The Science of The Total Environment, Journal Year: 2016, Volume and Issue: 574, P. 272 - 281
Published: Oct. 14, 2016
Language: Английский
The Science of The Total Environment, Journal Year: 2016, Volume and Issue: 574, P. 272 - 281
Published: Oct. 14, 2016
Language: Английский
Earth-Science Reviews, Journal Year: 2014, Volume and Issue: 138, P. 313 - 334
Published: June 27, 2014
Language: Английский
Citations
292Journal of Hydrology, Journal Year: 2020, Volume and Issue: 589, P. 125163 - 125163
Published: June 12, 2020
Language: Английский
Citations
209The Science of The Total Environment, Journal Year: 2018, Volume and Issue: 640-641, P. 1548 - 1565
Published: June 18, 2018
Language: Английский
Citations
179Wiley Interdisciplinary Reviews Water, Journal Year: 2024, Volume and Issue: 11(4)
Published: March 5, 2024
Abstract Rising water temperatures in rivers due to climate change are already having observable impacts on river ecosystems. Warming has both direct and indirect aquatic life, further aggravates pervasive issues such as eutrophication, pollution, the spread of disease. Animals can survive higher through physiological and/or genetic acclimation, behavioral phenological change, range shifts more suitable locations. As such, those animals that adapted cool‐water regions typically found high altitudes latitudes where there fewer dispersal opportunities most at risk future extinction. However, sub‐lethal animal physiology phenology, body‐size, trophic interactions could have significant population‐level effects elsewhere. Rivers vulnerable warming because historic management left them exposed solar radiation removal riparian shade, hydrologically disconnected longitudinally, laterally, vertically. The resilience riverine ecosystems is also limited by anthropogenic simplification habitats, with implications for resource use resident organisms. Due complex ecosystems, species‐specific response organisms warming, predicting how will challenging. Restoring provide connectivity heterogeneity conditions would a expected co‐occurring pressures, including should be considered priority part global strategies adaptation mitigation. This article categorized under: Science Water > Environmental Change Life Nature Freshwater Ecosystems Stresses Pressures
Language: Английский
Citations
32Water Resources Research, Journal Year: 2014, Volume and Issue: 50(4), P. 3253 - 3274
Published: March 27, 2014
Abstract Cold groundwater discharge to streams and rivers can provide critical thermal refuge for threatened salmonids other aquatic species during warm summer periods. Climate change may influence temperature flow rates, which in turn impact riverine ecosystems. This study evaluates the potential of climate on timing, magnitude, from small, unconfined aquifers that undergo seasonal freezing thawing. Seven downscaled scenarios 2046–2065 were utilized drive surficial water energy balance models (HELP3 ForHyM2) obtain future projections daily ground surface recharge. These conditions then applied as boundary subsurface simulations variably saturated transport. The performed with U.S. Geological Survey finite element model SUTRA was recently modified include dynamic freeze‐thaw process. indicate a rise magnitude (up 34%) 3.6°C) adjacent river months due projected increases air precipitation. response is shown be strongly dependent aquifer dimensions. Thus, demonstrate sensitivity baseflow‐dominated decadal more complex than previously thought. Furthermore, results probability exceeding thresholds within groundwater‐sourced refugia significantly increase under most extreme scenarios.
Language: Английский
Citations
168Fungal ecology, Journal Year: 2015, Volume and Issue: 19, P. 190 - 200
Published: Aug. 1, 2015
Language: Английский
Citations
126Hydrology and earth system sciences, Journal Year: 2015, Volume and Issue: 19(5), P. 2469 - 2489
Published: May 26, 2015
Abstract. Climate change is expected to increase stream temperatures and the projected warming may alter spatial extent of habitat for cold-water fish other aquatic taxa. Recent studies have proposed that thermal sensitivities, derived from short-term air temperature variations, can be employed infer future due long-term climate change. However, this approach does not consider potential streambed heat fluxes gradual shallow subsurface. The groundwater particularly important regimes groundwater-dominated streams rivers. Also, recent investigated how land surface perturbations, such as wildfires or timber harvesting, influence by changing fluxes, but these typically considered disturbances also fluxes. In study, several analytical solutions one-dimensional unsteady advection–diffusion equation subsurface transport are estimate timing magnitude changes seasonal variability in temperatures. Groundwater sensitivity formulae accommodate different scenarios. suggest will warm response depends on rate warming, properties, bulk aquifer depth, velocity. results emphasize difference between (e.g., seasonal) multi-decadal) surface-temperature variability, thus demonstrate limitations using water records project warming. Suggestions provided implementing models
Language: Английский
Citations
107Journal of Hydrology, Journal Year: 2017, Volume and Issue: 563, P. 1169 - 1180
Published: Sept. 15, 2017
Language: Английский
Citations
101Environmental Research Letters, Journal Year: 2017, Volume and Issue: 12(3), P. 034005 - 034005
Published: Feb. 10, 2017
Only meters below our feet, shallow aquifers serve as sustainable energy source and provide freshwater storage ecological habitats. All of these aspects are crucially impacted by the thermal regime subsurface. Due to limited accessibility however, temperature measurements scarce. Most commonly, groundwater temperatures approximated adding an offset annual mean surface air temperatures. Yet, value this is not well defined, often arbitrarily set, rarely validated. Here, we propose usage satellite-derived land instead 2 548 measurement points in 29 countries compiled, revealing characteristic trends between Here it shown that evapotranspiration snow cover impact on globally, through latent heat flow insulation. Considering two processes only, global estimated a resolution approximately 1 km × km. When comparing with measured ones coefficient determination 0.95 root square error 1.4 K found.
Language: Английский
Citations
90Journal of Hydrology X, Journal Year: 2020, Volume and Issue: 11, P. 100071 - 100071
Published: Dec. 28, 2020
Climate change will have both quantitative and qualitative effects on groundwater resources. These impacts differ for aquifers in solid unconsolidated rock, urban or rural locations, the principal processes of recharge. Having knowledge about intrinsic key parameters (aquifer geometries, storage properties, renewal rates, residence times, etc.), recharge processes, temperature imprinting makes it possible to compare forecast sensitivity individual climate change. The future development selected projections was qualitatively investigated representative Swiss rock resources Central Plateau as well Jura Alpine region. For non-urban areas, is expected a strong overall impact temperatures. In however, direct anthropogenic influences are likely dominate. Increased thermal subsurface use waste heat from underground structures, adaptation strategies mitigate global warming, increase Likewise, measurements city Basel show that temperatures increased by an average 3.0 ± 0.7 °C period 1993 2016, they can exceed 18 °C, especially densely urbanized areas. Similarly, regarding shallow with low saturated zone thicknesses, such Davos (Canton Grisons), strongly be influenced changes regimes. contrast, within deep large Biel/Bienne Bern), some cases distances land surface table extended unsaturated zones, Winterthur Zurich), attenuated only over long time periods. context presented research we hypothesized associated primarily determined infiltrating waters (i.e. "river-fed aquifers"). We seasonal shifts could important factor affecting Moreover, interaction during high runoff periods influence Accordingly, "business usual" scenario end century, shift precipitation river flood events summer winter months accompanied comparatively cool seasons, which would tendency "cool down"
Language: Английский
Citations
79