2020
DOI: 10.1007/s13280-019-01310-x
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High Arctic ecosystem states: Conceptual models of vegetation change to guide long-term monitoring and research

Abstract: Vegetation change has consequences for terrestrial ecosystem structure and functioning and may involve climate feedbacks. Hence, when monitoring ecosystem states and changes thereof, the vegetation is often a primary monitoring target. Here, we summarize current understanding of vegetation change in the High Arctic-the World's most rapidly warming region-in the context of ecosystem monitoring. To foster development of deployable monitoring strategies, we categorize different kinds of drivers (disturbances or s… Show more

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Cited by 31 publications
(34 citation statements)
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References 81 publications
(105 reference statements)
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“…In addition to the short‐term gain of higher plant productivity, we anticipate two other positive warming effects. First, vegetation communities are predicted to change from moss‐dominated, to graminoid‐dominated swards, where the reduction in moss layer reinforces soil warming and mineralization, to further increase productivity (Ravolainen et al, 2020). This process is driven partly by positive feedback mechanisms from the greater density of reindeer (Van der Wal & Brooker, 2004).…”
Section: Discussionmentioning
confidence: 99%
“…In addition to the short‐term gain of higher plant productivity, we anticipate two other positive warming effects. First, vegetation communities are predicted to change from moss‐dominated, to graminoid‐dominated swards, where the reduction in moss layer reinforces soil warming and mineralization, to further increase productivity (Ravolainen et al, 2020). This process is driven partly by positive feedback mechanisms from the greater density of reindeer (Van der Wal & Brooker, 2004).…”
Section: Discussionmentioning
confidence: 99%
“…For example, from south to north, 85 species were found at Alexandra Fiord (Muc et al 1989), 40 in the central part of Ellesmere Island (Lévesque 1997), 75 at Sverdrup Pass (Bergeron andSvoboda 1989), 151 at Quttinirpaaq National Park (Parks Canada 1994), and 36 at Ward Hunt Island (Vincent et al 2011). Part of the variation among surveys likely reflects the size of the surveyed area, as well as environmental conditions and landscape heterogeneity (e.g., topography, hydrology, substrate, and microclimate; Ravolainen et al 2020;Taylor et al 2020).…”
Section: Discussionmentioning
confidence: 99%
“…These ecosystems are expected to be the most impacted by the ongoing climate change due to Arctic amplification, which refers to the greater climatic changes occurring near the North pole compared to the rest of the globe (Smith et al 2019). With the steep climate warming occurring over the last decades (Meehl et al 2007), Arctic regions have already experienced changes in vegetation composition, biomass, and diversity (Elmendorf et al 2012a(Elmendorf et al , 2012bRavolainen et al 2020). Therefore, establishing ecological baselines and updating past inventories are critical scientific endeavors to monitor, predict, and manage current and future impacts of climate change (Mihoub et al 2017).…”
Section: Introductionmentioning
confidence: 99%
“…These include species diversity and composition, phenology, spatial structure, demographics, temporal cycles, health, and productivity and other ecosystem functions and processes. Presented within this issue are complementary approaches to vegetation monitoring, ranging from plotbased measures (Bjorkman et al 2020) to literature and database analyses (Wasowicz et al 2020), conceptual discussions (Ravolainen et al 2020), and pan-Arctic remote sensing derived data analyses (Jenkins et al 2020). Monitoring attributes describing productivity and phenology is Fig.…”
Section: Vegetationmentioning
confidence: 99%