Tree-ring width and maximum latewood density at the North American tree line: parameters of climatic change
Tree-ring width and maximum latewood density at the North American tree line: parameters of climatic change
复制标题
DOI:
10.1139/x92-171
复制
发表时间:
1992-09
影响因子:
2.2
通讯作者:
R. D’Arrigo;G. Jacoby;R. Free
中科院分区:
文献类型:
--
作者:
R. D’Arrigo;G. Jacoby;R. Free
In remote subarctic North America, instrumental records are very short and sparsely distributed. Yet a long-term understanding of subarctic climate is critical to studies of global change. Annual tree-ring width and maximum latewood density are complementary, high-resolution parameters with different environmental and physiological controls that can be used to assess recent centuries of climatic change. In this paper we present a comparison of the different temperature information inferred from these parameters for white spruce (Piceaglauca (Moench) Voss), a dominant North American latitudinal tree line species. Ring-width and maximum latewood density chronologies (with a common period from 1720–1977) are shown for five sites along a widely spaced transect of the forest–tundra transition in northern Canada. The positive temperature response of maximum latewood density to year to year local temperatures is more consistent and covers a longer portion of the growing season than does that of ring width. Unlik...