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On the variability of cold region flooding
Stockholm University, Faculty of Science, Department of Physical Geography. Coventry University, UK.
Stockholm University, Faculty of Science, Department of Physical Geography.ORCID iD: 0000-0002-1137-648X
Number of Authors: 3
2016 (English)In: Journal of Hydrology, ISSN 0022-1694, E-ISSN 1879-2707, Vol. 534, 669-679 p.Article in journal (Refereed) Published
Abstract [en]

Cold region hydrological systems exhibit complex interactions with both climate and the cryosphere. Improving knowledge on that complexity is essential to determine drivers of extreme events and to predict changes under altered climate conditions. This is particularly true for cold region flooding where independent shifts in both precipitation and temperature can have significant influence on high flows. This study explores changes in the magnitude and the timing of streamflow in 18 Swedish Sub-Arctic catchments over their full record periods available and a common period (1990–2013). The Mann–Kendall trend test was used to estimate changes in several hydrological signatures (e.g. annual maximum daily flow, mean summer flow, snowmelt onset). Further, trends in the flood frequency were determined by fitting an extreme value type I (Gumbel) distribution to test selected flood percentiles for stationarity using a generalized least squares regression approach.

Results highlight shifts from snowmelt-dominated to rainfall-dominated flow regimes with all significant trends (at the 5% significance level) pointing toward (1) lower magnitudes in the spring flood; (2) earlier flood occurrence; (3) earlier snowmelt onset; and (4) decreasing mean summer flows. Decreasing trends in flood magnitude and mean summer flows suggest widespread permafrost thawing and are supported by increasing trends in annual minimum daily flows. Trends in selected flood percentiles showed an increase in extreme events over the full periods of record (significant for only four catchments), while trends were variable over the common period of data among the catchments. An uncertainty analysis emphasizes that the observed trends are highly sensitive to the period of record considered. As such, no clear overall regional hydrological response pattern could be determined suggesting that catchment response to regionally consistent changes in climatic drivers is strongly influenced by their physical characteristics.

Place, publisher, year, edition, pages
2016. Vol. 534, 669-679 p.
Keyword [en]
flood generation, Sweden Sub-Arctic, trend analysis, Mann-Kendall test, Gumbel distribution
National Category
Oceanography, Hydrology, Water Resources
Identifiers
URN: urn:nbn:se:su:diva-126435DOI: 10.1016/j.jhydrol.2016.01.055ISI: 000371940900054OAI: oai:DiVA.org:su-126435DiVA: diva2:899483
Projects
Swedish Research Council VR (Project Number 2011-4390)Swedish Research Council Formas (Project Number 942-2015-321)Swedish Geological Survey (SGU) (Project Number 60-1626)
Funder
Swedish Research Council, 2011-4390Swedish Research Council Formas, 942-2015-321
Available from: 2016-02-02 Created: 2016-02-02 Last updated: 2016-07-01Bibliographically approved

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Lyon, Steve W.
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