@article{WienhoeferLindenmaierZehe2011,
  author    = {Wienh{\"o}fer, Jan and Lindenmaier, Falk and Zehe, Erwin},
  title     = {Challenges in understanding the hydrologic controls on the mobility of slow-moving landslides},
  series = {Vadose zone journal},
  volume    = {10},
  journal   = {Vadose zone journal},
  number    = {2},
  publisher = {Soil Science Society of America},
  address   = {Madison},
  issn      = {1539-1663},
  doi       = {10.2136/vzj2009.0182},
  pages     = {496 -- 511},
  year      = {2011},
  abstract  = {Slow-moving landslides are a wide-spread type of active mass movement, can cause severe damages to infrastructure, and may be a precursor of sudden catastrophic slope failures. Pore-water pressure is commonly regarded as the most important among a number of possible factors controlling landslide velocity. We used high-resolution monitoring data to explore the relations of landslide mobility and hydrologic processes at the Heumoser landslide in Austria, which is characterized by continuous slow movement along a shear zone. Movement rates showed a seasonality that was associated with elevated pore-water pressures. Pore pressure monitoring revealed a system of confined and separated aquifers with differing dynamics. Analysis of a simple infinite slope mobility model showed that small variations in parameters, along with measured pore pressure dynamics, provided a perfect match to our observations. Modeling showed a stabilizing effect of snow cover due to the additional load. This finding was supported by a multiple regression model, which further suggested that effective pore pressures at the slip surface were partially differing from the borehole observations and were related to preferential infiltration and subsurface flow in adjacent areas. It appears that in a setting like the Heumoser landslide, hydrologic processes delicately influence slope mobility through their control on pore pressure dynamics and the weight of the landslide body, which challenges observation and modeling. Moreover, it appears that their simplicity, and especially their high sensitivity to parameter variations, limits the conclusions that can be drawn from infinite slope models.},
  language  = {en}
}
@article{Wiemann2011,
  author    = {Wiemann, Dirk},
  title     = {Grenz{\"u}berschreitende Provinzialit{\"a}t: Richardsons Pamela und die verborgenen Ressourcen des europ{\"a}ischen Romans},
  isbn      = {978-3-89971-877-5},
  year      = {2011},
  language  = {de}
}
@article{Wiemann2011,
  author    = {Wiemann, Dirk},
  title     = {Der Salon : ein Modell kultureller Begegnungsr{\"a}umeweiblicher Pr{\"a}gung},
  isbn      = {978-3-89971-877-5},
  year      = {2011},
  language  = {de}
}
@article{Wiemann2011,
  author    = {Wiemann, Dirk},
  title     = {The boomerang effect of colonial practice : free-born englishmen and cavalier slaves},
  isbn      = {978-3-86956-090-8},
  year      = {2011},
  language  = {en}
}
@article{Wiemann2011,
  author    = {Wiemann, Dirk},
  title     = {Achievers, clones and pirates : Indian graphic novels},
  isbn      = {978-3- 86821-332-4},
  year      = {2011},
  language  = {en}
}
@article{Wiemann2011,
  author    = {Wiemann, Dirk},
  title     = {Michael Arditti and the return of "Totalitarianism"},
  issn      = {0171-1695},
  year      = {2011},
  language  = {en}
}
@article{Wiemann2011,
  author    = {Wiemann, Dirk},
  title     = {The boomerang effect of colonial practice},
  series = {Mobilisierte Kulturen},
  journal   = {Mobilisierte Kulturen},
  number    = {1},
  issn      = {2192-3019},
  url       = {http://nbn-resolving.de/urn:nbn:de:kobv:517-opus-57445},
  pages     = {353 -- 376},
  year      = {2011},
  language  = {en}
}
@article{WielandDalchowSommeretal.2011,
  author    = {Wieland, Ralf and Dalchow, Claus and Sommer, Michael and Fukuda, Kyoko},
  title     = {Multi-Scale Landscape Analysis (MSLA) a method to identify correlation of relief with ecological point data},
  series = {Ecological informatics : an international journal on ecoinformatics and computational ecolog},
  volume    = {6},
  journal   = {Ecological informatics : an international journal on ecoinformatics and computational ecolog},
  number    = {2},
  publisher = {Elsevier},
  address   = {Amsterdam},
  issn      = {1574-9541},
  doi       = {10.1016/j.ecoinf.2010.09.002},
  pages     = {164 -- 169},
  year      = {2011},
  abstract  = {A common problem in ecology is identifying the relationship between relief and site properties obtainable only by point measurements. The method of Multi-Scale Landscape Analysis (MSLA) identifies such correlations. MSLA combines frequency filtering of the digital elevation model (DEM) with an estimation of the optimum filter coefficients using an optimization procedure. Tested using point data of soil decarbonation from a German young moraine landscape, MSLA provided significant results. Implemented within open source software SAMT. MSLA is comfortable and flexible to use, offering applications for numerous other spatial analysis problems.},
  language  = {en}
}
@article{WiederkehrBousquetZiemannetal.2011,
  author    = {Wiederkehr, Michael and Bousquet, Romain and Ziemann, Martin Andreas and Berger, Alfons and Schmid, Stefan M.},
  title     = {3-D assessment of peak-metamorphic conditions by Raman spectroscopy of carbonaceous material an example from the margin of the Lepontine dome (Swiss Central Alps)},
  series = {International journal of earth sciences},
  volume    = {100},
  journal   = {International journal of earth sciences},
  number    = {5},
  publisher = {Springer},
  address   = {New York},
  issn      = {1437-3254},
  doi       = {10.1007/s00531-010-0622-2},
  pages     = {1029 -- 1063},
  year      = {2011},
  abstract  = {This study monitors regional changes in the crystallinity of carbonaceous matter (CM) by applying Micro-Raman spectroscopy to a total of 214 metasediment samples (largely so-called Bundnerschiefer) dominantly metamorphosed under blueschist- to amphibolite-facies conditions. They were collected within the northeastern margin of the Lepontine dome and easterly adjacent areas of the Swiss Central Alps. Three-dimensional mapping of isotemperature contours in map and profile views shows that the isotemperature contours associated with the Miocene Barrow-type Lepontine metamorphic event cut across refolded nappe contacts, both along and across strike within the northeastern margin of the Lepontine dome and adjacent areas. Further to the northeast, the isotemperature contours reflect temperatures reached during the Late Eocene subduction-related blueschist-facies event and/or during subsequent near-isothermal decompression; these contours appear folded by younger, large-scale post-nappe-stacking folds. A substantial jump in the recorded maximum temperatures across the tectonic contact between the frontal Adula nappe complex and surrounding metasediments indicates that this contact accommodated differential tectonic movement of the Adula nappe with respect to the enveloping Bundnerschiefer after maximum temperatures were reached within the northern Adula nappe, i.e. after Late Eocene time.},
  language  = {en}
}
@misc{Widdau2011,
  author    = {Widdau, Christoph Sebastian},
  title     = {Scheler, M., Die Idee des Friedens und der Pazifismus; Berlin, Der Neue Geistverl., 1931},
  isbn      = {978-3-941880-21-4},
  year      = {2011},
  language  = {de}
}