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Christoph Schneider

Researcher at Humboldt University of Berlin

Publications -  169
Citations -  3090

Christoph Schneider is an academic researcher from Humboldt University of Berlin. The author has contributed to research in topics: Glacier & Glacier mass balance. The author has an hindex of 25, co-authored 157 publications receiving 2535 citations. Previous affiliations of Christoph Schneider include University of Freiburg & RWTH Aachen University.

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A glacier inventory for the western Nyainqentanglha Range and the Nam Co Basin, Tibet, and glacier changes 1976-2009

TL;DR: The western Nyainqentanglha Range is located in the south-eastern centre of the Tibetan Plateau as discussed by the authors, and the region is of spe- cial interest for glacio-climatological research as it is influ- enced by both the continental climate of Central Asia and the Indian Monsoon system, and situated at the transition zone between temperate and subcontinental glaciers.
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Weather Observations Across the Southern Andes at 53°S

TL;DR: In this paper, regional variations of weather pattern were analyzed along a west-to-east profile across the Southern Andes (53°S), one of the most pronounced climate-divides in the world.
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Feasibility and Efficacy of High Dose Conformal Radiotherapy for Patients with Locally Advanced Pancreatic Carcinoma

TL;DR: The feasibility and efficacy of high dose conformal radiotherapy were examined in the treatment of patients with locally advanced, unresectable pancreatic carcinoma.
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Esho Quality Assurance Guidelines for Regional Hyperthermia

TL;DR: QA guidelines have been formulated based on the experience of the institutes which are active in clinical regional hyperthermia using radiative equipment and the focus is on what must be done not on how it should be done.
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Energy and mass balance of Zhadang glacier surface, central Tibetan Plateau

TL;DR: In this article, the authors examined the annual cycle of the surface energy and mass balance on Zhadang glacier in the central Tibetan Plateau over a 2 year period using a physically based energy-balance model forced by routine meteorological data.