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Modelling and observation of biosphere-atmosphere interactions in natural savannah in Burkina Faso, West Africa

机译:西非布基纳法索自然稀树草原中生物圈-大气相互作用的模拟和观测

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Savannahs are highly dynamic ecosystems but many of their properties and the related balances of energy, carbon, nitrogen, and water are still poorly understood. A particular scientific issue is the quantification of trace gases emitted from the soil of savannah ecosystems and their interaction with regional and global climate and air chemistry. Therefore it is important to develop and evaluate land-surface models that on the one hand represent vegetation and soil dynamics and on the other hand provide energy and water fluxes in a temporal resolution suitable for the application in climate/air chemistry models. In this paper, we present a consistent Coupling between a common land-surface model (OSU) and a widely used biogeochemical model (DNDC) that is a first step for a full coupling of climate/air chemistry and biogeochemical processes. For consistency reasons, both models are linked to a general physiologically based plant model to provide the physical boundary conditions as well as the carbon and nitrogen in- and Output variables. Evaluation is carried out with measurements of soil temperature, latent heat flux, soil water content, and soil emission data from two vegetation periods collected at a natural grassland site in Bontioli Nature Reserve, Burkina Faso (Africa). The results demonstrate that simulations of biogeochemical processes based on soil environmental conditions, calculated either with the land-surface model or with the unchanged biogeochemical model, do not differ significantly from each other. The OSU model simulates more realistic day-to-day variation of soil temperature as DNDC but the sensitivity of the biogeochemical simulation to this variation is small. In contrast, the sensitivity to differences in soil water content is high, but simulation results of both models are very similar on the daily scale and hardly depend on spatial soil resolution.
机译:稀树草原是高度动态的生态系统,但对它们的许多特性以及能量,碳,氮和水的相关平衡仍然知之甚少。一个特殊的科学问题是对稀树草原生态系统土壤中排放的痕量气体的定量及其与区域和全球气候及空气化学的相互作用。因此,开发和评估一方面代表植被和土壤动力学,另一方面以适合于气候/空气化学模型应用的时间分辨率提供能量和水通量的陆地表面模型非常重要。在本文中,我们提出了一个常见的陆地表面模型(OSU)与广泛使用的生物地球化学模型(DNDC)之间的一致耦合,这是将气候/空气化学与生物地球化学过程完全耦合的第一步。出于一致性原因,这两个模型都链接到基于生理的一般植物模型,以提供物理边界条件以及碳和氮的输入和输出变量。通过对在布基纳法索(非洲)邦蒂奥利自然保护区的天然草地场采集的两个植被时期的土壤温度,潜热通量,土壤水分含量和土壤排放数据进行测量来进行评估。结果表明,基于土壤环境条件的生物地球化学过程模拟,无论是用陆地表面模型还是使用不变的生物地球化学模型计算,都没有显着差异。 OSU模型以DNDC来模拟更实际的土壤温度的日常变化,但是生物地球化学模拟对这种变化的敏感性很小。相反,对土壤含水量差异的敏感性很高,但是两个模型的模拟结果在日尺度上非常相似,并且几乎不依赖于空间土壤分辨率。

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