Ecosystem change and stability over multiple decades in the Swedish subarctic: complex processes and multiple drivers

Author:

Callaghan Terry V12,Jonasson Christer13,Thierfelder Tomas4,Yang Zhenlin12,Hedenås Henrik5,Johansson Margareta16,Molau Ulf78,Van Bogaert Rik9,Michelsen Anders10,Olofsson Johan11,Gwynn-Jones Dylan12,Bokhorst Stef5,Phoenix Gareth2,Bjerke Jarle W.13,Tømmervik Hans13,Christensen Torben R.614,Hanna Edward15,Koller Eva K.216,Sloan Victoria L.217

Affiliation:

1. Royal Swedish Academy of Sciences, PO Box 500 05, Stockholm 104 05, Sweden

2. Department of Animal and Plant Sciences, University of Sheffield, Sheffield S10 2TN, UK

3. Polar Research Secretariat, Lilla Frescativägen 4A, Stockholm 114 18, Sweden

4. Swedish University of Agricultural Sciences, Uppsala 750 07, Sweden

5. Department of Forest Resource Management, Swedish University of Agricultural Sciences, Umeå 901 83, Sweden

6. Department of Physical Geography and Ecosystem Science, Lund University, Lund 22362, Sweden

7. Department of Biological and Environmental Sciences, University of Gothenburg, Gothenburg 40530, Sweden

8. Stockholm Resilience Centre, Stockholm University, Kräftriket 2B, Stockholm

9. Natural Resources Canada, Canadian Forest Service, Canada

10. Center for Permafrost (CENPERM), University of Copenhagen, Øster Voldgade 10, 1350 K, Denmark

11. Department of Ecology and Environmental Science, Umeå University, Umeå 901 87, Sweden

12. Aberystwyth University, Aberystwyth, UK

13. Norwegian Institute for Nature Research, FRAM – High North Research Centre for Climate and the Environment, Tromsø 9296, Norway

14. Greenland Climate Research Centre, Nuuk, Greenland

15. Department of Geography, University of Sheffield, Sheffield S10 2TN, UK

16. School of Environment, Natural Resources and Geography, Bangor University, Bangor LL57 2UW, Wales, UK

17. Oak Ridge National Laboratory, Environmental Sciences Division, Oak Ridge, TN, USA

Abstract

The subarctic environment of northernmost Sweden has changed over the past century, particularly elements of climate and cryosphere. This paper presents a unique geo-referenced record of environmental and ecosystem observations from the area since 1913. Abiotic changes have been substantial. Vegetation changes include not only increases in growth and range extension but also counterintuitive decreases, and stability: all three possible responses. Changes in species composition within the major plant communities have ranged between almost no changes to almost a 50 per cent increase in the number of species. Changes in plant species abundance also vary with particularly large increases in trees and shrubs (up to 600%). There has been an increase in abundance of aspen and large changes in other plant communities responding to wetland area increases resulting from permafrost thaw. Populations of herbivores have responded to varying management practices and climate regimes, particularly changing snow conditions. While it is difficult to generalize and scale-up the site-specific changes in ecosystems, this very site-specificity, combined with projections of change, is of immediate relevance to local stakeholders who need to adapt to new opportunities and to respond to challenges. Furthermore, the relatively small area and its unique datasets are a microcosm of the complexity of Arctic landscapes in transition that remains to be documented.

Publisher

The Royal Society

Subject

General Agricultural and Biological Sciences,General Biochemistry, Genetics and Molecular Biology

Reference170 articles.

1. AMAP. 2011 Snow water ice and permafrost in the Arctic (SWIPA): climate change and the cryosphere. Arctic monitoring and assessment programme (AMAP) Oslo Norway.

2. Ecological Dynamics Across the Arctic Associated with Recent Climate Change

3. Circumpolar Arctic Tundra Vegetation Change Is Linked to Sea Ice Decline

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