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Anders Wörman
Researcher at Royal Institute of Technology
Publications - 119
Citations - 3742
Anders Wörman is an academic researcher from Royal Institute of Technology. The author has contributed to research in topics: Groundwater & Hyporheic zone. The author has an hindex of 28, co-authored 109 publications receiving 3145 citations. Previous affiliations of Anders Wörman include Vattenfall & Swedish University of Agricultural Sciences.
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Journal ArticleDOI
Hyporheic flow and transport processes: Mechanisms, models, and biogeochemical implications
Fulvio Boano,Judson W. Harvey,Andrea Marion,Aaron I. Packman,Roberto Revelli,Luca Ridolfi,Anders Wörman +6 more
TL;DR: In this paper, a review summarizes results from modeling studies and field observations about flow and transport processes in the hyporheic zone and describes the theories proposed in hydrology and fluid dynamics developed to quantitatively model and predict the hypheic transport of water, heat, and dissolved and suspended compounds from sediment grain scale up to watershed scale.
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How old is streamwater? Open questions in catchment transit time conceptualization, modelling and analysis
Jeffrey J. McDonnell,Jeffrey J. McDonnell,Kevin J. McGuire,Pradeep K. Aggarwal,Keith Beven,Daniela Biondi,Georgia Destouni,Sarah M. Dunn,April L. James,James W. Kirchner,Philipp Kraft,Steve W. Lyon,P. Maloszewski,B. Newman,Laurent Pfister,Andrea Rinaldo,Allan Rodhe,Takahiro Sayama,Jan Seibert,K. Solomon,Chris Soulsby,Michael K. Stewart,Doerthe Tetzlaff,C. Tobin,Peter Troch,Markus Weiler,Andrew W. Western,Anders Wörman,Sebastian Wrede +28 more
TL;DR: The time water spends travelling subsurface through a catchment to the stream network (i.e., the catchment water transit time) fundamentally describes the storage, flow pathway heterogeneity and sou...
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Effect of flow‐induced exchange in hyporheic zones on longitudinal transport of solutes in streams and rivers
TL;DR: In this article, temporary storage of solutes in streams is often controlled by flow-induced uptake in hyporheic zones, which accounts for the tails that are generally observed following the passage of a stream.
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A multiscale model for integrating hyporheic exchange from ripples to meanders
TL;DR: In this article, a spectral scaling approach is employed as the basis for a generalized analysis of topography-induced stream-subsurface exchange at the bed-form-to-reach scale using readily measurable system characteristics.
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Fractal topography and subsurface water flows from fluvial bedforms to the continental shield
TL;DR: In this paper, surface-subsurface flow interactions are critical to a wide range of geochemical and ecological processes and to the fate of contaminants in freshwater environments and Fractal scaling relationships are analyzed.