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Smaller future floods imply less habitat for riparian plants along a boreal river
Umeå universitet, Teknisk-naturvetenskapliga fakulteten, Institutionen för ekologi, miljö och geovetenskap. (Arcum)
Umeå universitet, Teknisk-naturvetenskapliga fakulteten, Institutionen för ekologi, miljö och geovetenskap.
Umeå universitet, Teknisk-naturvetenskapliga fakulteten, Institutionen för ekologi, miljö och geovetenskap. (Arcum)
2019 (engelsk)Inngår i: Ecological Applications, ISSN 1051-0761, E-ISSN 1939-5582, Vol. 29, nr 8, artikkel-id e01977Artikkel i tidsskrift (Fagfellevurdert) Published
Abstract [en]

Climate-change projections suggest large changes in riverine flow regime, which will likely alter riparian communities. In northern Europe, forecasts propose lower annual spring flood peaks and higher winter flows, resulting in narrower riparian zones. To estimate the impact of climate change on habitat extent of riparian plants, we developed a framework estimating the sensitivity and exposure of individual species to streamflow change, and surveyed five reaches along the free-flowing Vindel River in northern Sweden. We modeled the hydrologic niche of riparian plant species based on the probability of occurrence along gradients of flood frequency and duration and used predicted future water-level fluctuations (based on climate models and IPCC emission scenarios) to calculate changes in flow-related habitat availability of individual species. Despite projected increases in runoff, we predict most species to decrease in riparian elevational extent by on average 12-29% until the end of the century, depending on scenario. Species growing in the upper, spring-flood-controlled part of the riparian zone will likely lose most habitat, with the largest reductions in species with narrow ranges of inundation duration tolerance (decreases of up to 54%). In contrast, the elevational extent of most amphibious species is predicted to increase, but conditions creating isoetid vegetation will become rarer or disappear: isoetid vegetation is presently found in areas where ice formed in the fall settles on the riverbank during the winter as water levels subside. Higher winter flows will make these conditions rare. We argue that our framework is useful to project the effects of hydrologic change caused by climate change as well as other stressors such as flow regulation also in other regions. With few rivers remaining unaffected by dams and other human stressors, these results call for monitoring to detect species declines. Management to alleviate species losses might include mitigation of habitat degradation from land-use activities, more environmentally friendly flow schemes, and more intensive management options such as mowing riparian meadows no longer regularly maintained by recurrent floods.

sted, utgiver, år, opplag, sider
John Wiley & Sons, 2019. Vol. 29, nr 8, artikkel-id e01977
Emneord [en]
climate change, flooding, inundation, niche width, riverbanks, river, water table
HSV kategori
Identifikatorer
URN: urn:nbn:se:umu:diva-162858DOI: 10.1002/eap.1977ISI: 000481122800001PubMedID: 31323161Scopus ID: 2-s2.0-85070303264OAI: oai:DiVA.org:umu-162858DiVA, id: diva2:1349123
Tilgjengelig fra: 2019-09-06 Laget: 2019-09-06 Sist oppdatert: 2021-06-16bibliografisk kontrollert

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Jansson, RolandStröm, LottaNilsson, Christer

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