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The effect of climate on the net primary productivity (NPP) of Pinus koraiensis in the Changbai Mountains over the past 50 years

机译:近50年来气候变化对长白山红松净初级生产力的影响

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This study investigated the relationship between climate and Pinus koraiensis net primary productivity (NPP) (estimated using tree-ring widths) and the effect of climate on NPP in the Changbai Mountains. Three typical areas of Pinus koraiensis and a broad-leaved mixed forest were investigated and sampled. NPP was estimated using biomass equations and the annual diameter at breast height, calculated from tree-ring widths. A stepwise regression was used for the quantitative analysis of the response of NPP to climate variation, whereas correlation and response analyses were used to illustrate the relationship between the climatic variables and NPP. The results showed that between 1960 and 2012, the biomass of sampled Pinus koraiensis in the Changbai Mountains almost doubled, from 107.70 to 205.29 t ha(-1). The NPP of Pinus koraiensis varied steadily within a confined range over the past 52 years, with an average of 1.88 t ha(-1) year(-1). In this study, it was deduced that NPP was simultaneously affected by temperature and precipitation. The minimum temperature in April and the precipitation in June and July, which most affected the changes in NPP, could explain 28.4 % of the NPP variance. The extreme values of these principal climatic controls corresponded well with extreme NPP values. However, an increase in NPP caused by recent warming prior to the growing season might have been offset by a decrease in summer precipitation. Furthermore, the effect of temperature change on NPP was complex. An increase in monthly low temperatures induced by warming acted to increase NPP, while the monthly high temperatures during the growing season had a negative impact on NPP for the drought.
机译:本研究调查了长白山气候与红松净初级生产力(NPP)(用树轮宽度估计)之间的关系以及气候对NPP的影响。调查并采样了红松和阔叶混交林的三个典型区域。使用生物量方程式和根据树木年轮宽度计算的乳房高度年直径来估算NPP。逐步回归用于定量分析NPP对气候变化的响应,而相关和响应分析则用于说明气候变量与NPP之间的关系。结果表明,从1960年到2012年,长白山采样的红松生物量几乎翻了一番,从107.70 t到205.29 t ha(-1)。在过去的52年中,红松的NPP一直在一个狭窄的范围内稳定变化,平均为1.88 t ha(-1)年(-1)。在这项研究中,推论出NPP同时受到温度和降水的影响。 4月的最低温度和6月和7月的降水量对NPP的变化影响最大,可以解释28.4%的NPP变化。这些主要气候控制的极值与极端NPP值非常吻合。但是,由于生长期之前的最近变暖导致的NPP的增加可能已被夏季降水的减少所抵消。此外,温度变化对NPP的影响是复杂的。变暖引起的每月低温升高增加了NPP,而生长期期间的每月高温对干旱对NPP产生了负面影响。

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