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Climatic Factors for Limiting Northward Distribution of Eight Temperate Tree Species in Eastern North America

机译:限制北美东部八种温带树种向北分布的气候因素

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Eight temperate deciduous tree species, Acer rubrum L. , A. saccharinum L. , A. saccharum Marsh., Belluta alleghaniensis Britton. , Fraxinus nigra Marsh., Quercus rubra L. , Titia americana L., and Ulmus americana L. in eastern North America, were selected to explore relationship between the northward distribution of temperate tree species and climatic factors. For each species, more than 30 sites at their north limits of distribution were obtained from their distribution maps, and 11 climatic indices at the north limits were computed. The standardized standard deviation (SD) method, which compares the magnitude of variance of climatic indices, was used to detect which climatic parameter was the most important for explaining northward distribution of these species. We presume that the climatic parameter that has the smallest variance at the north limit would be assigned as the dominant climatic factor for limiting the distribution of this species. The results derived from the standardized SD method indicated that the SD value of warmth index (WI) and/or annual biotemperature (ABT) were the smallest among the 11 climatic indices. Since both WI and ABT represent growing season temperature, it suggested that growing season temperature was the most important climatic factor for explaining the northward distribution of these temperate tree species. The relationships between several climatic indices, WI, coldness index (CI) , annual precipitation (AP) , annual range of temperature (ART) and humid/arid index were also analyzed. As a result, at the north limits of all these species, both WI and CI decreased with an increase of AP, and CI increased with an increase of ART. Besides growing season temperature, precipitation and climatic continentality also have influence on the northward distribution of the temperate trees in eastern North America.
机译:八种温带落叶乔木树种,宏A,糖精,湿地沼泽,百里香aleghaniensis布里顿。选择北美东部的白蜡树,黑曲霉沼泽,栎栎,美洲斑Ti和美洲榆树,探讨温带树种向北分布与气候因子之间的关系。对于每个物种,从其分布图获得了北分布的30多个站点,并计算了北边界的11个气候指数。通过比较气候指数方差幅度的标准化标准差(SD)方法,可以确定哪种气候参数对于解释这些物种的北向分布最为重要。我们假设在北限具有最小变化的气候参数将被指定为限制该物种分布的主要气候因素。标准化SD方法得出的结果表明,在11个气候指数中,温暖指数(WI)和/或年度生物温度(ABT)的SD值最小。由于WI和ABT均代表生长季节的温度,因此表明生长季节的温度是解释这些温带树种向北分布的最重要的气候因素。还分析了几个气候指数,WI,寒冷指数(CI),年降水量(AP),年温度范围(ART)和湿度/干旱指数之间的关系。结果,在所有这些物种的北限,WI和CI均随着AP的增加而降低,CI随ART的增加而增加。除了生长季节的温度外,降水和气候大陆性因素还影响着北美东部温带树木的北向分布。

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