Featured Thesis Figure
Drivers of Inter-Annual Variability in Wood Density
Dendroclimatology utilizes a number of tree-ring parameters to reconstruct past climates. This thesis investigates the mechanisms that drive variations in wood density of eight Pinus cembra cores, using an image analysis software with very high resolution.
A biplot of the first two principal components (PC) shows the relationships between relevant anatomical features of tree rings (shown are abbreviations in the Figure). The first PC (x-axis; explaining 47% of the variance in the original dataset) can be seen as a measure of the cell wall thickening phase. The second PC (y-axis; 19% explained) is a good measure of mean and maximum density. The vector length is equal to the variance of the variables. Furthermore, the distance between vectors refers to the similarity between variables. In short, latewood width (LWW; highlighted) is strongly correlated to density parameters (MDCWT & MDCWA), i.e., closely resembles mean density.
This suggests that latewood width can serve as a surrogate for density if such measurements are not attainable. Understanding how anatomical features of tree rings are related to density parameters helps to better understand the mechanisms that drive inter-annual variations in wood density. (Figure 34, page 55, from the master thesis by Lisbeth Haberbauer)
Reconstruction of historical flood levels of the river Aare in Aarau
Over the past centuries, the Swiss city of Aarau has been recurrently affected by floods. In this thesis, historical floods are assessed by means of administrative protocols, chronicles, maps, paintings, and newspaper articles. Between 1400 and 1900, a number of 39 flood events were dated (not shown). Prior to 1700, floods occurred significantly earlier in the year than after 1700, a seasonal pattern that is in accordance with observations of rivers in Germany. Water levels of ten of these events were reconstructed for the first time in this thesis (orange dots for events prior to 1852, the bars indicate probable ranges). Data after 1852 are adjusted gauge readings. Local river regulations were rather ineffective, and recurring conflicts between involved political levels delayed effective measures until the 1850s. On a regional scale, the upstream Kander deviation in 1714 and the Jura water correction 1868-1891 had a great impact on the river system in Aarau. They substantially deepened the riverbed and thus decreased the danger of floods (effect approximated by the two black dotted lines). (Figure 17, page 85, from the master thesis by Mauro Bolzern)
This decade's solar photovoltaic emergence: a cross-sectorial investigation
Solar photovoltaic technology has been available since the 1950’s however the technology has not been widely applied until the beginning of this decade. In this thesis, the paramount factors for this boom are investigated using Qualitative Comparative Analysis of the leading promoting countries, i.e. with at least 10 gigawatts of installed solar photovoltaic capacity.
The analysis revealed three potential pathways. The first positive pathway (Path 1 in the Figure; dot sizes represent importance) includes the cases of Japan and the United States. They are representative of cases that have "Ability" and* "Resource Intensive Populations" and* "Potential to decarbonize their electricity and heat production sectors". The second pathway (Path 2), represented by China and Japan, is similar to the first in the sense that they have the same parsimonious solution (taking only the large circles into consideration). The third and final pathway (Path 3) is indicative of a more sustainable path taken by European countries such as, Germany and Italy. This more sustainable pathway is highlighted by the presence of "Kyoto Commitments" and* the "Inability to rely on nuclear power production in the future" and* "Potential to decarbonize" and* "Ability".
Path 3 is in essence the most desirable because it encompasses emission reduction pledges under international climate negotiations. In contrast, Path 1 and 2 seem to be primarily fueled by large, resource intensive populations and growing economical necessities. (Figure 15, page 50, from the master thesis by Simon Steffen).)
Changes in the risk of spring frost damage for grapevines due to climate change
A case study in the Swiss Rhone Valley
Global warming does not only cause the growing phases of plants to start earlier, it also leads to a shift in the average day of year of latest frost days. Depending on the magnitude of these changes, as well as on the corresponding variances, it is not clear if risk for spring frost damage will increase or decrease. Focusing on the Swiss Rhone Valley, future risk according to the SRES A1B scenario was modelled by combining two locations, four frost indices, twelve phenology models and 16 climate model chains. The solid lines indicate the yearly means of the frost indices (i.e. the probability of a frost day after budburst (BBCH09), p(T.n<0°C), the frequency of frost days after BBCH09, f(T.n<0°C), the temperature sum of daily minimum temperature below 0 °C after BBCH09, ∑(T.n<0°C), and the temperature sum of daily mean temperatures below 2 °C after BBCH09, ∑(T.0<2°C)), the day of year (DOY) of the last frost day and of BBCH09. The shaded areas indicate the range of +/- one standard deviation around the yearly means. The broken red lines visualize the mean trends for the period 2001 to 2050. The average risk for spring frost damage is predicted to slightly decrease. This may support winemakers in their decisions regarding future grape varieties and frost damage prevention measures.
(Figure 12, page 66, from the master thesis by Michael Meier)
Quinoa yields w.r.t. temperature and precipitation (Lampa, Arapa, and Chuquibambilla stations, Peru, years 1964 - 2012)
The potential value of seasonal climate forecasts for allocating agricultural land is estimated in this thesis. Therefore, a theoretical model was developed and applied to the region of Puno in Peru. The application relies on using statistical climate data and simulated yields for quinoa and potato crops - the Figure presents yield simulations for quinoa depending on two climatic indicators, i.e. the seasonal precipitation sum and the minimum temperature during the flowering stage. The analysis shows that the expected revenue can be increased by 4.66 % when key decisions are made with seasonal forecasts, compared to a scenario without seasonal forecasts. The positive value indicates the potential of integrating high-quality seasonal forecasts into decision-making when allocating agricultural land to specific crops.
(Figure 4, page 24, from the master thesis by Anita Frehner)
Mean runoff of the river Thur in a present-day versus a pre-industrial climate
The thesis assesses the influence of anthropogenic greenhouse gas emissions on temperature, precipitation and runoff of the river Thur in Switzerland. To achieve this, thousands of Global Climate Model simulations with both present-day (A2000) and pre-industrial (A2000N) climate conditions are bias-corrected (from raw to corr; see Figure) and fed into a hydrological model for the river Thur. Higher mean runoff in winter and spring is formed in the present-day scenario (red colors) compared to the pre-industrial scenario (blue colors). This is mainly caused by the combination of increased precipitation and higher temperatures in winter, resulting in less snow accumulation in the present-day scenario. Therefore, more liquid water is available in the hydrological model, leading to enhanced runoff. In contrast, the present-day simulations exhibit lower runoff in summer and autumn than the pre-industrial simulations. This may be caused by the higher temperatures in the present-day scenario which enhance evapotranspiration and thus decrease the amount of water entering the hydrological model. These findings may support decision-makers in climate-related risk and adaptation management.
(Figure 5.7, page 41, from the master thesis by Regula Mülchi)
Weak points along the main rivers of the Bernese Oberland (Switzerland).
Weak points are locations along a river bed where the channel capacity is frequently exceeded during periods of high river discharges. Hence, weak points indicate potential focii for flood protection measures. Technically, weak points are defined as cross sections of the river bed where the bank-full discharge (channel capacity) has a flood recurrence period (HQ) between 30 and 100 years (red to yellow lines). Whereas specific river sections had been analyzed in practice so far, entire watersheds of the Bernese Oberland (Switzerland) were investigated in this thesis. The highest numbers of weak points (relative to the number of measured cross sections) are found for the Simme, Weisse Lütschine and the Hasli-Aare rivers. The good news is that frequently exceeded channel capacities (<= HQ30) are located along unpopulated areas. However, the protection aim of HQ100 along populated areas is not hold along parts of the Weisse Lütschine and the Simme, and neither along the Aare within the cities of Thun and Bern. These findings provide valuable information for both national and regional watershed administration.
(Figure 3.40, page 87, from the master thesis by Danielle Huser)
Seasonal total precipitation near Mt. Kenya, interpolated from gauge measurements during the Long Rains (March-April-May) in 1977.
Recent changes in agricultural practices and population growth have triggered conflicts between different water users, as economy and food security highly depend on rain-fed agriculture and river water discharge. In this context, the provided spatial information about rainfall can be used for water ressource allocations, for hydrological studies or to monitor trends over space and time.
(Figure 5.4, page 35, from the master thesis by Noemi Imfeld)
Cumulative influences of various drivers on the total CO2 emissions in the US from 1997 to 2013.
(Figure 2, page 51, from the master thesis by Marius Schneider)