首页> 外文期刊>Tree-Ring Research >Growth-climate relationships of Pinus strobus in the floodway versus terrace forest along the banks of the Red Cedar River, Michigan.
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Growth-climate relationships of Pinus strobus in the floodway versus terrace forest along the banks of the Red Cedar River, Michigan.

机译:密歇根州红雪松河两岸的河道松花Pin与梯田林的生长气候关系。

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We examined the effects of climate (i.e. temperature, precipitation, moisture index, river discharge) on the radial growth of eastern white pine (Pinus strobus) in two contrasting microhabitats (floodway versus terrace) in relation to an elevational and moisture gradient along the banks of the Red Cedar River, Michigan. We hypothesized that trees growing on the terrace sites would have a greater sensitivity to climatic factors than trees growing in the floodway. Increment cores were sampled and crossdated from dominant and co-dominant trees in the floodway and terrace sites and standardized growth chronologies were developed. Mean sensitivity, standard deviation, percentage of absent rings, and intertree correlation were generally greater for eastern white pine on the terrace compared to the floodway forests. Dendroclimatic relationships were examined with bootstrapped correlation analysis, which indicated that radial growth of eastern white pine in both floodway and terrace sites was negatively associated with summer temperature (i.e. June and July) of the current growing season. Radial growth in both floodway and terrace sites were positively related to current May precipitation, moisture index, and river discharge. Dendroclimatic response of eastern white pine in floodway and terrace sites differed in that the effect of summer moisture stress was more persistent in the terrace sites into later summer (i.e. current July) whereas floodway sites showed a negative response to prior-year May precipitation and moisture index. Although precipitation and hydrological conditions of the river were generally favorable during the summer months, which appeared to have promoted soil moisture recharge, flooding in early winter (i.e. prior November) had a negative impact on growth in both microhabitats. The effect of winter river discharge was significantly negative in January (t) in the floodway sites compared to the terrace sites.Digital Object Identifier http://dx.doi.org/10.3959/1536-1098-69.2.37
机译:我们研究了气候(即温度,降水,湿度指数,河流流量)对两个相反的微生境(水道与阶地)相对于沿岸的海拔和湿度梯度的东部白松(Pinus strobus)径向生长的影响密歇根州红雪松河的全景。我们假设在梯田上生长的树木比在洪水道上生长的树木对气候因素的敏感性更高。对增量核心进行了采样,并与洪水道和梯田地点的优势树和共同优势树进行了交叉,并制定了标准化的生长时间顺序。与梯级林相比,阶地上东部白松的平均敏感性,标准偏差,无环百分比和树间相关性通常更大。用自举相关分析检查了树状气候关系,这表明洪水道和阶地的东部白松径向生长与当前生长季节的夏季温度(即六月和七月)呈负相关。洪水道和阶地的径向生长与当前的5月降水,湿度指数和河流流量成正相关。洪水道和阶地中东部白松的树状气候响应不同,在于阶地中夏季水分胁迫的影响在夏末(即当前的7月)更为持久,而洪水道对上年5月的降水和水分表现出负响应。指数。尽管在夏季,河流的降水和水文条件总体上是有利的,这似乎促进了土壤水分的补给,但冬季初(11月之前)的洪水对这两个微生境的生长都产生了负面影响。与梯田地点相比,洪水河道地点的冬季河水排放在1月(t)显着为负。数字对象标识符http://dx.doi.org/10.3959/1536-1098-69.2.37

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