@misc{AuhagenUth2022, author = {Auhagen, Christopher Patrick and Uth, Melanie}, title = {Variation of relative complementizers in Yucatecan Spanish}, series = {Zweitver{\"o}ffentlichungen der Universit{\"a}t Potsdam : Philosophische Reihe}, journal = {Zweitver{\"o}ffentlichungen der Universit{\"a}t Potsdam : Philosophische Reihe}, issn = {1866-8380}, doi = {10.25932/publishup-58437}, url = {http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-584375}, pages = {18}, year = {2022}, abstract = {The starting point of this article is the occurrence of determiner-less and bare que relative complementizers like (en) que, '(in) that', instead of (en) el que, '(in) which', in Yucatecan Spanish (southeast Mexico). While reference grammars treat complementizers with a determiner as the standard option, previous diachronic research has shown that determiner-less complementizers actually predate relative complementizers with a determiner. Additionally, Yucatecan Spanish has been in long-standing contact with Yucatec Maya. Relative complementation in Yucatec Maya differs from that in Spanish (at least) in that the non-complex complementizer tu'ux ('where') is generally the only option for locative complementation. The paper explores monolingual and bilingual data from Yucatecan Spanish to discuss the question whether the determiner-less and bare que relative complementizers in our data constitute a historic remnant or a dialectal recast, possibly (but not necessarily) due to language contact. Although our pilot study may not answer these far-reaching questions, it does reveal two separate, but intertwined developments: (i) a generally increased rate of bare que relative complementation, across both monolingual speakers of Spanish and Spanish Maya bilinguals, compared to other Spanish varieties, and (ii) a preference for donde at the cost of other locative complementizer constructions in the bilingual group. Our analysis thus reveals intriguing differences between the complementizer preferences of monolingual and bilingual speakers, suggesting that different variational patterns caused by different (socio-)linguistic factors can co-develop in parallel in one and the [same] region.}, language = {en} } @phdthesis{Pregla2023, author = {Pregla, Dorothea}, title = {Variability in sentence processing performance in German people with aphasia and unimpaired German native speakers}, doi = {10.25932/publishup-61420}, url = {http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-614201}, school = {Universit{\"a}t Potsdam}, pages = {171}, year = {2023}, abstract = {Individuals with aphasia vary in the speed and accuracy they perform sentence comprehension tasks. Previous results indicate that the performance patterns of individuals with aphasia vary between tasks (e.g., Caplan, DeDe, \& Michaud, 2006; Caplan, Michaud, \& Hufford, 2013a). Similarly, it has been found that the comprehension performance of individuals with aphasia varies between homogeneous test sentences within and between sessions (e.g., McNeil, Hageman, \& Matthews, 2005). These studies ascribed the variability in the performance of individuals with aphasia to random noise. This conclusion would be in line with an influential theory on sentence comprehension in aphasia, the resource reduction hypothesis (Caplan, 2012). However, previous studies did not directly compare variability in language-impaired and language-unimpaired adults. Thus, it is still unclear how the variability in sentence comprehension differs between individuals with and without aphasia. Furthermore, the previous studies were exclusively carried out in English. Therefore, the findings on variability in sentence processing in English still need to be replicated in a different language. This dissertation aims to give a systematic overview of the patterns of variability in sentence comprehension performance in aphasia in German and, based on this overview, to put the resource reduction hypothesis to the test. In order to reach the first aim, variability was considered on three different dimensions (persons, measures, and occasions) following the classification by Hultsch, Strauss, Hunter, and MacDonald (2011). At the dimension of persons, the thesis compared the performance of individuals with aphasia and language-unimpaired adults. At the dimension of measures, this work explored the performance across different sentence comprehension tasks (object manipulation, sentence-picture matching). Finally, at the dimension of occasions, this work compared the performance in each task between two test sessions. Several methods were combined to study variability to gain a large and diverse database. In addition to the offline comprehension tasks, the self-paced-listening paradigm and the visual world eye-tracking paradigm were used in this work. The findings are in line with the previous results. As in the previous studies, variability in sentence comprehension in individuals with aphasia emerged between test sessions and between tasks. Additionally, it was possible to characterize the variability further using hierarchical Bayesian models. For individuals with aphasia, it was shown that both between-task and between-session variability are unsystematic. In contrast to that, language-unimpaired individuals exhibited systematic differences between measures and between sessions. However, these systematic differences occurred only in the offline tasks. Hence, variability in sentence comprehension differed between language-impaired and language-unimpaired adults, and this difference could be narrowed down to the offline measures. Based on this overview of the patterns of variability, the resource reduction hypothesis was evaluated. According to the hypothesis, the variability in the performance of individuals with aphasia can be ascribed to random fluctuations in the resources available for sentence processing. Given that the performance of the individuals with aphasia varied unsystematically, the results support the resource reduction hypothesis. Furthermore, the thesis proposes that the differences in variability between language-impaired and language-unimpaired adults can also be explained by the resource reduction hypothesis. More specifically, it is suggested that the systematic changes in the performance of language-unimpaired adults are due to decreasing fluctuations in available processing resources. In parallel, the unsystematic variability in the performance of individuals with aphasia could be due to constant fluctuations in available processing resources. In conclusion, the systematic investigation of variability contributes to a better understanding of language processing in aphasia and thus enriches aphasia research.}, language = {en} } @misc{CohenCampisanoArrowsmithetal.2016, author = {Cohen, Abby and Campisano, Christopher and Arrowsmith, J. Ramon and Asrat, Asfawossen and Behrensmeyer, A. K. and Deino, A. and Feibel, C. and Hill, A. and Johnson, R. and Kingston, J. and Lamb, Henry F. and Lowenstein, T. and Noren, A. and Olago, D. and Owen, Richard Bernhart and Potts, R. and Reed, Kate and Renaut, R. and Sch{\"a}bitz, F. and Tiercelin, J.-J. and Trauth, Martin H. and Wynn, J. and Ivory, S. and Brady, K. and O'Grady, R. and Rodysill, J. and Githiri, J. and Russell, Joellen and Foerster, Verena and Dommain, Ren{\´e} and Rucina, J. S. and Deocampo, D. and Russell, J. and Billingsley, A. and Beck, C. and Dorenbeck, G. and Dullo, L. and Feary, D. and Garello, D. and Gromig, R. and Johnson, T. and Junginger, Annett and Karanja, M. and Kimburi, E. and Mbuthia, A. and McCartney, Tannis and McNulty, E. and Muiruri, V. and Nambiro, E. and Negash, E. W. and Njagi, D. and Wilson, J. N. and Rabideaux, N. and Raub, Timothy and Sier, Mark Jan and Smith, P. and Urban, J. and Warren, M. and Yadeta, M. and Yost, Chad and Zinaye, B.}, title = {The Hominin Sites and Paleolakes Drilling Project}, series = {Postprints der Universit{\"a}t Potsdam : Mathematisch-Naturwissenschaftliche Reihe}, journal = {Postprints der Universit{\"a}t Potsdam : Mathematisch-Naturwissenschaftliche Reihe}, number = {611}, doi = {10.25932/publishup-41249}, url = {http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-412498}, pages = {16}, year = {2016}, abstract = {The role that climate and environmental history may have played in influencing human evolution has been the focus of considerable interest and controversy among paleoanthropologists for decades. Prior attempts to understand the environmental history side of this equation have centered around the study of outcrop sediments and fossils adjacent to where fossil hominins (ancestors or close relatives of modern humans) are found, or from the study of deep sea drill cores. However, outcrop sediments are often highly weathered and thus are unsuitable for some types of paleoclimatic records, and deep sea core records come from long distances away from the actual fossil and stone tool remains. The Hominin Sites and Paleolakes Drilling Project (HSPDP) was developed to address these issues. The project has focused its efforts on the eastern African Rift Valley, where much of the evidence for early hominins has been recovered. We have collected about 2 km of sediment drill core from six basins in Kenya and Ethiopia, in lake deposits immediately adjacent to important fossil hominin and archaeological sites. Collectively these cores cover in time many of the key transitions and critical intervals in human evolutionary history over the last 4 Ma, such as the earliest stone tools, the origin of our own genus Homo, and the earliest anatomically modern Homo sapiens. Here we document the initial field, physical property, and core description results of the 2012-2014 HSPDP coring campaign.}, language = {en} } @misc{DallmeyerClaussenFischeretal.2015, author = {Dallmeyer, Anne and Claussen, M. and Fischer, N. and Haberkorn, K. and Wagner, S. and Pfeiffer, M. and Jin, L. and Khon, Vyacheslav and Wang, Y. and Herzschuh, Ulrike}, title = {The evolution of sub-monsoon systems in the Afro-Asian monsoon region during the Holocene}, series = {Postprints der Universit{\"a}t Potsdam : Mathematisch-Naturwissenschaftliche Reihe}, journal = {Postprints der Universit{\"a}t Potsdam : Mathematisch-Naturwissenschaftliche Reihe}, number = {587}, issn = {1866-8372}, doi = {10.25932/publishup-40972}, url = {http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-409727}, pages = {22}, year = {2015}, abstract = {The recently proposed global monsoon hypothesis interprets monsoon systems as part of one global-scale atmospheric overturning circulation, implying a connection between the regional monsoon systems and an in-phase behaviour of all northern hemispheric monsoons on annual timescales (Trenberth et al., 2000). Whether this concept can be applied to past climates and variability on longer timescales is still under debate, because the monsoon systems exhibit different regional characteristics such as different seasonality (i. e. onset, peak and withdrawal). To investigate the interconnection of different monsoon systems during the pre-industrial Holocene, five transient global climate model simulations have been analysed with respect to the rainfall trend and variability in different sub-domains of the Afro-Asian monsoon region. Our analysis suggests that on millennial timescales with varying orbital forcing, the monsoons do not behave as a tightly connected global system. According to the models, the Indian and North African monsoons are coupled, showing similar rainfall trend and moderate correlation in centennial rainfall variability in all models. The East Asian monsoon changes independently during the Holocene. The dissimilarities in the seasonality of the monsoon sub-systems lead to a stronger response of the North African and Indian monsoon systems to the Holocene insolation forcing than of the East Asian monsoon and affect the seasonal distribution of Holocene rainfall variations. Within the Indian and North African monsoon domain, precipitation solely changes during the summer months, showing a decreasing Holocene precipitation trend. In the East Asian monsoon region, the precipitation signal is determined by an increasing precipitation trend during spring and a decreasing precipitation change during summer, partly balancing each other. A synthesis of reconstructions and the model results do not reveal an impact of the different seasonality on the timing of the Holocene rainfall optimum in the different sub-monsoon systems. Rather they indicate locally inhomogeneous rainfall changes and show that single palaeo-records should not be used to characterise the rainfall change and monsoon evolution for entire monsoon sub-systems.}, language = {en} } @misc{SeibertMerzApel2017, author = {Seibert, Mathias and Merz, Bruno and Apel, Heiko}, title = {Seasonal forecasting of hydrological drought in the Limpopo Basin}, series = {Postprints der Universit{\"a}t Potsdam : Mathematisch Naturwissenschaftliche Reihe}, journal = {Postprints der Universit{\"a}t Potsdam : Mathematisch Naturwissenschaftliche Reihe}, number = {626}, doi = {10.25932/publishup-41844}, url = {http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-418442}, pages = {1611 -- 1629}, year = {2017}, abstract = {The Limpopo Basin in southern Africa is prone to droughts which affect the livelihood of millions of people in South Africa, Botswana, Zimbabwe and Mozambique. Seasonal drought early warning is thus vital for the whole region. In this study, the predictability of hydrological droughts during the main runoff period from December to May is assessed using statistical approaches. Three methods (multiple linear models, artificial neural networks, random forest regression trees) are compared in terms of their ability to forecast streamflow with up to 12 months of lead time. The following four main findings result from the study. 1. There are stations in the basin at which standardised streamflow is predictable with lead times up to 12 months. The results show high inter-station differences of forecast skill but reach a coefficient of determination as high as 0.73 (cross validated). 2. A large range of potential predictors is considered in this study, comprising well-established climate indices, customised teleconnection indices derived from sea surface temperatures and antecedent streamflow as a proxy of catchment conditions. El Nino and customised indices, representing sea surface temperature in the Atlantic and Indian oceans, prove to be important teleconnection predictors for the region. Antecedent streamflow is a strong predictor in small catchments (with median 42\% explained variance), whereas teleconnections exert a stronger influence in large catchments. 3. Multiple linear models show the best forecast skill in this study and the greatest robustness compared to artificial neural networks and random forest regression trees, despite their capabilities to represent nonlinear relationships. 4. Employed in early warning, the models can be used to forecast a specific drought level. Even if the coefficient of determination is low, the forecast models have a skill better than a climatological forecast, which is shown by analysis of receiver operating characteristics (ROCs). Seasonal statistical forecasts in the Limpopo show promising results, and thus it is recommended to employ them as complementary to existing forecasts in order to strengthen preparedness for droughts.}, language = {en} } @misc{DeSouzaSilveiraCarlsohnLangenetal.2016, author = {De Souza Silveira, Raul and Carlsohn, Anja and Langen, Georg and Mayer, Frank and Scharhag-Rosenberger, Friederike}, title = {Reliability and day-to-day variability of peak fat oxidation during treadmill ergometry}, series = {Postprints der Universit{\"a}t Potsdam : Humanwissenschaftliche Reihe}, journal = {Postprints der Universit{\"a}t Potsdam : Humanwissenschaftliche Reihe}, number = {423}, url = {http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-407334}, pages = {7}, year = {2016}, abstract = {Background: Exercising at intensities where fat oxidation rates are high has been shown to induce metabolic benefits in recreational and health-oriented sportsmen. The exercise intensity (Fat peak ) eliciting peak fat oxidation rates is therefore of particular interest when aiming to prescribe exercise for the purpose of fat oxidation and related metabolic effects. Although running and walking are feasible and popular among the target population, no reliable protocols are available to assess Fat peak as well as its actual velocity (V PFO ) during treadmill ergometry. Our purpose was therefore, to assess the reliability and day-to-day variability of V PFO and Fat peak during treadmill ergometry running. Methods: Sixteen recreational athletes (f = 7, m = 9; 25 ± 3 y; 1.76 ± 0.09 m; 68.3 ± 13.7 kg; 23.1 ± 2.9 kg/m 2 ) performed 2 different running protocols on 3 different days with standardized nutrition the day before testing. At day 1, peak oxygen uptake (VO 2peak ) and the velocities at the aerobic threshold (V LT ) and respiratory exchange ratio (RER) of 1.00 (V RER ) were assessed. At days 2 and 3, subjects ran an identical submaximal incremental test (Fat-peak test) composed of a 10 min warm-up (70 \% V LT ) followed by 5 stages of 6 min with equal increments (stage 1 = V LT , stage 5 = V RER ). Breath-by-breath gas exchange data was measured continuously and used to determine fat oxidation rates. A third order polynomial function was used to identify V PFO and subsequently Fat peak . The reproducibility and variability of variables was verified with an int raclass correlation coef ficient (ICC), Pearson ' s correlation coefficient, coefficient of variation (CV) an d the mean differences (bias) ± 95 \% limits of agreement (LoA). Results: ICC, Pearson ' s correlation and CV for V PFO and Fat peak were 0.98, 0.97, 5.0 \%; and 0.90, 0.81, 7.0 \%, respectively. Bias ± 95 \% LoA was - 0.3 ± 0.9 km/h for V PFO and - 2±8\%ofVO 2peak for Fat peak. Conclusion: In summary, relative and absolute reliability indicators for V PFO and Fat peak were found to be excellent. The observed LoA may now serve as a basis for future training prescriptions, although fat oxidation rates at prolonged exercise bouts at this intensity still need to be investigated.}, language = {en} } @phdthesis{Schaber2002, author = {Schaber, J{\"o}rg}, title = {Phenology in Germany in the 20th century : methods, analyses and models}, url = {http://nbn-resolving.de/urn:nbn:de:kobv:517-0000532}, school = {Universit{\"a}t Potsdam}, year = {2002}, abstract = {Die L{\"a}nge der Vegetationsperiode (VP) spielt eine zentrale Rolle f{\"u}r die interannuelle Variation der Kohlenstoffspeicherung terrestrischer {\"O}kosysteme. Die Analyse von Beobachtungsdaten hat gezeigt, dass sich die VP in den letzten Jahrzehnten in den n{\"o}rdlichen Breiten verl{\"a}ngert hat. Dieses Ph{\"a}nomen wurde oft im Zusammenhang mit der globalen Erw{\"a}rmung diskutiert, da die Ph{\"a}nologie von der Temperatur beeinflusst wird. Die Analyse der Pflanzenph{\"a}nologie in S{\"u}ddeutschland im 20. Jahrhundert zeigte: - Die starke Verfr{\"u}hung der Fr{\"u}hjahrsphasen in dem Jahrzehnt vor 1999 war kein singul{\"a}res Ereignis im 20. Jahrhundert. Schon in fr{\"u}heren Dekaden gab es {\"a}hnliche Trends. Es konnten Perioden mit unterschiedlichem Trendverhalten identifiziert werden. - Es gab deutliche Unterschiede in den Trends von fr{\"u}hen und sp{\"a}ten Fr{\"u}hjahrsphasen. Die fr{\"u}hen Fr{\"u}hjahrsphasen haben sich stetig verfr{\"u}ht, mit deutlicher Verfr{\"u}hung zwischen 1931 und 1948, moderater Verfr{\"u}hung zwischen 1948 und 1984 und starker Verfr{\"u}hung zwischen 1984 und 1999. Die sp{\"a}ten Fr{\"u}hjahrsphasen hingegen, wechselten ihr Trendverhalten in diesen Perioden von einer Verfr{\"u}hung zu einer deutlichen Versp{\"a}tung wieder zu einer starken Verfr{\"u}hung. Dieser Unterschied in der Trendentwicklung zwischen fr{\"u}hen und sp{\"a}ten Fr{\"u}hjahrsphasen konnte auch f{\"u}r ganz Deutschland in den Perioden 1951 bis 1984 und 1984 bis 1999 beobachtet werden. Der bestimmende Einfluss der Temperatur auf die Fr{\"u}hjahrsphasen und ihr modifizierender Einfluss auf die Herbstphasen konnte best{\"a}tigt werden. Es zeigt sich jedoch, dass - die Ph{\"a}nologie bestimmende Funktionen der Temperatur nicht mit einem globalen j{\"a}hrlichen CO2 Signal korreliert waren, welches als Index f{\"u}r die globale Erw{\"a}rmung verwendet wurde - ein Index f{\"u}r grossr{\"a}umige regionale Zirkulationsmuster (NAO-Index) nur zu einem kleinen Teil die beobachtete ph{\"a}nologischen Variabilit{\"a}t erkl{\"a}ren konnte. Das beobachtete unterschiedliche Trendverhalten zwischen fr{\"u}hen und sp{\"a}ten Fr{\"u}hjahrsphasen konnte auf die unterschiedliche Entwicklung von M{\"a}rz- und Apriltemperaturen zur{\"u}ckgef{\"u}hrt werden. W{\"a}hrend sich die M{\"a}rztemperaturen im Laufe des 20. Jahrhunderts mit einer zunehmenden Variabilit{\"a}t in den letzten 50 Jahren stetig erh{\"o}ht haben, haben sich die Apriltemperaturen zwischen dem Ende der 1940er und Mitte der 1980er merklich abgek{\"u}hlt und dann wieder deutlich erw{\"a}rmt. Es wurde geschlussfolgert, dass die Verfr{\"u}hungen in der Fr{\"u}hjahrsph{\"a}nologie in den letzten Dekaden Teile multi-dekadischer Fluktuationen sind, welche sich nach Spezies und relevanter saisonaler Temperatur unterscheiden. Aufgrund dieser Fluktuationen konnte kein Zusammenhang mit einem globalen Erw{\"a}rmungsignal gefunden werden. Im Durchschnitt haben sich alle betrachteten Fr{\"u}hjahrsphasen zwischen 1951 und 1999 in Naturr{\"a}umen in Deutschland zwischen 5 und 20 Tagen verfr{\"u}ht. Ein starker Unterschied in der Verfr{\"u}hung zwischen fr{\"u}hen und sp{\"a}ten Fr{\"u}hjahrsphasen liegt an deren erw{\"a}hntem unterschiedlichen Verhalten. Die Blattverf{\"a}rbung hat sich zwischen 1951 und 1999 f{\"u}r alle Spezies versp{\"a}tet, aber nach 1984 im Durchschnitt verfr{\"u}ht. Die VP hat sich in Deutschland zwischen 1951 und 1999 um ca. 10 Tage verl{\"a}ngert. Es ist haupts{\"a}chlich die {\"A}nderung in den Fr{\"u}hjahrphasen, die zu einer {\"A}nderung in der potentiell absorbierten Strahlung (PAS) f{\"u}hrt. Dar{\"u}ber hinaus sind es die sp{\"a}ten Fr{\"u}hjahrsphasen, die pro Tag Verfr{\"u}hung st{\"a}rker profitieren, da die zus{\"a}tzlichen Tage l{\"a}nger undw{\"a}rmer sind als dies f{\"u}r die fr{\"u}hen Phasen der Fall ist. Um die relative {\"A}nderung in PAS im Vergleich der Spezies abzusch{\"a}tzen, m{\"u}ssen allerdings auch die Ver{\"a}nderungen in den Herbstphasen ber{\"u}cksichtigt werden. Der deutliche Unterschied zwischen fr{\"u}hen und sp{\"a}ten Fr{\"u}hjahrsphasen konnte durch die Anwendung einer neuen Methode zur Konstruktion von Zeitreihen herausgearbeitet werden. Der neue methodische Ansatz erlaubte die Ableitung verl{\"a}sslicher 100-j{\"a}hriger Zeitreihen und die Konstruktion von lokalen kombinierten Zeitreihen, welche die Datenverf{\"u}gbarkeit f{\"u}r die Modellentwicklung erh{\"o}hten. Ausser analysierten Protokollierungsfehlern wurden mikroklimatische, genetische und Beobachtereinfl{\"u}sse als Quellen von Unsicherheit in ph{\"a}nologischen Daten identifiziert. Ph{\"a}nologischen Beobachtungen eines Ortes k{\"o}nnen sch{\"a}tzungsweise 24 Tage um das parametrische Mittel schwanken.Dies unterst{\"u}tzt die 30-Tage Regel f{\"u}r die Detektion von Ausreissern. Neue Ph{\"a}nologiemodelle, die den Blattaustrieb aus t{\"a}glichen Temperaturreihen simulieren, wurden entwickelt. Diese Modelle basieren auf einfachen Interaktionen zwischen aktivierenden und hemmenden Substanzen, welche die Entwicklungsstadien einer Pflanze bestimmen. Im Allgemeinen konnten die neuen Modelle die Beobachtungsdaten besser simulieren als die klassischen Modelle. Weitere Hauptresultate waren: - Der Bias der klassischen Modelle, d.h. {\"U}bersch{\"a}tzung von fr{\"u}hen und Untersch{\"a}tzung von sp{\"a}ten Beobachtungen, konnte reduziert, aber nicht vollst{\"a}ndig eliminiert werden. - Die besten Modellvarianten f{\"u}r verschiedene Spezies wiesen darauf hin, dass f{\"u}r die sp{\"a}ten Fr{\"u}hjahrsphasen die Tagesl{\"a}nge eine wichtigere Rolle spielt als f{\"u}r die fr{\"u}hen Phasen. - Die Vernalisation spielte gegen{\"u}ber den Temperaturen kurz vor dem Blattaustrieb nur eine untergeordnete Rolle.}, language = {en} } @misc{ClasonMairNienowetal.2015, author = {Clason, Caroline C. and Mair, D. W. F. and Nienow, P. W. and Bartholomew, I. D. and Sole, Andrew and Palmer, Steven and Schwanghart, Wolfgang}, title = {Modelling the transfer of supraglacial meltwater to the bed of Leverett Glacier, Southwest Greenland}, series = {Postprints der Universit{\"a}t Potsdam : Mathematisch-Naturwissenschaftliche Reihe}, journal = {Postprints der Universit{\"a}t Potsdam : Mathematisch-Naturwissenschaftliche Reihe}, number = {513}, issn = {1866-8372}, doi = {10.25932/publishup-40905}, url = {http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-409053}, pages = {16}, year = {2015}, abstract = {Meltwater delivered to the bed of the Greenland Ice Sheet is a driver of variable ice-motion through changes in effective pressure and enhanced basal lubrication. Ice surface velocities have been shown to respond rapidly both to meltwater production at the surface and to drainage of supraglacial lakes, suggesting efficient transfer of meltwater from the supraglacial to subglacial hydrological systems. Although considerable effort is currently being directed towards improved modelling of the controlling surface and basal processes, modelling the temporal and spatial evolution of the transfer of melt to the bed has received less attention. Here we present the results of spatially distributed modelling for prediction of moulins and lake drainages on the Leverett Glacier in Southwest Greenland. The model is run for the 2009 and 2010 ablation seasons, and for future increased melt scenarios. The temporal pattern of modelled lake drainages are qualitatively comparable with those documented from analyses of repeat satellite imagery. The modelled timings and locations of delivery of meltwater to the bed also match well with observed temporal and spatial patterns of ice surface speed-ups. This is particularly true for the lower catchment (< 1000 m a.s.l.) where both the model and observations indicate that the development of moulins is the main mechanism for the transfer of surface meltwater to the bed. At higher elevations (e.g. 1250-1500 m a.s.l.) the development and drainage of supraglacial lakes becomes increasingly important. At these higher elevations, the delay between modelled melt generation and subsequent delivery of melt to the bed matches the observed delay between the peak air temperatures and subsequent velocity speed-ups, while the instantaneous transfer of melt to the bed in a control simulation does not. Although both moulins and lake drainages are predicted to increase in number for future warmer climate scenarios, the lake drainages play an increasingly important role in both expanding the area over which melt accesses the bed and in enabling a greater proportion of surface melt to reach the bed.}, language = {en} } @misc{SchaeferBittmann2020, author = {Schaefer, Laura and Bittmann, Frank}, title = {Mechanotendography in Achillodynia shows reduced oscillation variability of pre-loaded Achilles tendon}, series = {Postprints der Universit{\"a}t Potsdam : Humanwissenschaftliche Reihe}, journal = {Postprints der Universit{\"a}t Potsdam : Humanwissenschaftliche Reihe}, number = {668}, issn = {1866-8364}, doi = {10.25932/publishup-48349}, url = {http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-483499}, pages = {13}, year = {2020}, abstract = {The present study focuses on an innovative approach in measuring the mechanical oscillations of pre-loaded Achilles tendon by using Mechanotendography (MTG) during application of a short yet powerful mechanical pressure impact. This was applied on the forefoot from the plantar side in direction of dorsiflexion, while the subject stood on the ball of the forefoot on one leg. Participants with Achilles tendinopathy (AT; n = 10) were compared to healthy controls (Con; n = 10). Five trials were performed on each side of the body. For evaluation, two intervals after the impulse began (0-100ms; 30-100ms) were cut from the MTG and pressure raw signals. The intrapersonal variability between the five trials in both intervals were evaluated using the arithmetic mean and coefficient of variation of the mean correlation (Spearman rank correlation) and the normalized averaged mean distances, respectively. The AT-group showed a significantly reduced variability in MTG compared to the Con-group (from p = 0.006 to p = 0.028 for different parameters). The 95\% confidence intervals (CI) of MTG results were disjoint, whereas the 95\% CIs of the pressure signals were similar (p = 0.192 to p = 0.601). We suggest from this work that the variability of mechanical tendon oscillations could be an indicative parameter of an altered Achilles tendon functionality.}, language = {en} } @misc{RottlerFranckeBuergeretal.2020, author = {Rottler, Erwin and Francke, Till and B{\"u}rger, Gerd and Bronstert, Axel}, title = {Long-term changes in central European river discharge for 1869-2016}, series = {Zweitver{\"o}ffentlichungen der Universit{\"a}t Potsdam : Mathematisch-Naturwissenschaftliche Reihe}, journal = {Zweitver{\"o}ffentlichungen der Universit{\"a}t Potsdam : Mathematisch-Naturwissenschaftliche Reihe}, number = {4}, issn = {1866-8372}, doi = {10.25932/publishup-51776}, url = {http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-517763}, pages = {22}, year = {2020}, abstract = {Recent climatic changes have the potential to severely alter river runoff, particularly in snow-dominated river basins. Effects of changing snow covers superimpose with changes in precipitation and anthropogenic modifications of the watershed and river network. In the attempt to identify and disentangle long-term effects of different mechanisms, we employ a set of analytical tools to extract long-term changes in river runoff at high resolution. We combine quantile sampling with moving average trend statistics and empirical mode decomposition and apply these tools to discharge data recorded along rivers with nival, pluvial and mixed flow regimes as well as temperature and precipitation data covering the time frame 1869-2016. With a focus on central Europe, we analyse the long-term impact of snow cover and precipitation changes along with their interaction with reservoir constructions. Our results show that runoff seasonality of snow-dominated rivers decreases. Runoff increases in winter and spring, while discharge decreases in summer and at the beginning of autumn. We attribute this redistribution of annual flow mainly to reservoir constructions in the Alpine ridge. During the course of the last century, large fractions of the Alpine rivers were dammed to produce hydropower. In recent decades, runoff changes induced by reservoir constructions seem to overlap with changes in snow cover. We suggest that Alpine signals propagate downstream and affect runoff far outside the Alpine area in river segments with mixed flow regimes. Furthermore, our results hint at more (intense) rain-fall in recent decades. Detected increases in high discharge can be traced back to corresponding changes in precipitation.}, language = {en} }