David Schubert
University of Cologne
4 Papers
5 Citations
David Schubert is an academic researcher from University of Cologne. The author has contributed to research in topics: Glacier & Precipitation. The author has an hindex of 2, co-authored 3 publications. Previous affiliations of David Schubert include Ostwestfalen-Lippe University of Applied Sciences.
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Papers
Soil organic carbon sequestration in agricultural long-term field experiments as derived from particulate and mineral-associated organic matter
Christoph Dr Just,Martin Armbruster,Dietmar Barkusky,Michael Baumecker,Michael Diepolder,Thomas F. Döring,Bernd Honermeier,M. Jate,Ines Merbach,David Schubert,Franziska Schulz,Kathlin Schweitzer,Sabine J. Seidel,Michael Sommer,Heide Spiegel,Ulrich Thumm,Peer Urbatzka,Jörg Zimmer,Ingrid Kögel-Knabner,Martin Wiesmeier +19 more
TL;DR: In this article , the authors analyzed changes in fast-cycling particulate organic matter (POM) and slow-cycled mineral-associated organic matter induced by common management practices, i.e., fertilization and crop rotation in topsoils from 25 Central European long-term field experiments.
25
Statistical‐dynamical downscaling of precipitation for Vietnam: methodology and evaluation for the recent climate
David Schubert,David Schubert,Roderick van der Linden,Mark Reyers,Andreas H. Fink,Klaus Massmeyer,Joaquim G. Pinto,Joaquim G. Pinto +7 more
TL;DR: In this article, a statistical-dynamical downscaling approach that combines weather typing and dynamical scaling is developed to obtain a high-resolution precipitation climatology for tropical Southeast Asia.
6
Future Climate Change and Its Impact on Runoff Generation from the Debris-Covered Inylchek Glaciers, Central Tian Shan, Kyrgyzstan
Wilfried Hagg,Elisabeth Mayr,Birgit Mannig,Mark Reyers,David Schubert,Joaquim G. Pinto,Juliane Peters,Tino Pieczonka,M. Juen,Tobias Bolch,Heiko Paeth,Christoph Mayer +11 more
TL;DR: In this paper, a conceptual hydrological model able to incorporate discharge from debris-covered glacier areas is presented, which is used to simulate glacier melt and subsequent runoff in the past (1970/1971-1999/2000) and future (2070/2071-2099/2100).