@misc{OPUS4-64156,
  title     = {forum:logop{\"a}die 30.2016, 1},
  series = {Forum Logop{\"a}die : Zeitschrift des Deutschen Bundesverbandes f{\"u}r Logop{\"a}die e.V, dbl},
  volume    = {30},
  journal   = {Forum Logop{\"a}die : Zeitschrift des Deutschen Bundesverbandes f{\"u}r Logop{\"a}die e.V, dbl},
  number    = {1},
  publisher = {Schulz-Kirchner},
  address   = {Idstein},
  organization    = {Deutscher Bundesverband f{\"u}r Logop{\"a}die e.V.},
  issn      = {0932-0547},
  pages     = {79},
  year      = {2016},
  language  = {de}
}
@misc{OPUS4-64153,
  title     = {forum:logop{\"a}die 30.2016, 2},
  series = {Forum Logop{\"a}die : Zeitschrift des Deutschen Bundesverbandes f{\"u}r Logop{\"a}die e.V, dbl},
  volume    = {30},
  journal   = {Forum Logop{\"a}die : Zeitschrift des Deutschen Bundesverbandes f{\"u}r Logop{\"a}die e.V, dbl},
  number    = {2},
  publisher = {Schulz-Kirchner},
  address   = {Idstein},
  organization    = {Deutscher Bundesverband f{\"u}r Logop{\"a}die e.V.},
  issn      = {0932-0547},
  pages     = {78},
  year      = {2016},
  language  = {de}
}
@misc{OPUS4-64152,
  title     = {forum:logop{\"a}die 30.2016, 3},
  series = {Forum Logop{\"a}die : Zeitschrift des Deutschen Bundesverbandes f{\"u}r Logop{\"a}die e.V, dbl},
  volume    = {30},
  journal   = {Forum Logop{\"a}die : Zeitschrift des Deutschen Bundesverbandes f{\"u}r Logop{\"a}die e.V, dbl},
  number    = {3},
  publisher = {Schulz-Kirchner},
  address   = {Idstein},
  organization    = {Deutscher Bundesverband f{\"u}r Logop{\"a}die e.V.},
  issn      = {0932-0547},
  pages     = {66},
  year      = {2016},
  language  = {de}
}
@misc{OPUS4-64061,
  title     = {forum:logop{\"a}die 30.2016, 4},
  series = {Forum Logop{\"a}die : Zeitschrift des Deutschen Bundesverbandes f{\"u}r Logop{\"a}die e.V, dbl},
  volume    = {30},
  journal   = {Forum Logop{\"a}die : Zeitschrift des Deutschen Bundesverbandes f{\"u}r Logop{\"a}die e.V, dbl},
  number    = {4},
  publisher = {Schulz-Kirchner},
  address   = {Idstein},
  organization    = {Deutscher Bundesverband f{\"u}r Logop{\"a}die e.V.},
  issn      = {0932-0547},
  pages     = {71},
  year      = {2016},
  language  = {de}
}
@misc{OPUS4-64060,
  title     = {forum:logop{\"a}die 30.2016, 5},
  series = {Forum Logop{\"a}die : Zeitschrift des Deutschen Bundesverbandes f{\"u}r Logop{\"a}die e.V, dbl},
  volume    = {30},
  journal   = {Forum Logop{\"a}die : Zeitschrift des Deutschen Bundesverbandes f{\"u}r Logop{\"a}die e.V, dbl},
  number    = {5},
  publisher = {Schulz-Kirchner},
  address   = {Idstein},
  organization    = {Deutscher Bundesverband f{\"u}r Logop{\"a}die e.V.},
  issn      = {0932-0547},
  pages     = {83},
  year      = {2016},
  language  = {de}
}
@misc{OPUS4-64055,
  title     = {forum:logop{\"a}die 30.2016, 6},
  series = {Forum Logop{\"a}die : Zeitschrift des Deutschen Bundesverbandes f{\"u}r Logop{\"a}die e.V, dbl},
  volume    = {30},
  journal   = {Forum Logop{\"a}die : Zeitschrift des Deutschen Bundesverbandes f{\"u}r Logop{\"a}die e.V, dbl},
  number    = {6},
  publisher = {Schulz-Kirchner},
  address   = {Idstein},
  organization    = {Deutscher Bundesverband f{\"u}r Logop{\"a}die e.V.},
  issn      = {0932-0547},
  pages     = {71},
  year      = {2016},
  language  = {de}
}
@misc{SchickEckertPontiusetal.2016,
  author    = {Schick, Daniel and Eckert, Sebastian and Pontius, Niko and Mitzner, Rolf and F{\"o}hlisch, Alexander and Holldack, Karsten and Sorgenfrei, Nomi},
  title     = {Versatile soft X-ray-optical cross-correlator for ultrafast applications},
  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    = {1331},
  issn      = {1866-8372},
  doi       = {10.25932/publishup-43696},
  url       = {http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-436962},
  pages     = {054304-1 -- 054304-8},
  year      = {2016},
  abstract  = {We present an X-ray-optical cross-correlator for the soft (> 150 eV) up to the hard X-ray regime based on a molybdenum-silicon superlattice. The cross-correlation is done by probing intensity and position changes of superlattice Bragg peaks caused by photoexcitation of coherent phonons. This approach is applicable for a wide range of X-ray photon energies as well as for a broad range of excitation wavelengths and requires no external fields or changes of temperature. Moreover, the cross-correlator can be employed on a 10 ps or 100 fs time scale featuring up to 50\% total X-ray reflectivity and transient signal changes of more than 20\%. (C) 2016 Author(s).},
  language  = {en}
}
@misc{LichtDupontNivetPullenetal.2016,
  author    = {Licht, Alexis and Dupont-Nivet, Guillaume and Pullen, Alex and Kapp, Paul and Abels, Hemmo A. and Lai, Zulong and Guo, ZhaoJie and Abell, Jordan and Giesler, Dominique},
  title     = {Resilience of the Asian atmospheric circulation shown by paleogene dust provenance},
  series = {Postprints der Universit{\"a}t Potsdam : Mathematisch-Naturwissenschaftliche Reihe},
  journal   = {Postprints der Universit{\"a}t Potsdam : Mathematisch-Naturwissenschaftliche Reihe},
  number    = {1114},
  issn      = {1866-8372},
  doi       = {10.25932/publishup-43638},
  url       = {http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-436381},
  pages     = {8},
  year      = {2016},
  abstract  = {The onset of modern central Asian atmospheric circulation is traditionally linked to the interplay of surface uplift of the Mongolian and Tibetan-Himalayan orogens, retreat of the Paratethys sea from central Asia and Cenozoic global cooling. Although the role of these players has not yet been unravelled, the vast dust deposits of central China support the presence of arid conditions and modern atmospheric pathways for the last 25 million years (Myr). Here, we present provenance data from older (42-33 Myr) dust deposits, at a time when the Tibetan Plateau was less developed, the Paratethys sea still present in central Asia and atmospheric pCO(2) much higher. Our results show that dust sources and near-surface atmospheric circulation have changed little since at least 42 Myr. Our findings indicate that the locus of central Asian high pressures and concurrent aridity is a resilient feature only modulated by mountain building, global cooling and sea retreat.},
  language  = {en}
}
@misc{XiongStolleLuehretal.2016,
  author    = {Xiong, Chao and Stolle, Claudia and L{\"u}hr, Hermann and Park, Jaeheung and Fejer, Bela G. and Kervalishvili, Guram N.},
  title     = {Scale analysis of equatorial plasma irregularities derived from Swarm constellation},
  series = {Postprints der Universit{\"a}t Potsdam : Mathematisch-Naturwissenschaftliche Reihe},
  journal   = {Postprints der Universit{\"a}t Potsdam : Mathematisch-Naturwissenschaftliche Reihe},
  number    = {1112},
  issn      = {1866-8372},
  doi       = {10.25932/publishup-43184},
  url       = {http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-431842},
  pages     = {14},
  year      = {2016},
  abstract  = {In this study, we investigated the scale sizes of equatorial plasma irregularities (EPIs) using measurements from the Swarm satellites during its early mission and final constellation phases. We found that with longitudinal separation between Swarm satellites larger than 0.4°, no significant correlation was found any more. This result suggests that EPI structures include plasma density scale sizes less than 44 km in the zonal direction. During the Swarm earlier mission phase, clearly better EPI correlations are obtained in the northern hemisphere, implying more fragmented irregularities in the southern hemisphere where the ambient magnetic field is low. The previously reported inverted-C shell structure of EPIs is generally confirmed by the Swarm observations in the northern hemisphere, but with various tilt angles. From the Swarm spacecrafts with zonal separations of about 150 km, we conclude that larger zonal scale sizes of irregularities exist during the early evening hours (around 1900 LT).},
  language  = {en}
}
@misc{RadosavljevicLantuitPollardetal.2016,
  author    = {Radosavljevic, Boris and Lantuit, Hugues and Pollard, Wayne and Overduin, Pier Paul and Couture, Nicole and Sachs, Torsten and Helm, Veit and Fritz, Michael},
  title     = {Erosion and flooding-threats to coastal Infrastructure in the Arctic},
  series = {Postprints der Universit{\"a}t Potsdam : Mathematisch-Naturwissenschaftliche Reihe},
  journal   = {Postprints der Universit{\"a}t Potsdam : Mathematisch-Naturwissenschaftliche Reihe},
  number    = {996},
  issn      = {1866-8372},
  doi       = {10.25932/publishup-43227},
  url       = {http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-432279},
  pages     = {18},
  year      = {2016},
  abstract  = {Arctic coastal infrastructure and cultural and archeological sites are increasingly vulnerable to erosion and flooding due to amplified warming of the Arctic, sea level rise, lengthening of open water periods, and a predicted increase in frequency of major storms. Mitigating these hazards necessitates decision-making tools at an appropriate scale. The objectives of this paper are to provide such a tool by assessing potential erosion and flood hazards at Herschel Island, a UNESCO World Heritage candidate site. This study focused on Simpson Point and the adjacent coastal sections because of their archeological, historical, and cultural significance. Shoreline movement was analyzed using the Digital Shoreline Analysis System (DSAS) after digitizing shorelines from 1952, 1970, 2000, and 2011. For purposes of this analysis, the coast was divided in seven coastal reaches (CRs) reflecting different morphologies and/or exposures. Using linear regression rates obtained from these data, projections of shoreline position were made for 20 and 50 years into the future. Flood hazard was assessed using a least cost path analysis based on a high-resolution light detection and ranging (LiDAR) dataset and current Intergovernmental Panel on Climate Change sea level estimates. Widespread erosion characterizes the study area. The rate of shoreline movement in different periods of the study ranges from -5.5 to 2.7 m·a⁻¹ (mean -0.6 m·a⁻¹). Mean coastal retreat decreased from -0.6 m·a⁻¹ to -0.5 m·a⁻¹, for 1952-1970 and 1970-2000, respectively, and increased to -1.3 m·a⁻¹ in the period 2000-2011. Ice-rich coastal sections most exposed to wave attack exhibited the highest rates of coastal retreat. The geohazard map combines shoreline projections and flood hazard analyses to show that most of the spit area has extreme or very high flood hazard potential, and some buildings are vulnerable to coastal erosion. This study demonstrates that transgressive forcing may provide ample sediment for the expansion of depositional landforms, while growing more susceptible to overwash and flooding.},
  language  = {en}
}