阶段和趋势。先前的研究表明,仅靠遥感数据不足以在这些类型的景观上绘制植被图,因为辐射信息的最重要部分与矿物景观成分有关。因此,作者采用了一种间接方法,该方法包括以下步骤。 1.一种优化的采样程序用于收集地理参考的植被图数据。然后,使用多变量分析来定义可能与不同定居阶段和环境环境相关的植被类型。 2.然后使用彩色红外航空照片制作基线植被图。然后将此地图与已知可控制植物定殖过程的其他环境因素(例如气候(风,温度),自然景观成分(栖息地特征)和形态动力学过程(径流))一起集成到数据库中。 3.使用条件概率的贝叶斯模型来识别与不同植被类型相对应的主要环境栖息地。该协议在Midre Lovenbreen(斯瓦尔巴特)冰川的前场进行了测试,其中几个植被带对应于冰川作用的明确定义阶段以及相应的局部条件,例如微地形,微气候和径流动力学。

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