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黄河流域两类取样环境的树木年轮生长量订正分析 总被引:2,自引:0,他引:2
黄河流域存在着两类不同的树木年轮取样环境。在典型的取样环境中,树木生长多遵循缓慢递减的规律,作生长量订正时,可采用传统的树木年轮学订正方法。在非典型的取样环境中,树木生长形式较为复杂,可引进新的分析途径,包括多项式函数和样条函数的应用。随样本环境的不同,各类订正分析的可适用性亦有差异。 相似文献
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样条函数拟合在年轮气候学分析中的可适用性 总被引:4,自引:0,他引:4
在树木年轮气候学分析中,应消除树木生长受遗传因子控制的缓慢生长趋势,进行生长量订正,使得年轮宽度序列转变成表征局地气候变化的指数序列。目前,最为广泛采用的是带尾的指数函数拟合方法,这在我国许多典型取样环境的年轮分析中,亦被证实是十分有效的。随着树木年轮取样的多样化,对非典型取样环境的样本,则必须采用较复杂的、多种函数形式进行订正,样条函数为其中之一。样条函数方法的应用现仍有争议,尤其是它的可适用性尚待更多资料论证。本文根据我国年轮样 相似文献
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RECONSTRUCTING MIDDLE-TIBET CLIMATE DURING THE LAST 600 YEARS BY DENDROCLIMATOLOGICAL METHOD 下载免费PDF全文
Based on four tree-ring chronologies which was analyscd with appropriate collection and accurate datingin the middle Tibetan Plateau,an essential procedure on reconstruction of past climate has been pointed outin this paper.First,the response function of each dendrochronology has been built and used to estimate howring-width growth responds to variations in monthly climatic change.Second,the climate factors which couldbe produced with different tree-ring series have been selected.Then,the transfer function equation,includinga new set of orthogonal variables,can be used to reconstruct local past temperature or precipitation.Itshould be emphasized that prior growth has been considered in the relationship between climate factor andtree-ring chronology,Besides,some different periods for calibration and verification have been divided.Andsome statistics and other kinds of proxy data have been adopted as test approaches.As a result,the variationsof air temperature during the last 600 years and precipitation during the last 340 years were reconstructedby combining the same types of tree-ring series in the middle Tibet. 相似文献
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