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Published in: Ambio 2/2011

01-03-2011

Governance of Water Resources in the Phase of Change: A Case Study of the Implementation of the EU Water Framework Directive in Sweden

Authors: Monica Hammer, Berit Balfors, Ulla Mörtberg, Mona Petersson, Andrew Quin

Published in: Ambio | Issue 2/2011

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Abstract

In this article, focusing on the ongoing implementation of the EU Water Framework Directive, we analyze some of the opportunities and challenges for a sustainable governance of water resources from an ecosystem management perspective. In the face of uncertainty and change, the ecosystem approach as a holistic and integrated management framework is increasingly recognized. The ongoing implementation of the Water Framework Directive (WFD) could be viewed as a reorganization phase in the process of change in institutional arrangements and ecosystems. In this case study from the Northern Baltic Sea River Basin District, Sweden, we focus in particular on data and information management from a multi-level governance perspective from the local stakeholder to the River Basin level. We apply a document analysis, hydrological mapping, and GIS models to analyze some of the institutional framework created for the implementation of the WFD. The study underlines the importance of institutional arrangements that can handle variability of local situations and trade-offs between solutions and priorities on different hierarchical levels.

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Footnotes
1
Topographic Wetness Index (TWI) can be calculated as ln(α/tanβ) where α is the cumulative upslope area draining through a point and tan β is the slope angle at that point. The index describes the tendency of water to accumulate at any point in a catchment, in terms of α, and the tendency for gravitational forces to move that water downslope, expressed in terms of tan β as an approximate hydraulic gradient (Quinn et al. 1995). Thus, wet areas can arise either from large contributing drainage areas or from very flat slopes, whereas areas with low index values are drier, resulting from either steep slopes or small contributing drainage areas. The relatively coarse DEM (50 m) was interpolated to 5 m using kriging, before calculating TWI. In order to create a smooth surface for enhances visibility, neighborhood statistics was then calculated on the TWI results with a 50 m radius.
 
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Metadata
Title
Governance of Water Resources in the Phase of Change: A Case Study of the Implementation of the EU Water Framework Directive in Sweden
Authors
Monica Hammer
Berit Balfors
Ulla Mörtberg
Mona Petersson
Andrew Quin
Publication date
01-03-2011
Publisher
Springer Netherlands
Published in
Ambio / Issue 2/2011
Print ISSN: 0044-7447
Electronic ISSN: 1654-7209
DOI
https://doi.org/10.1007/s13280-010-0132-2

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