<p>Alpine glaciers around the world are in retreat and are unlikely to reverse course. This dissertation focuses on improving our understanding of the impact of glacial melt on mountainous alpine groundwater systems. Studies on glacial melt-groundwater interactions have become more prevalent, particularly in the past 5 years, because we are recognizing that the contribution of glacial melt to the hydrologic cycle is not limited to melt-season surficial streamflow. The importance of glacial melt to mountain groundwater systems has the potential to not only influence spring and streamflow generation, but also the longevity of alpine specific, and frequently endangered species, dependent on this source of recharge. This recharge may be vital for human water needs such as potable water, agriculture, and hydrothermal power.</p>The impact that a transition from glacial melt to snow- or rain-dominated streamflow and recharge will have on alpine ecosystems in a continually warming climate is far reaching. This dissertation: 1) tests whether glacial melt is an important source of recharge for mountain springs and their microbial communities, 2) investigates the spatial impact of glacial-melt recharge on residence times and flowpaths that support alpine springs, and 3) explores the impact of post-peak water on alpine baseflow using a statistical, timeseries approach. My results show that the groundwater systems in glaciated mountainous, alpine regions are particularly vulnerable to climate change. Springs in Mount Hood National Forest and Glacier National Park were sampled over a 4-year period, and in addition, publicly available long-term streamflow datasets were are also utilized. The chapters composing this work build upon each other, and compare and contrast the factors most important in glacial melt recharging the mountain-block. Information that is vital to the management of alpine water resources by landowners, watershed groups, scientists, and others interested in mountain groundwater systems in glaciated alpine regions is presented in the following pages.

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This thesis examines the readiness and perception in the regions of Gothenburg and Bremen towards future sea level rise. It does so through the theoretical lens of risk psychology / policy research and of climate science research. Results are built on some of the most recent research of these fields, as well as interviews with 14 people on the local, regional and national level in Germany and Sweden. Key findings of this thesis are that both contexts struggle to deal with the great uncertainties inherent in sea level rise. On the German North Sea coast, there is long experience with sea level variation and extensive civil institutions created to deal with storm surges, dikes and sea level rise which may partially compensate for inherent vulnerability to future sea level rise in this region. The novelty of sea level rise in Gothenburg and Sweden means that it is in the process of creating similar institutions and national-regional divisions of responsibility from scratch. The great uncertainty around the pace and extent of future sea level rise is however an obstacle which may have to be overcome before a more coherent response may be developed. / Denna uppsats undersöker beredskap och uppfattningar kring framtida havsnivåhöjningar i Göteborg och Bremen. Detta görs med de teoretiska ansatserna riskpsykologi / beslutspsykologi och grundläggande klimatvetenskap. Uppsatsens resultat bygger på de senaste resultaten inom dessa fält, samt intervjuer med 14 personer på lokal, regional och nationell nivå i Tyskland och Sverige. Efter genomförd studie kan konstateras att bägge kontext har svårigheter att hantera de stora osäkerheter som havsnivåhöjningen medför. Tyska Nordsjökusten har mycket lång erfarenhet och kapabla offentliga institutioner vilka skapats för att hantera skyddsvallar, sjunkande landnivåer och stormfloder, vilket balanserar det prekära läge som området annars står inför. I Göteborg och i Sverige är havsnivåhöjning något fundamentalt nytt, vilket innebär att man nu försöker skapa liknande institutioner och ansvarsfördelning mellan nationellt och regionalt som de Bremen och Tyskland redan har. Ett hinder för detta är de stora osäkerheter som råder kring hastighet och absolut nivå på framtida havsnivåhöjningar. Dessa osäkerheter kan komma behöva reduceras innan problemet börjar hanteras på ett mer samordnat sätt.