Climate Change and Future Position of Arctic Tree Line

Author(s):  
Peter A. Scott ◽  
Claude Lavoie ◽  
Glen M. MacDonald ◽  
Bjartmar Sveinbjörnsson ◽  
Ross W. Wein
2015 ◽  
Vol 25 (3) ◽  
pp. 263-273 ◽  
Author(s):  
Aitor Ameztegui ◽  
Lluís Coll ◽  
Lluís Brotons ◽  
Josep M. Ninot

2020 ◽  
Vol 10 (1) ◽  
Author(s):  
Bikram Shrestha ◽  
Pavel Kindlmann

AbstractThe snow leopard is one of the most endangered large mammals. Its population, already low, is declining, most likely due to the consequences of human activity, including a reduction in the size and number of suitable habitats. With climate change, habitat loss may escalate, because of an upward shift in the tree line and concomitant loss of the alpine zone, where the snow leopard lives. Migration between suitable areas, therefore, is important because a decline in abundance in these areas may result in inbreeding, fragmentation of populations, reduction in genetic variation due to habitat fragmentation, loss of connectivity, bottlenecks or genetic drift. Here we use our data collected in Nepal to determine the areas suitable for snow leopards, by using habitat suitability maps, and describe the genetic structure of the snow leopard within and between these areas. We also determine the influence of landscape features on the genetic structure of its populations and reveal corridors connecting suitable areas. We conclude that it is necessary to protect these natural corridors to maintain the possibility of snow leopards’ migration between suitable areas, which will enable gene flow between the diminishing populations and thus maintain a viable metapopulation of snow leopards.


2002 ◽  
Vol 90 (4) ◽  
pp. 537-544 ◽  
Author(s):  
J. GRACE

2012 ◽  
Vol 30 (2) ◽  
pp. 121-126 ◽  
Author(s):  
Xiaohua Gou ◽  
Fen Zhang ◽  
Yang Deng ◽  
Gregory J. Ettl ◽  
Meixue Yang ◽  
...  

2013 ◽  
Vol 80 (2) ◽  
pp. 180-188 ◽  
Author(s):  
Louis A. Scuderi ◽  
Peter J. Fawcett

Development of an accurate chronology for glacial deposits in the Sierra Nevada has long been problematic given the lack of suitable organic material for radiocarbon dating. Lichenometry initially appeared promising as ages showed an increase from cirque headwalls to down-canyon moraines. However, while Recess Peak lichen age estimates range from 2 to 3 ka, recent work shows these deposits to be at least 10 ka older. Here, we present evidence for a late Holocene reset of Recess Peak lichen ages by significant post-depositional climate change. Following late-Pleistocene deposition of Recess Peak moraines, warming through the mid-Holocene allowed forests to advance into shallow basins eliminating local inverted tree lines. This produced a partial canopy where shading killed the original post-Pleistocene crustose lichen colonies. Late-Holocene cooling resulted in forest retreat from these basins as alpine tree line fell. Lichens then recolonized the re-exposed Recess Peak deposits. We conclude that while Recess Peak lichen ages are accurate to within the dating uncertainty of the technique, existing lichen ages actually date the timing of post-mid-Holocene cooling and recolonization, and not the original emplacement of these deposits. Thus, applications of Lichenometry should consider post-depositional environmental change when interpreting the meaning of these dates.


Trees ◽  
2009 ◽  
Vol 23 (6) ◽  
pp. 1321-1329 ◽  
Author(s):  
Keyan Fang ◽  
Xiaohua Gou ◽  
Fahu Chen ◽  
Jianfeng Peng ◽  
Rosanne D’Arrigo ◽  
...  

Ecosystems ◽  
2010 ◽  
Vol 13 (3) ◽  
pp. 393-409 ◽  
Author(s):  
Nina S. Reuss ◽  
Dan Hammarlund ◽  
Mats Rundgren ◽  
Ulf Segerström ◽  
Lars Eriksson ◽  
...  

Forests ◽  
2020 ◽  
Vol 11 (9) ◽  
pp. 985
Author(s):  
Athanasios Zindros ◽  
Kalliopi Radoglou ◽  
Elias Milios ◽  
Kyriaki Kitikidou

One of the effects of climate change is, among others, changes to forest ecosystems. Research Highlights: Temperature increases and upward tree line shifts are linked in many studies. However, the impact of climate change on tree lines has not been studied in Greece. Background and Objectives: The aim of this study is to assess the relation of tree line shifts and climate change in Olympus mountain, and especially in a protected area. Materials and Methods: In the Olympus mountain, which includes a protected area (the Olympus National Park core) since 1938, GIS data regarding forest cover were analyzed, while climate change from a previous study is presented. Results: Forest expansion and an upward tree line shift are proven in the Olympus mountain area. In the National Park core, the tree line shift is the result of climate change and attributed to the significant temperature increase in the growing season. Conclusions: There are strong indications that a temperature increase leads to an upward shift of the tree lines in the National Park core.


2012 ◽  
Vol 28 ◽  
pp. 1-18 ◽  
Author(s):  
Erich Szerencsits

Mountain timber lines are relevant in the context of land abandonment and climate change. For Switzerland, GIS-compliant delimitations of the tree line and the forest line are still lacking. Recent high-resolution landcover information offers new possibilities for GIS-based approaches. In a Swiss-wide study, an analysis based on slope zones was combined with a moving-window analysis to assess tree and forest line altitude, using topographic data. The tree and the forest lines were delimited at the upper altitude reached by a tree or closed forest respectively. The model delivered a fine-scaled delimitation sensitive to local conditions. The results indicate that earlier studies underestimated the tree line altitudes for the fringes of the Alps. Also the variability inside climatic and bio-geographical regions is larger than it was estimated up to now.


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