Abstract:[1] Continental freshwater transports and loads excess nutrients and pollutants from various land surface sources into downstream inland and coastal water environments. This study shows that even small, hydrologically unmonitored near-coastal catchment areas may generate large nutrient and pollutant mass loading to the sea of a magnitude similar to or greater than monitored river loads. Systematic near-coastal gaps in the monitoring of freshwater discharges to the sea may therefore mislead the quantification o… Show more
“…In contrast to this need, we found here that the supply of such time series is declining and mostly so in basins where the greatest temperature, and in particular, precipitation changes, are expected. Analogous biases in hydrological monitoring have also been reported for other parts of the world, in studies showing gaps prevailing most in the hotspots of greatest population and other water pollution pressures (Hannerz and Destouni 2006;Destouni et al 2008). Such results converge with the present in indicating an increasing need to identify and prioritize relevant hydrological monitoring for observing climate and environmental change in the Arctic and worldwide.…”
Rapid changes to the Arctic hydrological cycle challenge both our process understanding and our ability to find appropriate adaptation strategies. We have investigated the relevance and accuracy development of climate change projections for assessment of water cycle changes in major Arctic drainage basins. Results show relatively good agreement of climate model projections with observed temperature changes, but high model inaccuracy relative to available observation data for precipitation changes. Direct observations further show systematically larger (smaller) runoff than precipitation increases (decreases). This result is partly attributable to uncertainties and systematic bias in precipitation observations, but still indicates that some of the observed increase in Arctic river runoff is due to water storage changes, for example melting permafrost and/or groundwater storage changes, within the drainage basins. Such causes of runoff change affect sea level, in addition to ocean salinity, and inland water resources, ecosystems, and infrastructure. Process-based hydrological modeling and observations, which can resolve changes in evapotranspiration, and groundwater and permafrost storage at and below river basin scales, are needed in order to accurately interpret and translate climate-driven precipitation changes to changes in freshwater cycling and runoff. In contrast to this need, our results show that the density of Arctic runoff monitoring has become increasingly biased and less relevant by decreasing most and being lowest in river basins with the largest expected climatic changes.
“…In contrast to this need, we found here that the supply of such time series is declining and mostly so in basins where the greatest temperature, and in particular, precipitation changes, are expected. Analogous biases in hydrological monitoring have also been reported for other parts of the world, in studies showing gaps prevailing most in the hotspots of greatest population and other water pollution pressures (Hannerz and Destouni 2006;Destouni et al 2008). Such results converge with the present in indicating an increasing need to identify and prioritize relevant hydrological monitoring for observing climate and environmental change in the Arctic and worldwide.…”
Rapid changes to the Arctic hydrological cycle challenge both our process understanding and our ability to find appropriate adaptation strategies. We have investigated the relevance and accuracy development of climate change projections for assessment of water cycle changes in major Arctic drainage basins. Results show relatively good agreement of climate model projections with observed temperature changes, but high model inaccuracy relative to available observation data for precipitation changes. Direct observations further show systematically larger (smaller) runoff than precipitation increases (decreases). This result is partly attributable to uncertainties and systematic bias in precipitation observations, but still indicates that some of the observed increase in Arctic river runoff is due to water storage changes, for example melting permafrost and/or groundwater storage changes, within the drainage basins. Such causes of runoff change affect sea level, in addition to ocean salinity, and inland water resources, ecosystems, and infrastructure. Process-based hydrological modeling and observations, which can resolve changes in evapotranspiration, and groundwater and permafrost storage at and below river basin scales, are needed in order to accurately interpret and translate climate-driven precipitation changes to changes in freshwater cycling and runoff. In contrast to this need, our results show that the density of Arctic runoff monitoring has become increasingly biased and less relevant by decreasing most and being lowest in river basins with the largest expected climatic changes.
“…Malmström et al, 2004Malmström et al, , 2008Darracq and Destouni, 2007;Cunningham and Fadel, 2007;Jardine, 2008) -the errors of mass transport measurements implied by the chosen measurement methods and the coverage gaps between the chosen measurement points in time and space (e.g. Hannerz and Destouni, 2006;Beven, 2006;Jarsjö and Bayer-Raich, 2008;Destouni et al, 2008) -the chosen model resolutions and possible neglect of potentially important contributing mass transport processes at different scales (e.g. Lindgren and Destouni, 2004;Refsgaard et al, 2006;Destouni et al, 2006;Ganoulis, 2009).…”
Abstract. This paper quantifies and maps the effects of coupled physical and biogeochemical variability on diffuse hydrological mass transport through and from catchments. It further develops a scenario analysis approach and investigates its applicability for handling uncertainties about both physical and biogeochemical variability and their different possible cross-correlation. The approach enables identification of conservative assumptions, uncertainty ranges, as well as pollutant/nutrient release locations and situations for which further investigations are most needed in order to reduce the most important uncertainty effects. The present scenario results provide different statistical and geographic distributions of advective travel times for diffuse hydrological mass transport. The geographic mapping can be used to identify potential hotspot areas with large mass loading to downstream surface and coastal waters, as well as their opposite, potential lowest-impact areas within the catchment. Results for alternative travel time distributions show that neglect or underestimation of the physical advection variability, and in particular of those transport pathways with much shorter than average advective solute travel times, can lead to substantial underestimation of pollutant and nutrient loads to downstream surface and coastal waters. This is particularly true for relatively high catchment-characteristic product of average attenuation rate and average advective travel time, for which mass delivery would be near zero under assumed transport homogeneity but can be orders of magnitude higher for variable transport conditions. A scenario of high advection variability, with a significant fraction of relatively short travel times, combined with a relevant average Correspondence to: K. Persson (klas.persson@natgeo.su.se) biogeochemical mass attenuation rate, emerges consistently from the present results as a generally reasonable, conservative assumption for estimating maximum diffuse mass loading, when the prevailing physical and biogeochemical variability and cross-correlation are uncertain.
“…Such studies are currently hampered by a lack of comprehensive and consistent data on pesticide occurrence in Swedish groundwater, resulting from nationally deficient statutory monitoring of anthropogenic pollutants in groundwater (Destouni et al 2008;Baresel and Destouni 2009). …”
Section: Discussionmentioning
confidence: 99%
“…In order to secure WFD compliance and thereby also future groundwater quality, Sweden further needs to develop and implement statutory regulations enforcing adequate monitoring and assessment of the occurrence of not only pesticides but, as previously noted, also other anthropogenic pollutants (Destouni et al 2008;Baresel and Destouni 2009;European Commission 2012;SEPA 2013) in groundwater nationwide. As for general groundwater quality monitoring and assessment, precepts effectively already exist (e.g.…”
Section: Data and Management Limitations And Requirementsmentioning
confidence: 99%
“…However, to thoroughly assess the character and cause of pesticide pollution of Scanian, and effectively overall Swedish groundwater resources, is challenging due to a nationwide lack of comprehensive and consistent long-term groundwater monitoring data relevant to anthropogenic pollution concerns. This monitoring deficiency has previously been highlighted in relation to nutrient and pollutant loads in coastal areas (Destouni et al 2008), with regards to heavy metal drainage from mining areas (Baresel and Destouni 2009), and more recently in view of general groundwater status and quality assessment in accordance with national environmental objectives and the WFD (European Commission 2012; SEPA 2013). Basically, the national groundwater monitoring network as set up and maintained by the national groundwater authority (SGU; the Geological Survey of Sweden), focuses on areas with minimal human impact to constrain background/reference conditions and does not involve pesticide analyses (Nordberg and Persson 1974;SGU 2013a).…”
Twenty-three south-Swedish public supply wells were studied to assess pesticide pollution of regional groundwater resources. Relations between pesticide occurrence, hydrogeology, and land use were analyzed using Kohonen's Self-Organizing Maps approach. Pesticides are demonstrated to be substantially present in regional groundwater, with detections in 18 wells. Concentrations above the drinking water threshold are confirmed for nine wells. Observations indicate considerable urban influence, and lagged effects of past, less restricted use. Modern, oxic waters from shallow, unconfined, unconsolidated or fracture-type bedrock aquifers appear particularly vulnerable. Least affected waters appear primarily associated with deeper wells, anoxic conditions, and more confined sediment aquifers lacking urban influence. Comprehensive, standardized monitoring of pesticides in groundwater need to be implemented nationwide to enable sound assessments of pollution status and trends, and to develop sound groundwater management plans in accordance with the Water Framework Directive. Further, existing water protection areas and associated regulations need to be reassessed.
scite is a Brooklyn-based organization that helps researchers better discover and understand research articles through Smart Citations–citations that display the context of the citation and describe whether the article provides supporting or contrasting evidence. scite is used by students and researchers from around the world and is funded in part by the National Science Foundation and the National Institute on Drug Abuse of the National Institutes of Health.