Zobrazeno 1 - 10
of 17
pro vyhledávání: '"Henning Franke"'
Autor:
Markus Eisenbach, Henning Franke, Erik Franze, Mona Köhler, Dustin Aganian, Daniel Seichter, Horst-Michael Gross
Publikováno v:
Automation, Vol 5, Iss 3, Pp 373-406 (2024)
Object detection is a crucial capability of autonomous agents for human–robot collaboration, as it facilitates the identification of the current processing state. In industrial scenarios, it is uncommon to have comprehensive knowledge of all the ob
Externí odkaz:
https://doaj.org/article/99e533fc7fdc4f72b88dc1126192a075
Autor:
Henning Franke, Marco A. Giorgetta
Publikováno v:
Journal of Advances in Modeling Earth Systems, Vol 16, Iss 10, Pp n/a-n/a (2024)
Abstract This study presents the first attempt to simulate a full cycle of the quasi‐biennial oscillation (QBO) in a global storm‐resolving model (GSRM) that explicitly simulates deep convection and gravity waves instead of parameterizing them. U
Externí odkaz:
https://doaj.org/article/8555e7e611f445f4aad5c7081ea97b44
Autor:
Debra K. Weisenstein, Daniele Visioni, Henning Franke, Ulrike Niemeier, Sandro Vattioni, Gabriel Chiodo, Thomas Peter, David W. Keith
Publikováno v:
Atmospheric Chemistry and Physics. 22:2955-2973
Studies of stratospheric solar geoengineering have tended to focus on modification of the sulfuric acid aerosol layer, and almost all climate model experiments that mechanistically increase the sulfuric acid aerosol burden assume injection of SO2. A
Autor:
Ilaria Quaglia, Claudia Timmreck, Ulrike Niemeier, Daniele Visioni, Giovanni Pitari, Christina Brodowsky, Christoph Brühl, Sandip S. Dhomse, Henning Franke, Anton Laakso, Graham W. Mann, Eugene Rozanov, Timofei Sukhodolov
Publikováno v:
Atmospheric Chemistry and Physics, 23 (2)
Atmospheric Chemistry and Physics
Atmospheric Chemistry and Physics
A previous model intercomparison of the Tambora aerosol cloud has highlighted substantial differences among simulated volcanic aerosol properties in the pre-industrial stratosphere and has led to questions about the applicability of global aerosol mo
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::d2dfc870570af688c3d26e573cee10ca
Autor:
Ilaria Quaglia, Claudia Timmreck, Ulrike Niemeier, Daniele Visioni, Giovanni Pitari, Christoph Brühl, Sandip Dhomse, Henning Franke, Anton Laakso, Graham Mann, Eugene Rozanov, Timofei Sukhodolov
Recent model inter-comparison studies highlighted model discrepancies in reproducing the climatic impacts of large explosive volcanic eruptions, calling into question the reliability of global aerosol model simulations for future scenarios. Here, we
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::4c9f7f3973f32f6eeed9ad0411626df1
https://acp.copernicus.org/preprints/acp-2022-514/
https://acp.copernicus.org/preprints/acp-2022-514/
Autor:
Ilaria Quaglia, Claudia Timmreck, Ulrike Niemeier, Daniele Visioni, Giovanni Pitari, Christoph Brühl, Sandip Dhomse, Henning Franke, Anton Laakso, Graham Mann, Eugene Rozanov, Timofei Sukhodolov
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::cd02ac39647e01eea043631582a59095
https://doi.org/10.5194/acp-2022-514-supplement
https://doi.org/10.5194/acp-2022-514-supplement
Autor:
Marco A. Giorgetta, William Sawyer, Xavier Lapillonne, Panagiotis Adamidis, Dmitry Alexeev, Valentin Clément, Remo Dietlicher, Jan Frederik Engels, Monika Esch, Henning Franke, Claudia Frauen, Walter M. Hannah, Benjamin R. Hillman, Luis Kornblueh, Philippe Marti, Matthew R. Norman, Robert Pincus, Sebastian Rast, Daniel Reinert, Reiner Schnur, Uwe Schulzweida, Bjorn Stevens
Publikováno v:
eISSN
Geoscientific Model Development, 15 (18)
Geoscientific Model Development
Geoscientific Model Development, 15 (18)
Geoscientific Model Development
Classical numerical models for the global atmosphere, as used for numerical weather forecasting or climate research, have been developed for conventional central processing unit (CPU) architectures. This hinders the employment of such models on curre
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::ebc8d88901073b24bc297ecd598f38c7
https://doi.org/10.5194/egusphere-2022-152
https://doi.org/10.5194/egusphere-2022-152
Autor:
Julia Windmiller, Bjorn Stevens, Henning Franke, Ilaria Quaglia, Katharina Stolla, Ronny Engelmann, Jonas Lehmke, Hugo Rubio, Thomas Ruhtz, Annett Skupin
The intertropical convergence zone (ITCZ) plays a central role for the tropical weather and climate and structures the large-scale circulation. As a result, the ITCZ has long been an intensively studied research topic, with most studies of the ITCZ f
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e95f99f1a306ee6a89548c367a78a1f5
https://doi.org/10.5194/dach2022-283
https://doi.org/10.5194/dach2022-283
Autor:
Ulrike Niemeier, David W. Keith, Henning Franke, Gabriel Chiodo, Debra K. Weisenstein, Daniele Visioni, Thomas Peter, Sandro Vattioni
Analyses of stratospheric solar geoengineering have focused on sulfate aerosol, and almost all climate model experiments on sulfate aerosol have assumed injection of SO2. Yet continuous injection of SO2 may produce overly large aerosols. Injection of
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::365d65c56b34f8c2098ac56e6feebdd6
https://acp.copernicus.org/preprints/acp-2021-569/
https://acp.copernicus.org/preprints/acp-2021-569/
Publikováno v:
Atmospheric Chemistry and Physics
A known adverse side effect of stratospheric aerosol modification (SAM) is the modification of the quasi-biennial oscillation (QBO), which is caused by the stratospheric heating associated with an artificial aerosol layer. Multiple studies found the
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::6bca8338d65454cd18d6f089d5f0dcc2
https://hdl.handle.net/21.11116/0000-0007-7DD0-221.11116/0000-0008-8592-C21.11116/0000-0008-C19C-E21.11116/0000-0008-C19D-D21.11116/0000-0007-7D90-A
https://hdl.handle.net/21.11116/0000-0007-7DD0-221.11116/0000-0008-8592-C21.11116/0000-0008-C19C-E21.11116/0000-0008-C19D-D21.11116/0000-0007-7D90-A