• Energy Research

Abstract Non-perennial streams are widespread, critical to ecosystems and society, and the subject of ongoing policy debate. Prior large-scale research on stream intermittency has been based on long-term averages, generally using annually aggregated data to characterize a highly variable process. As a result, it is not well understood if, how, or why the hydrology of non-perennial streams is changing. Here, we investigate trends and drivers of three intermittency signatures that describe the duration, timing, and dry-down period of stream intermittency across the continental United States (CONUS). Half of gages exhibited a significant trend through time in at least one of the three intermittency signatures, and changes in no-flow duration were most pervasive (41% of gages). Changes in intermittency were substantial for many streams, and 7% of gages exhibited changes in annual no-flow duration exceeding 100 days during the study period. Distinct regional patterns of change were evident, with widespread drying in southern CONUS and wetting in northern CONUS. These patterns are correlated with changes in aridity, though drivers of spatiotemporal variability were diverse across the three intermittency signatures. While the no-flow timing and duration were strongly related to climate, dry-down period was most strongly related to watershed land use and physiography. Our results indicate that non-perennial conditions are increasing in prevalence over much of CONUS and binary classifications of ‘perennial’ and ‘non-perennial’ are not an accurate reflection of this change. Water management and policy should reflect the changing nature and diverse drivers of changing intermittency both today and in the future.

Abstract Climate change is expected to affect hydrologic and thermal regimes of river ecosystems. During dry periods when river flows decrease and water temperatures increase, the hyporheic zone (HZ) can provide a refuge to surface aquatic invertebrates and enhance the resilience capacity of riverine ecosystems. However, shifts from up‐ to downwelling flow conditions in the HZ could jeopardise this capacity. Using laboratory mesocosms and high‐resolution fibre‐optic distributed temperature sensing, we explored the combined effects of five different increased surface water temperature treatments (from 15 to 27°C at 3°C intervals) and the direction of water exchange on the ability of Gammarus pulex (Crustacea: Amphipoda: Gammaridae) to migrate into the HZ as a response to warming. We determined the survival rates of this ubiquitous hyporheic dweller and its rates of consumption of alder (Alnus glutinosa; Betulaceae) leaf litter in the HZ. Results showed that at increasing surface water temperature, leaf‐litter breakdown was observed at a greater depth in the sediments under downwelling flow conditions, that is, G. pulex migrated deeper into the HZ compared with upwelling conditions, resulting in greater survival rates (64 ± 11 vs. 44 ± 10%). However, under both upwelling and downwelling conditions, we found evidence for potential use of the hyporheic zone as a thermal refuge for G. pulex. Below sediment depths of 25 cm, temperatures remained low (<22°C) even when surface waters were at 27°C, so temperatures deep in the hyporheic zone never exceeded critical thermal thresholds for G. pulex. This study provides evidence that alterations to the direction of groundwater–surface water exchange can alter the capacity of the HZ to provide a refuge for benthic invertebrates, thereby affecting the resilience of river communities to warming under climate change.

Key messages from the modelling results of flow intermittence projections under climate change scenarios in the six European river networks studied as part of the H2020 DRYvER project (https://www.dryver.eu/). The dataset contains one global summary fact sheet as well as one fact sheet per studied river network : Albarine (France), Bükkösdi (Hungary), Butiznica (Croatia), Genal (Spain), Lepsämänjoki (Finland), and Velicka (Czechia).

AbstractUnderstanding and predicting how biological communities respond to climate change is critical for assessing biodiversity vulnerability and guiding conservation efforts. Glacier‐ and snow‐fed rivers are one of the most sensitive ecosystems to climate change, and can provide early warning of wider‐scale changes. These rivers are frequently used for hydropower production but there is minimal understanding of how biological communities are influenced by climate change in a context of flow regulation. This study sheds light on this issue by disentangling structural (water temperature preference, taxonomic composition, alpha, beta and gamma diversities) and functional (functional traits, diversity, richness, evenness, dispersion and redundancy) effects of climate change in interaction with flow regulation in the Alps. For this, we compared environmental and aquatic invertebrate data collected in the 1970s and 2010s in regulated and unregulated alpine catchments. We hypothesized a replacement of cold‐adapted species by warming‐tolerant ones, high temporal and spatial turnover in taxa and trait composition, along with reduced taxonomic and functional diversities in consequence of climate change. We expected communities in regulated rivers to respond more drastically due to additive or synergistic effects between flow regulation and climate change. We found divergent structural but convergent functional responses between free‐flowing and regulated catchments. Although cold‐adapted taxa decreased in both of them, greater colonization and spread of thermophilic species was found in the free‐flowing one, resulting in higher spatial and temporal turnover. Since the 1970s, taxonomic diversity increased in the free flowing but decreased in the regulated catchment due to biotic homogenization. Colonization by taxa with new functional strategies (i.e. multivoltine taxa with small body size, resistance forms, aerial dispersion and reproduction by clutches) increased functional diversity but decreased functional redundancy through time. These functional changes could jeopardize the ability of aquatic communities facing intensification of ongoing climate change or new anthropogenic disturbances.

More than half of the global river network is composed of intermittent rivers and ephemeral streams (IRES), which are expanding in response to climate change and increasing water demands. After years of obscurity, the science of IRES has bloomed recently and it is being recognised that IRES support a unique and high biodiversity, provide essential ecosystem services and are functionally part of river networks and groundwater systems. However, they still lack protective and adequate management, thereby jeopardizing water resources at the global scale. This Action brings together hydrologists, biogeochemists, ecologists, modellers, environmental economists, social researchers and stakeholders from 14 different countries to develop a research network for synthesising the fragmented, recent knowledge on IRES, improving our understanding of IRES and translating this into a science-based, sustainable management of river networks. Deliverables will be provided through i) research workshops synthesising and addressing key challenges in IRES science, supporting research exchange and educating young researchers, and ii) researcher-stakeholder workshops translating improved knowledge into tangible tools and guidelines for protecting IRES and raising awareness of their importance and value in societal and decision-maker spheres. This Action is organized within six Working Groups to address: (i) the occurrence, distribution and hydrological trends of IRES; (ii) the effects of flow alterations on IRES functions and services; (iii) the interaction of aquatic and terrestrial biogeochemical processes at catchment scale; (iv) the biomonitoring of the ecological status of IRES; (v) synergies in IRES research at the European scale, data assemblage and sharing; (vi) IRES management and advocacy training.

Data repository for ‘Hydroperiod is a key driver of alpine pond communities along an altitudinal gradient in the French Alps and Pyrenees’ (in prep) Abstract: alpine pond species are particularly vulnerable to the effects of climate change, such as warming, drying and isolation. While the role of temperature and hydroperiod in structuring communities along an altitudinal gradient has been demonstrated in alpine lakes or rivers, very few studies have been conducted in alpine ponds, and the role of hydroperiod is actively debated. To understand which environmental factors structure alpine pond communities, we investigated the relationship between three biotic groups (Odonata, Amphibia and macrophytes) and their environment in 500 ponds in the French Alps and Pyrenees. As predicted, most communities varied along an altitudinal gradient, though not uniformly within the alpine biogeographic region. We also showed that hydroperiod is a key determinant of community variation in alpine ponds common to all geographic zones in the alpine biogeographic area. Finally, we demonstrated that connectivity between ponds should be maintained to conserve alpine specialist communities and mediate the effects of temperature and hydroperiod in the context of climate change. In order to design effective conservation measures for alpine pond communities, further research is needed on the drought resistance of non-permanent pond communities and on the connectivity between alpine ponds.