Spatiotemporal dynamics of encroaching tall vegetation in timberline ecotone of the Polar Urals Region, Russia

被引:2
|
作者
Zhou, Wenbo [1 ]
Mazepa, Valeriy [5 ]
Shiyatov, Stepan [5 ]
Zhang, Tianqi [4 ]
Liu, Desheng [4 ]
Sheshukov, Aleksey [2 ]
Wang, Jingfeng [3 ]
El Sharif, Husayn [3 ,5 ]
Valeriy, Ivanov [1 ]
Shalaumova, Yulia, V [6 ]
机构
[1] Univ Michigan, Dept Civil & Environm Engn, Ann Arbor, MI 48109 USA
[2] Kansas State Univ, Dept Biol & Agr Engn, Manhattan, KS 66506 USA
[3] Georgia Inst Technol, Sch Civil & Environm Engn, Atlanta, GA 30332 USA
[4] Ohio State Univ, Dept Geog, Columbus, OH 43210 USA
[5] Russian Acad Sci, Ural Branch, Inst Plant & Anim Ecol, Ekaterinburg, Russia
[6] Russian Acad Sci, Ural Branch, Inst Ind Ecol, Lab Math Modeling Ecol & Med, Ekaterinburg, Russia
来源
ENVIRONMENTAL RESEARCH LETTERS | 2022年 / 17卷 / 01期
基金
美国国家科学基金会; 俄罗斯基础研究基金会;
关键词
encroachment; ecotone; patterns; microtopography; snow; ARCTIC CLIMATE-CHANGE; SIBERIAN LARCH; TREE-GROWTH; TUNDRA VEGETATION; SPATIAL-PATTERNS; NORTHERN ALASKA; SHRUB; TEMPERATURE; VARIABILITY; EXPANSION;
D O I
10.1088/1748-9326/ac3694
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Previous studies discovered a spatially heterogeneous expansion of Siberian larch into the tundra of the Polar Urals (Russia). This study reveals that the spatial pattern of encroachment of tree stands is related to environmental factors including topography and snow cover. Structural and allometric characteristics of trees, along with terrain elevation and snow depth were collected along a transect 860 m long and 80 m wide. Terrain curvature indices, as representative properties, were derived across a range of scales in order to characterize microtopography. A density-based clustering method was used here to analyze the spatial and temporal patterns of tree stems distribution. Results of the topographic analysis suggest that trees tend to cluster in areas with convex surfaces. The clustering analysis also indicates that the patterns of tree locations are linked to snow distribution. Records from the earliest campaign in 1960 show that trees lived mainly at the middle and bottom of the transect across the areas of high snow depth. As trees expanded uphill following a warming climate trend in recent decades, the high snow depth areas also shifted upward creating favorable conditions for recent tree growth at locations that were previously covered with heavy snow. The identified landscape signatures of increasing tall vegetation, and the effects of microtopography and snow may facilitate the understanding of treeline dynamics at larger scales.
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页数:13
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