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首页> 外文期刊>Global change biology >Climate-driven uncertainties in modeling terrestrial energy and water fluxes: a site-level to global-scale analysis.
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Climate-driven uncertainties in modeling terrestrial energy and water fluxes: a site-level to global-scale analysis.

机译:由气候驱动的不确定性,用于模拟地面能量和水通量:从站点级到全球范围的分析。

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We used a land surface model constrained using data from flux tower sites, to analyze the biases in ecosystem energy and water fluxes arising due to the use of meteorological reanalysis datasets. Following site-level model calibration encompassing major vegetation types from the tropics to the northern high-latitudes, we repeated the site and global simulations using two reanalysis datasets: the NCEP/NCAR and the CRUNCEP. In comparison with the model simulations using observed meteorology from sites, the reanalysis-driven simulations produced several systematic biases in net radiation (Rn), latent heat (LE), and sensible heat (H) fluxes. These include: (i) persistently positive tropical/subtropical biases in Rn using the NCEP/NCAR, and gradually transitioning to negative Rn biases in the higher latitudes; (ii) large positive H biases in the tropics/subtropics using the NCEP/NCAR; (iii) negative LE biases using the NCEP/NCAR above 40 degrees N; (iv) high tropical LE using the CRUNCEP in comparison with observationally derived global estimates; and (v) flux-partitioning biases from canopy and ground components. Across vegetation types, we investigated the role of the meteorological drivers (shortwave and longwave radiation, atmospheric humidity, temperature, precipitation) and their seasonal biases in controlling these reanalysis-driven uncertainties. At the global scale, our site-level analysis explains several model-data differences in the LE and H fluxes when compared with observationally derived global estimates of these fluxes. Using our results, we discuss the implications of site-level model calibration on subsequent regional/global applications to study energy and hydrological processes. The flux-partitioning biases presented in this study have potential implications on the couplings among terrestrial carbon, energy, and water fluxes, and for the calibration of land-atmosphere parameterizations that are dependent on LE/H partitioning.
机译:我们使用了受通量塔站点数据约束的地表模型,分析了由于使用气象再分析数据集而导致的生态系统能量和水通量偏差。在站点级别的模型校准涵盖了从热带到北部高纬度的主要植被类型之后,我们使用两个重新分析数据集(NCEP / NCAR和CRUNCEP)重复了站点和全局模拟。与使用现场观测气象的模型模拟相比,重新分析驱动的模拟在净辐射(R ),潜热(LE)和显热(H)通量方面产生了一些系统性偏差。其中包括:(i)使用NCEP / NCAR在R n 中持续保持正热带/亚热带偏向,并在高纬度地区逐渐转变为负R n 偏向; (ii)使用NCEP / NCAR在热带/亚热带具有较大的正H偏向; (iii)使用NCEP / NCAR在40度N以上产生负LE偏差; (iv)与通过观测得出的全球估算值相比,使用CRUNCEP的热带低气压; (v)冠层和地面部分的通量分配偏差。在各种植被类型中,我们研究了气象驱动因素(短波和长波辐射,大气湿度,温度,降水)及其季节性偏差在控制这些重新分析驱动的不确定性中的作用。在全球范围内,我们的站点级分析解释了LE和H通量与观测通量对这些通量的全球估算值相比的几种模型数据差异。使用我们的结果,我们讨论了站点级模型校准对随后的研究能源和水文过程的区域/全球应用的影响。这项研究中提出的通量分配偏差对陆地碳,能量和水通量之间的耦合以及依赖于LE / H划分的陆地-大气参数化的校准具有潜在的影响。

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