@misc{BlumensteinKrueger1995,
  author    = {Blumenstein, Oswald and Kr{\"u}ger, Wolfgang},
  title     = {W{\"u}thrich, C., Die biologische Aktivit{\"a}t arktischer B{\"o}den mit spezieller Ber{\"u}cksichtigung ornithogen eutrophierter Gebiete (Spitzbergen und Finnmark); Basel, Wepf, 1994},
  year      = {1995},
  language  = {de}
}
@misc{Heller2007,
  author    = {Heller, Wilfried},
  title     = {Wolf, J., Entwicklung der ethnischen Struktur des Banats 1890 - 1992; Berlin, Borntraeger, 1999},
  year      = {2007},
  language  = {de}
}
@misc{Felgentreff1997,
  author    = {Felgentreff, Carsten},
  title     = {Weiss, F., Die dreisten Frauen, eine Begegnung in Papua-Neuguinea; Frankfurt am Main, Fischer-Taschenbuch- Verl., 1996},
  year      = {1997},
  language  = {de}
}
@misc{Jessel2002,
  author    = {Jessel, Beate},
  title     = {Turner, M. G., Landscape ecology in theory and practice : pattern and process; New York, Springer, 2001},
  year      = {2002},
  language  = {en}
}
@misc{HussBookhagenHuggeletal.2017,
  author    = {Huss, Matthias and Bookhagen, Bodo and Huggel, C. and Jacobsen, Dean and Bradley, Raymond S. and Clague, J. J. and Vuille, Mathias and Buytaert, Wouter and Cayan, D. R. and Greenwood, G. and Mark, B. G. and Milner, A. M. and Weingartner, Rolf and Winder, M.},
  title     = {Toward mountains without permanent snow and ice},
  series = {Earths future},
  volume    = {5},
  journal   = {Earths future},
  publisher = {Wiley},
  address   = {Hoboken},
  issn      = {2328-4277},
  doi       = {10.1002/2016EF000514},
  pages     = {418 -- 435},
  year      = {2017},
  abstract  = {The cryosphere in mountain regions is rapidly declining, a trend that is expected to accelerate over the next several decades due to anthropogenic climate change. A cascade of effects will result, extending from mountains to lowlands with associated impacts on human livelihood, economy, and ecosystems. With rising air temperatures and increased radiative forcing, glaciers will become smaller and, in some cases, disappear, the area of frozen ground will diminish, the ratio of snow to rainfall will decrease, and the timing and magnitude of both maximum and minimum streamflow will change. These changes will affect erosion rates, sediment, and nutrient flux, and the biogeochemistry of rivers and proglacial lakes, all of which influence water quality, aquatic habitat, and biotic communities. Changes in the length of the growing season will allow low-elevation plants and animals to expand their ranges upward. Slope failures due to thawing alpine permafrost, and outburst floods from glacier-and moraine-dammed lakes will threaten downstream populations.Societies even well beyond the mountains depend on meltwater from glaciers and snow for drinking water supplies, irrigation, mining, hydropower, agriculture, and recreation. Here, we review and, where possible, quantify the impacts of anticipated climate change on the alpine cryosphere, hydrosphere, and biosphere, and consider the implications for adaptation to a future of mountains without permanent snow and ice.},
  language  = {en}
}
@misc{ManzoniCapekPoradaetal.2018,
  author    = {Manzoni, Stefano and Capek, Petr and Porada, Philipp and Thurner, Martin and Winterdahl, Mattias and Beer, Christian and Bruchert, Volker and Frouz, Jan and Herrmann, Anke M. and Lindahl, Bjorn D. and Lyon, Steve W. and Šantrůčkov{\´a}, Hana and Vico, Giulia and Way, Danielle},
  title     = {Reviews and syntheses},
  series = {Biogeosciences},
  volume    = {15},
  journal   = {Biogeosciences},
  number    = {19},
  publisher = {Copernicus},
  address   = {G{\"o}ttingen},
  issn      = {1726-4170},
  doi       = {10.5194/bg-15-5929-2018},
  pages     = {5929 -- 5949},
  year      = {2018},
  abstract  = {The cycling of carbon (C) between the Earth surface and the atmosphere is controlled by biological and abiotic processes that regulate C storage in biogeochemical compartments and release to the atmosphere. This partitioning is quantified using various forms of C-use efficiency (CUE) - the ratio of C remaining in a system to C entering that system. Biological CUE is the fraction of C taken up allocated to biosynthesis. In soils and sediments, C storage depends also on abiotic processes, so the term C-storage efficiency (CSE) can be used. Here we first review and reconcile CUE and CSE definitions proposed for autotrophic and heterotrophic organisms and communities, food webs, whole ecosystems and watersheds, and soils and sediments using a common mathematical framework. Second, we identify general CUE patterns; for example, the actual CUE increases with improving growth conditions, and apparent CUE decreases with increasing turnover. We then synthesize > 5000CUE estimates showing that CUE decreases with increasing biological and ecological organization - from uni-cellular to multicellular organisms and from individuals to ecosystems. We conclude that CUE is an emergent property of coupled biological-abiotic systems, and it should be regarded as a flexible and scale-dependent index of the capacity of a given system to effectively retain C.},
  language  = {en}
}
@misc{Jessel2002,
  author    = {Jessel, Beate},
  title     = {Ph{\"a}nomen Landschaft},
  year      = {2002},
  language  = {de}
}
@misc{Jessel2004,
  author    = {Jessel, Beate},
  title     = {Michel-Fabian, P., Werte in der Umweltplanung : ethische Dimensionen und L{\"o}sungen am Beispiel der UVS ; Dortmund, Dortmunder Vertrieb f{\"u}r Bau- und Planungsliteratur, 2003},
  issn      = {0034-0111},
  year      = {2004},
  language  = {de}
}
@misc{Jessel2001,
  author    = {Jessel, Beate},
  title     = {Meyh{\"o}fer, T., Umsetzungsdefizite bei Kompensationsmaßnahmen in Bebauungspl{\"a}nen, Ursachen und L{\"o}sungswege; Berlin, Rhombos-Ver., 2000},
  year      = {2001},
  language  = {de}
}
@misc{Jessel2001,
  author    = {Jessel, Beate},
  title     = {Mengel, A., Stringenz und Nachvollziehbarkeit in der fachbezogenen Umweltplanung; Darmstadt, Inst. WAR, 2001},
  year      = {2001},
  language  = {de}
}
@misc{Szaramowicz2002,
  author    = {Szaramowicz, Martin},
  title     = {Kr{\"o}nert, R. (Hrsg.): Landscape Balance and Landscape Assessment; Berlin, Springer, 2001},
  year      = {2002},
  language  = {en}
}
@misc{Roessling2002,
  author    = {R{\"o}ßling, Holger},
  title     = {Kreibich, R. (Hrsg.), Global Change=Globaler Wandel, Ursachen und L{\"o}sungsans{\"a}tze; Berlin, Berlin- Verl. Spitz, 2000},
  year      = {2002},
  language  = {de}
}
@misc{Heller2007,
  author    = {Heller, Wilfried},
  title     = {Knappe, E., Transformation der Landwirtschaft in Mittel- und S{\"u}dosteuropa; Berlin, Borntr{\"a}ger, 2004},
  year      = {2007},
  language  = {de}
}
@misc{Heller1998,
  author    = {Heller, Wilfried},
  title     = {Kleger, H., Metropolitane Transformation durch urbane Regime, Berlin-Brandenburg auf dem Weg zu regionaler Handlungsf{\"a}higkeit; Amsterdam, Verl. Fakultas, 1996},
  year      = {1998},
  language  = {de}
}
@misc{Jessel2001,
  author    = {Jessel, Beate},
  title     = {Hohl, W., Landschaftsplanung : {\"A}sthetische und rekreative Aspekte; Berlin, Patzer, 2001},
  year      = {2001},
  language  = {de}
}
@misc{Jessel2003,
  author    = {Jessel, Beate},
  title     = {Helming, K. (Hrsg.), Sustainable Development of Multifunctional Landscapes; Berlin, Springer, 2003},
  year      = {2003},
  language  = {en}
}
@misc{Roessling2001,
  author    = {R{\"o}ßling, Holger},
  title     = {Ekardt, F., Steuerungsdefizite im Umweltrecht; Sinzheim, Pro Universitate Verl., 2001},
  year      = {2001},
  language  = {de}
}
@misc{FanScaringiKorupetal.2019,
  author    = {Fan, Xuanmei and Scaringi, Gianvito and Korup, Oliver and West, A. Joshua and van Westen, Cees J. and Tanyas, Hakan and Hovius, Niels and Hales, Tristram C. and Jibson, Randall W. and Allstadt, Kate E. and Zhang, Limin and Evans, Stephen G. and Xu, Chong and Li, Gen and Pei, Xiangjun and Xu, Qiang and Huang, Runqiu},
  title     = {Earthquake-Induced Chains of Geologic Hazards},
  series = {Reviews of geophysics},
  volume    = {57},
  journal   = {Reviews of geophysics},
  number    = {2},
  publisher = {American Geophysical Union},
  address   = {Washington},
  issn      = {8755-1209},
  doi       = {10.1029/2018RG000626},
  pages     = {421 -- 503},
  year      = {2019},
  abstract  = {Large earthquakes initiate chains of surface processes that last much longer than the brief moments of strong shaking. Most moderate- and large-magnitude earthquakes trigger landslides, ranging from small failures in the soil cover to massive, devastating rock avalanches. Some landslides dam rivers and impound lakes, which can collapse days to centuries later, and flood mountain valleys for hundreds of kilometers downstream. Landslide deposits on slopes can remobilize during heavy rainfall and evolve into debris flows. Cracks and fractures can form and widen on mountain crests and flanks, promoting increased frequency of landslides that lasts for decades. More gradual impacts involve the flushing of excess debris downstream by rivers, which can generate bank erosion and floodplain accretion as well as channel avulsions that affect flooding frequency, settlements, ecosystems, and infrastructure. Ultimately, earthquake sequences and their geomorphic consequences alter mountain landscapes over both human and geologic time scales. Two recent events have attracted intense research into earthquake-induced landslides and their consequences: the magnitude M 7.6 Chi-Chi, Taiwan earthquake of 1999, and the M 7.9 Wenchuan, China earthquake of 2008. Using data and insights from these and several other earthquakes, we analyze how such events initiate processes that change mountain landscapes, highlight research gaps, and suggest pathways toward a more complete understanding of the seismic effects on the Earth's surface.},
  language  = {en}
}
@misc{vanderKroefKoszinskiGrinatetal.2020,
  author    = {van der Kroef, Ilona and Koszinski, Sylvia and Grinat, Michael and van der Meij, Marijn W. and Hierold, Wilfried and S{\"u}dekum, Wolfgang and Sommer, Michael},
  title     = {Digital mapping of buried soil horizons using 2D and pseudo-3D geoelectrical measurements in a ground moraine landscape},
  series = {European journal of soil science : EJSS},
  volume    = {71},
  journal   = {European journal of soil science : EJSS},
  number    = {1},
  publisher = {Wiley},
  address   = {Hoboken},
  issn      = {1351-0754},
  pages     = {10 -- 26},
  year      = {2020},
  abstract  = {The identification of buried soil horizons in agricultural landscapes helps to quantify sediment budgets and erosion-related carbon dynamics. High-resolution mapping of buried horizons using conventional soil surveys is destructive and time consuming. Geoelectrical sensors can offer a fast and non-destructive alternative for determining horizon positions and properties. In this paper, we compare the suitability of several geoelectrical methods for measuring the depth to buried horizons (Apb, Ahb and Hab) in the hummocky ground moraine landscape of northeastern Germany. Soil profile descriptions were developed for 269 locations within a 6-ha experimental field "CarboZALF-D". A stepwise linear discriminant analysis (LDA) estimated the lateral position of the buried horizons using electromagnetic induction data and terrain attributes. To predict the depth of a buried horizon, multiple linear regression (MLR) was used for both a 120-m transect and a 0.2-ha pseudo-three-dimensional (3D) area. At these scales, apparent electrical conductivity (ECa), electrical resistivity (ER) and terrain attributes were used as independent variables. The LDA accurately predicted Apb- and Ahb-horizons (a correct classification of 93\%). The LDA of the Hab-horizon had a misclassification of 24\%, which was probably related to the smaller test set and the higher depth of this horizon. The MLR predicted the depth of the Apb-, Ahb- and Hab-horizons with relative root mean square errors (RMSEs) of 7, 3 and 13\%, respectively, in the pseudo-3D area. MLR had a lower accuracy for the 2D transect compared to the pseudo-3D area. Overall, the use of LDA and MLR has been an efficient methodological approach for predicting buried horizon positions. Highlights The suitability of geoelectrical measurements for digital modelling of diagnostic buried soil horizons was determined. LDA and MLR were used to detect multiple horizons with geoelectrical devices and terrain attributes. Geoelectrical variables were significant predictors of the position of the target soil horizons. The use of these tested digital technologies gives an opportunity to develop high-resolution soil mapping procedures.},
  language  = {en}
}
@misc{Felgentreff2002,
  author    = {Felgentreff, Carsten},
  title     = {Dickhardt, M., Das R{\"a}umliche des Kulturellen, Entwurf zu einer kulturanthropologischen Raumtheorie am Beispiel Fiji; M{\"u}nster, Lit, 2001},
  year      = {2002},
  language  = {de}
}
@misc{Heller1999,
  author    = {Heller, Wilfried},
  title     = {Buchhofer, E. (Hrsg.), Agrarwirtschaft und l{\"a}ndlicher Raum Ostmitteleuropas in der Transformation; Marburg, Herder-Inst., 1998},
  year      = {1999},
  language  = {de}
}
@misc{Heller1999,
  author    = {Heller, Wilfried},
  title     = {Brunn, G. (Hrsg.), Regionen und Regionsbildung in Europa, Konzeptionen der Forschung und empirische Befunden; Baden-Baden, Nomos, 1996},
  year      = {1999},
  language  = {de}
}
@misc{Jessel2001,
  author    = {Jessel, Beate},
  title     = {Ausgleich nur auf dem Papier},
  year      = {2001},
  language  = {de}
}
@misc{Heller1999,
  author    = {Heller, Wilfried},
  title     = {Albrecht, V. (Hrsg.), Ungarn in Europa, gesellschaftlicher und raumstruktureller Wandel in Vergangenheit und Gegenwart; Frankfurt am Main, Inst. f{\"u}r Didaktik der Geographie, 1998},
  year      = {1999},
  language  = {de}
}
@misc{Siemer2002,
  author    = {Siemer, Julia},
  title     = {Alban, E. (Hrsg.) Regionalatlas Rhein-Main, Natur-Gesellschaft-Wirtschaft; Frankfurt am Main, Selbstverl. Rhein- Mainische Forschung, 2000},
  year      = {2002},
  language  = {de}
}