>Magister Scientiae - MSc / The occurrence of droughts is a threat to global water resources and natural ecosystems, with the impact being more profound in semi-arid environments. The frequency of droughts is likely to increase because of climate change, and this poses a huge threat to the available water resources, to livelihoods and to ecosystems. Routine drought monitoring is fundamental for developing an early warning system and an area-specific drought mitigation and adaptation framework. Surface waterbodies, especially those in arid and semi-arid environments, are vulnerable to the impacts of drought. The development of moderate-resolution sensors, such as the Landsat 8 Operational Land Imager (OLI) and the Sentinel-2 Multispectral Instrument (MSI), allow new opportunities to monitor droughts and their impact on surface waterbodies.

Ponds are common and abundant features in nearly all landscapes typical of European lowland landscapes yet research on freshwater biodiversity has traditionally focussed on larger waterbodies such as lakes and rivers. This has led to an increased need to understand and quantify the biodiversity associated with pond habitats to better inform the active conservation and management of these small waterbodies. This thesis examines the aquatic macroinvertebrate biodiversity (alpha, beta and gamma) and conservation value of 95 ponds in Leicestershire, UK, across a variety of urban and rural landscape types and at a range of spatial scales. In addition, the relative importance of local (physicochemical and biological) and spatial (connectivity) variables in structuring macroinvertebrate communities within ponds is investigated. At a regional scale, the greatest macroinvertebrate biodiversity and conservation value was recorded within meadow ponds compared to urban, agricultural and forest ponds. Spatially, ponds were highly physically and biologically heterogeneous. Temporally (seasonally), invertebrate communities were most dissimilar in meadow and agricultural ponds but assemblages were similar in urban and forest ponds. In urban landscapes, park ponds supported a greater diversity of invertebrates than other urban or garden ponds and typically had a greater conservation value. Garden ponds were the most taxon poor of those investigated. Perennial floodplain meadow ponds supported a greater biodiversity of invertebrates compared to ephemeral meadow ponds although conservation value was similar. Despite regular inundation from the River Soar, ephemeral ponds supported distinct communities compared to perennial meadow ponds. Aquatic macrophytes supported a higher diversity of taxa than other pond mesohabitats across all landscapes studied. Physicochemical factors were identified to be the dominant influence on macroinvertebrate assemblages although, a combination of local and spatial factors best explained the variation in community composition at a regional scale and for meadow ponds. Spatial factors were not identified to significantly influence urban pond communities. This study highlights the ecological importance and conservation value of ponds in rural and anthropogenically disturbed landscapes. Recognition of the significant contribution of ponds to freshwater biodiversity at regional and landscape scales is important for future conservation of pond habitats and will help focus and direct conservation strategies to where they are needed most.

The focus of this work was to develop a general methodology for modeling water quality in coastal waterbodies. The methods were developed in the context of modeling bacterial total maximum daily loads (TMDLs), but the general approach is applicable to a wide variety of pollutants. The study area for this dissertation was the Copano Bay watershed, which is located on the Texas Gulf Coast. The developed approach combines simple modeling techniques, of the type recommended by state and national advisory groups, in a GIS (geographic information system) framework, resulting in a methodical, easily transferred approach. This work addresses coastal systems where water quality is a function of operations in non-tidal rivers, tidal rivers, and bays, combined with the effects of watershed contributions. An uncertainty analysis was done to quantify a subset of the variance in the modeled results. Outcomes from this work include modeling tools, a documented workflow for modeling water quality in coastal watersheds, procedures to quantify the uncertainty associated with the developed approach, insight to the factors affecting water quality in the study area, and mean annual bacterial TMDLs for the impaired waterbodies of the Copano Bay watershed. / text

Tropical Storm Irene’s most extreme rainfall resulted in record-breaking sediment loads from upland tributaries to the Connecticut River. However, was the event exceptional with respect to resultant deposition downstream? Off-river waterbodies to the Lower Connecticut River, such as cut-off meanders and blocked valley lakes, are a particularly important floodplain environment, which have been shown to serve as a focal point for the trapping of sediment and associated contaminants. This study evaluates the relative role of extreme events like Tropical Storm Irene in infilling these off-river environments. To meet this objective we compare the magnitude and composition of resultant sedimentation from Irene to that observed following the 2011 and 2013 spring freshets. Tropical Storm Irene deposits were identified as compositionally distinct, grey layers that were relatively inorganic compared to sediments deposited by the annual spring freshet. Sediment within the Irene deposit was enriched in elemental potassium and depleted in zircon, a finding consistent with being enriched by glacigenic lacustrine and till sediments. Decreased mercury levels in the Irene deposits suggest that this event served to cap highly contaminated, industrial era sediment with a layer of relatively clean, fine-grained silt and clay. Resampling of these waterbodies in Fall 2012 revealed preservation of the 2-3 cm thick Irene deposit as well as 3-4 cm of more recent sediments deposited on top of this event. Sediment contributions from rare events, like Tropical Storm Irene, were found to be less influential than the annual spring freshet in the long-term infilling of waterbodies along the Lower Connecticut River. However, sediments from Irene are compositionally unique and serve to highlight the importance of this event in removing glacially derived fines from the river’s upland catchments.

Over the past century, the world's rivers have become increasingly impounded to combat water scarcity and fossil-fuel reliance. Large dams have faded from popularity due to their adverse environmental effects, but small ponds and reservoirs continue to be constructed at high rates. Due to limited data regarding their size and flow, it has been difficult to assess how these smaller impoundments impact rivers. This study combined rainfall runoff data from the Chesapeake Bay Model with the unique routing framework of VA Hydro to create a simplistic hydrologic model capable of analyzing impoundment-induced flow alteration. Using standard design techniques and satellite imagery, a methodology was developed to build realistic stage-storage-discharge relationships for small and large impoundments. Eleven impoundments of the Difficult Run watershed were modeled within VA Hydro to assess their cumulative impact on downstream flow. Multiple models were created with different active impoundments and run for the full model period, 1984 - 2005. Flow alteration increased significantly with additional impoundments. Peak flows were attenuated as water was stored behind outlets, but median flows were increased as this water was slowly released. Average storm duration increased due to extended rising and falling limbs caused by impoundment outlets. Headwater channels increasingly ran dry, decreasing extreme low flows due to impoundment evaporation. Large reservoirs had a greater impact on median flows, but smaller ponds dominated low flow alteration. These results suggest that traditional hydrologic assumptions and metrics may be incapable of analyzing a changing flow regime without explicitly considering small and large impoundments upstream. / Master of Science / At first look, dams are an excellent solution to water scarcity and energy independence. They trap clean water and direct it through turbines. Unfortunately, their installation and operation creates many negative environmental impacts by fundamentally altering downstream channels, leading to a loss of fish vitality and river function. Large dam construction has decreased in the US because of these effects, but small dams continue to be built at high rates due to growing agricultural and stormwater demands. Their impact on rivers is less understood due to limited data availability regarding their size and function. This experiment used standard design techniques and widely available satellite data to create a representative model for dams of all size. Multiple tests were run, progressively increasing the number of dams within a watershed and analyzing their impact on downstream flow. With increased impoundment, high floods decreased in magnitude. However, more-typical medium flows increased. River flow became more static, with less extreme floods and more medium flows. The modeled dams greatly decreased drought flows as trapped water evaporated and decreased outflow. This impact was particularly noticeable in ponds that drained only a small area as they took longer to refill after drying. Larger dams more greatly impacted medium flows. These results contribute significantly to water availability prediction by more realistically representing dam processes. Although more work is needed to refine the impoundment modeling strategy, this study has effectively demonstrated that small and large dams affect flow in different manners and need to be accounted for accordingly.

Der Beitrag geht auf die Landschaftsveränderungen der Kulturlandschaft im Bauland und in Hohenlohe im nördlichen Baden-Württemberg ein. Untersucht wird insbesondere die Veränderung der typischen Stillgewässer.

Der Beitrag geht auf die Landschaftsveränderungen der Kulturlandschaft im Bauland und in Hohenlohe im nördlichen Baden-Württemberg ein. Untersucht wird insbesondere die Veränderung der typischen Stillgewässer.

Les petits plans d'eau, en particulier ceux riches en matière organique, sont encore négligés en tant que sources naturelles majeures d'émission de carbone (C) dans l'atmosphère et contributeurs importants au bilan mondial de C. Les mares de tourbières riches en matières organiques sont une source nette de C atmosphérique dans les écosystèmes de tourbières, qui sont généralement un puits net de C. Ces mares émettent des gaz à effet de serre (GES) à des taux plus élevés, en particulier de méthane (CH4), par rapport à d'autres petits plans d'eau lentiques (petits lacs et étangs), ce qui peut être attribué à la connectivité hydraulique des bassins donc aux apports en C de la tourbe environnante et aux caractéristiques morphologiques des mares. Cependant, il existe très peu d'informations sur les schémas et les mécanismes de la dynamique du C dans les bassins de tourbières par rapport à leur couvert végétal ainsi qu'à d'autres petits environnements aquatiques. En particulier, la matière organique dissoute (MOD), un important intermédiaire et substrat de C, peut influencer la dynamique des émissions de GES, mais son rôle demeure méconnu à l'échelle intra- et inter-régionale. Dans cette étude, nous avons caractérisé et identifié les patrons intra- et interrégionaux et les mécanismes potentiels contrôlant la quantité et la qualité de la MOD et des concentrations de GES, ainsi que leurs liens en analysant une gamme de variables optiques et chimiques et en compilant les données géographiques (c'est-à-dire le climat, le couvert végétal et morphométrie des bassins) à partir de bassins de tourbières ombrotrophes dans cinq régions de l'est du Canada (Grande plée Bleue, sud du Québec et région de la Minganie, est du Québec) et du sud de la Patagonie chilienne (Punta Arenas, parc Karukinka et île Navarino). Nous avons également effectué un échantillonnage interannuel dans la Grande plée Bleue pour identifier les tendances temporelles des concentrations et de la composition des GES et de MOD. Nous avons trouvé une variabilité interrégionale élevée dans les patrons de MOD et de GES par rapport à la variabilité intrarégionale qui était cohérente avec l'hétérogénéité des propriétés géographiques, en particulier, le climat. Les patrons interrégionaux des concentrations de GES étaient de plus déterminés par la couverture végétale environnante, la morphométrie du bassin et la composition de la MOD de type protéique. D'autre part, bien que nous n'ayons pas observé de patrons temporels significatifs dans les concentrations de GES, de MOD et de la composition de type humique terrestre au cours de l’été dans la Grande plée Bleue, les patrons temporels de GES ont été influencés par la concentration de MOD, la composition de type humique terrestre, et la chimie interne de l'eau. Dans l'ensemble, nos résultats suggèrent que les patrons interrégionaux de la MOD et des GES, et les liens entre eux, sont principalement contrôlés par le climat (température et précipitations), la couverture végétale et la morphométrie des bassins, tandis que les patrons temporels de la MOD et des GES sont principalement régis par des facteurs à l'échelle locale tels que la morphométrie des bassins et la connectivité hydrologique. / Small waterbodies, especially organic-rich, are still overlooked as a major natural source of carbon (C) emission to the atmosphere and an important contributor in the global C budget. Organic-rich peatland pools are generally net atmospheric C sources embedded in peatland ecosystems, which are generally net C sinks. They emit high areal rates of greenhouse gases (GHG), particularly methane (CH4), compared to other small lentic waterbodies (small lakes and ponds) which may be attributed to peat-pool hydraulic connectivity leading to C loading from the surrounding peat and morphological characteristics. But there is very little information on the patterns and drivers of C dynamics within peatland pools compared to their vegetated areas as well as other small aquatic environments. In particular, the role that dissolved organic matter (DOM), an important intermediate and C substrate, may play in GHG dynamics is poorly known at the intra- and inter-regional scales. In this study, we characterized and identified the intra- and inter regional patterns and drivers of DOM quantity and quality and GHG concentrations as well as their links. We did so by analyzing a range of optical and chemical variables and compiling geographic data (i.e., climate, vegetation cover and pool morphometry) from ombrotrophic peatland pools across five regions in eastern Canada (Grande plée Bleue, southern Québec and Minganie region, eastern Québec) and southern Chilean Patagonia (Punta Arenas, Karukinka Park and Navarino Island). We also conducted inter-annual sampling in Grande plée Bleue to identify the temporal patterns in GHG and DOM concentrations and composition. We found high inter-regional variability in DOM and GHG patterns compared to intra-regional variability which was coherent with the heterogeneity of geographical properties. Inter-regional patterns in GHG concentrations were driven by surrounding vegetation cover, pool morphometry and protein-like DOM composition. On the other hand, although we did not observe significant temporal patterns in GHG and DOM concentrations and terrestrial humic-like composition throughout the growing seasons in Grande plée Bleue, temporal patterns of GHG were influenced by the DOM concentration, terrestrial humic-like composition, and internal water chemistry. Overall, our results suggest that inter-regional patterns in DOM and GHG, and the links among them are predominantly controlled by the broad-scale patterns in climate (temperature and precipitation), vegetation cover, and pool morphometry, while temporal patterns in DOM and GHG are predominantly governed by local-scale drivers such as pool morphometry.

L'écologie urbaine est un nouveau champ de recherche qui cherche à comprendre les structures et les patrons des communautés et des écosystèmes situés dans des paysages urbains. Les petits plans d’eau sont connus comme des écosystèmes aquatiques qui peuvent contenir une biodiversité considérable pour plusieurs groupes taxonomiques (oiseaux, amphibiens, macroinvertébrés), ce qui en fait des écosystèmes intéressants pour les études de conservation. Cependant, la biodiversité du zooplancton, un élément central des réseaux trophiques aquatiques, n’est pas entièrement connue pour les plans d’eaux urbains et devrait être mieux décrite et comprise. Cette étude a évalué les patrons de biodiversité des communautés zooplanctoniques dans des plans d’eau urbains sur l’Ile de Montréal et leurs sources de variation. Des suggestions pour l’évaluation et la conservation de la biodiversité sont aussi discutées. La biodiversité zooplanctonique des plans d’eaux urbains s’est avérée être assez élevée, avec les cladocères et les rotifères montrant les contributions à la diversité gamma et bêta les plus élevées. Sur l’ensemble des plans d’eau, il y avait une corrélation négative entre les contributions à la bêta diversité des cladocères et des rotifères. Au niveau de chaque plan d'eau, la zone littorale colonisée par des macrophytes s'est avérée être un habitat important pour la biodiversité zooplactonique, contribuant considérablement à la richesse en taxons, souvent avec une différente composition en espèces. Les communautés zooplanctoniques répondaient aux facteurs ascendants et descendants, mais aussi aux pratiques d’entretien, car le fait de vider les plans d’eau en hiver affecte la composition des communautés zooplanctoniques. Les communautés de cladocères dans ces plans d’eau possédaient des quantités variables de diversité phylogénétique, ce qui permet de les classer afin de prioriser les sites à préserver par rapport à la diversité phylogénétique. Le choix des sites à préserver afin de maximiser la diversité phylogénétique devrait être correctement établi, afin d’eviter de faire des choix sous-optimaux. Cependant, pour des taxons tels que les cladocères, pour lesquels les relations phylogénétiques demeurent difficiles à établir, placer une confiance absolue dans un seul arbre est une procédure dangereuse. L’incorporation de l’incertitude phylogénétique a démontré que, lorsqu’elle est prise en compte, plusieurs différences potentielles entre la diversité phylogenétique ne sont plus supportées. Les patrons de composition des communautés différaient entre les plans d’eau, les mois et les zones d’échantillonnage. Etant donné les intéractions sont significatives entres ces facters; ceci indique que tous ces facteurs devraient êtres considérés. L’urbanisation ne semblait pas sélectionner pour un type unique de composition des groupes alimentaires, étant donné que les communautés pouvaient changer entres des assemblages de types alimentaires différents. Les variables environnementales, surtout la couverture du plan d’eau en macrophytes, étaient des facteurs importants pour la biodiversité zooplanctonique, affectant la richesse spécifique de divers groupes taxonomiques et alimentaires. Ces variables affectaient aussi la composition des communautés, mais dans une moindre mesure, étant des variables explicatives modestes, ce qui indiquerait le besoin de considérer d’autres processus. / Urban ecology is an emerging research field that seeks to understand the structures and patterns of communities and ecosystems located in urban landscapes. Small waterbodies are known as aquatic ecosystems that can harbour notable biodiversity for various taxonomic groups (birds, amphibians, macroinvertebrates), making them interesting ecosystems for conservation studies. However, the biodiversity of zooplankton, a central element of aquatic trophic networks, is still not entirely known for urban waterbodies and should be better described and understood. This study examined the biodiversity patterns of zooplanktonic communities in urban waterbodies on the Island of Montreal and their sources of variation. Suggestions for biodiversity assessment and for biodiversity preservation are also discussed. Zooplankton biodiversity urban waterbodies proved to be quite high, with cladoceran and rotifer taxa showing the highest contributions to gamma and beta diversity. Across waterbodies, there was a negative correlation between the contributions to cladoceran and rotifer beta diversity. Within waterbodies, the littoral zone showing macrophytes proved to be an important habitat for zooplankton biodiversity, considerably contributing species richness, often with a different species composition. Zooplankton communities responded to bottom-up and top-down forces, but also management practices, as waterbody emptying in winter affected zooplankton community composition. Cladoceran communities in these waterbodies showed varying amounts of phylogenetic diversity, which allowed them to be ranked in order to prioritize sites to preserve with regards to phylogenetic diversity. Selection of sites to preserve in order to maximize phylogenetic diversity should be properly guided, in order to avoid making suboptimal choices. However, for taxa such as Cladocera, for which phylogenetic relationships remain difficult to establish, placing absolute confidence in a single tree is a dangerous procedure. Incorporation of phylogenetic uncertainty showed that, when it is taken into account, then several potential differences in phylogenetic diversity were not supported anymore. Community composition patterns differed between waterbodies, months and sampling zones. Due to the presence of significant interactions between these factors, this indicates that all these factors should be considered. Urbanization did not seem to select for a single type of feeding group composition, as communities in waterbodies could shift between assemblages with different feeding types. Environmental variables, especially waterbody macrophyte coverage, were important factors for zooplankton biodiversity, positively affected species richness of various taxonomic groups and feeding groups. These variables also affected community composition, but to a lesser extent, being modest predictor variables, indicating the need to consider other processes.