首页> 外文期刊>Palaeogeography, Palaeoclimatology, Palaeoecology: An International Journal for the Geo-Sciences >High-resolution modelling closes the gap between data and model simulations for Mid-Holocene and present-day biomes of East Africa
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High-resolution modelling closes the gap between data and model simulations for Mid-Holocene and present-day biomes of East Africa

机译:高分辨率建模弥合了全新世中期和东非当今生物群落的数据与模型模拟之间的差距

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摘要

East Africa hosts a striking diversity of terrestrial ecosystems, which vary both in space and time due to complex regional topography and a dynamic climate. The structure and functioning of these ecosystems under this environmental setting can be studied with dynamic vegetation models (DVMs) in a spatially explicit way. Yet, regional applications of DVMs to East Africa are rare and a comprehensive validation of such applications is missing. Here, we simulated the present-day and mid-Holocene vegetation of East Africa with the DVM, LPJ-GUESS and we conducted an exhaustive comparison of model outputs with maps of potential modern vegetation distribution, and with pollen records of local change through time. Overall, the model was able to reproduce the observed spatial patterns of East African vegetation. To see whether running the model at higher spatial resolutions (10' x 10') contribute to resolve the vegetation distribution better and have a better comparison scale with the observational data (i.e. pollen data), we run the model with coarser spatial resolution (0.5 x 0.5) for the present-day as well. Both the area-and point-wise comparison showed that a higher spatial resolution allows to better describe spatial vegetation changes induced by the complex topography of East Africa. Our analysis of the difference between modelled mid-Holocene and modern-day vegetation showed that whether a biome shifts to another is best explained by both the amount of change in precipitation it experiences and the amount of precipitation it received originally. We also confirmed that tropical forest biomes were more sensitive to a decrease in precipitation compared to woodland and savanna biomes and that Holocene vegetation changes in East Africa were driven not only by changes in annual precipitation but also by changes in its seasonality. (C) 2015 Elsevier B.V. All rights reserved.
机译:东非拥有多种多样的陆地生态系统,由于复杂的区域地形和动态的气候,其时空变化。可以在空间环境下使用动态植被模型(DVM)研究这些环境下这些生态系统的结构和功能。但是,DVM在东非的地区应用很少,因此缺少对此类应用的全面验证。在这里,我们使用DVM,LPJ-GUESS模拟了东非的现今和中全新世植被,并对模型输出与潜在的现代植被分布图以及随时间变化的局部花粉记录进行了详尽的比较。总体而言,该模型能够重现观察到的东非植被的空间格局。要查看以较高的空间分辨率(10'x 10')运行模型是否有助于更好地解析植被分布并与观测数据(即花粉数据)具有更好的比较尺度,我们以较粗糙的空间分辨率(0.5)运行模型x 0.5)。面积和逐点比较都表明,较高的空间分辨率可以更好地描述东非复杂地形引起的空间植被变化。我们对模拟的全新世中期植被与现代植被之间差异的分析表明,生物群落是否迁移到另一个群落最好用其经历的降水变化量和最初接受的降水量来解释。我们还证实,与林地和热带稀树草原生物群落相比,热带森林生物群落对降水减少更为敏感,而且东非全新世植被的变化不仅受到年降水量变化的影响,还受其季节性变化的影响。 (C)2015 Elsevier B.V.保留所有权利。

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