首页> 外文期刊>International Journal of Climatology: A Journal of the Royal Meteorological Society >Reconstruction of a 1436-year soil moisture and vegetation water use history based on tree-ring widths from Qilian junipers in northeastern Qaidam Basin, northwestern China
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Reconstruction of a 1436-year soil moisture and vegetation water use history based on tree-ring widths from Qilian junipers in northeastern Qaidam Basin, northwestern China

机译:基于柴达木盆地东北祁连木杜鹃树轮宽度的1436年土壤水分和植被水分利用历史的重建

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摘要

Tree-ring widths have been used widely in studies of environmental changes and reconstructions of past climate. Eleven tree-ring chronologies of approximately 800-1500 years long were developed from Qilian junipers (Sabina przewalskii Kom.) for northeastern Qaidam Basin, along the margin of the Qinghai-Tibetan Plateau. Previous studies have revealed that water usage stress is the most limiting factor for tree growth in the study region. To evaluate the impact of the combined effects of temperature and precipitation changes over time, we performed water balance modelling using 1955-2002 meteorological data. We found that the tree-ring widths were strongly correlated with variables representing soil moisture conditions obtained from the water balance model. Specifically we considered actual evapotranspiration (AE) to represent the combined effect of water use demand and moisture availability, deficit as the difference between potential evapotranspiration (PE) and AE to represent the severity of water use stress, and relative soil moisture as the measure of moisture availability. For certain individual monthly and seasonal combinations, the tree-ring chronologies explained up to 80% of the variation in the soil moisture variables in regression analysis, indicating very good potential for reconstruction of regional soil moisture conditions in the past. These soil moisture variables outperformed precipitation and Palmer's drought severity index in most cases. We reconstructed the soil moisture conditions from 566 AD to 2001, which revealed major dry and wet periods and a general trend toward a wetter condition during the most recent 300 years. By comparing with other proxies in the region, we concluded that the moisture conditions reconstructed from tree-ring widths very well reflected the climate variability at the interannual and interdecadal scales. Copyright (C) 2007 Royal Meteorological Society.
机译:树环宽度已广泛用于环境变化和过去气候的重建研究中。沿着青藏高原边缘,在柴达木盆地东北部的祁连杜松树(Sabina przewalskii Kom。)开发了11种大约800-1500年长的年轮年表。先前的研究表明,用水压力是研究区域树木生长的最大限制因素。为了评估温度和降水变化随时间变化的综合影响,我们使用1955-2002年的气象数据进行了水平衡建模。我们发现,树轮宽度与代表从水平衡模型获得的土壤湿度条件的变量密切相关。具体来说,我们认为实际的蒸散量(AE)代表了用水需求和水分可利用性的综合影响,赤字表示的潜在蒸散量(PE)和AE之间的差异代表了用水压力的严重性,而相对土壤湿度则作为衡量水分利用强度的指标。水分供应。对于某些个别的月度和季节组合,树轮年表解释了回归分析中高达80%的土壤湿度变量变化,这表明过去重建区域土壤湿度条件的潜力很大。在大多数情况下,这些土壤湿度变量的表现优于降水量和Palmer的干旱严重性指数。我们重建了从公元566年到2001年的土壤湿度条件,该条件揭示了主要的干旱和湿润时期,以及最近300年来潮湿状况的总体趋势。通过与该地区的其他代理进行比较,我们得出的结论是,从年轮宽度重建的水分状况很好地反映了年际和年代际尺度的气候变化。皇家气象学会(C)2007。

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