Zobrazeno 1 - 10
of 23
pro vyhledávání: '"Sebastian Milinski"'
Autor:
Dirk Olonscheck, Laura Suarez‐Gutierrez, Sebastian Milinski, Goratz Beobide‐Arsuaga, Johanna Baehr, Friederike Fröb, Tatiana Ilyina, Christopher Kadow, Daniel Krieger, Hongmei Li, Jochem Marotzke, Étienne Plésiat, Martin Schupfner, Fabian Wachsmann, Lara Wallberg, Karl‐Hermann Wieners, Sebastian Brune
Publikováno v:
Journal of Advances in Modeling Earth Systems, Vol 15, Iss 10, Pp n/a-n/a (2023)
Abstract Single‐model initial‐condition large ensembles are powerful tools to quantify the forced response, internal climate variability, and their evolution under global warming. Here, we present the CMIP6 version of the Max Planck Institute Gra
Externí odkaz:
https://doaj.org/article/ecb2ea7c29e44b8ab477340be80f824a
Autor:
Nicola Maher, Sebastian Milinski, Laura Suarez‐Gutierrez, Michael Botzet, Mikhail Dobrynin, Luis Kornblueh, Jürgen Kröger, Yohei Takano, Rohit Ghosh, Christopher Hedemann, Chao Li, Hongmei Li, Elisa Manzini, Dirk Notz, Dian Putrasahan, Lena Boysen, Martin Claussen, Tatiana Ilyina, Dirk Olonscheck, Thomas Raddatz, Bjorn Stevens, Jochem Marotzke
Publikováno v:
Journal of Advances in Modeling Earth Systems, Vol 11, Iss 7, Pp 2050-2069 (2019)
Abstract The Max Planck Institute Grand Ensemble (MPI‐GE) is the largest ensemble of a single comprehensive climate model currently available, with 100 members for the historical simulations (1850–2005) and four forcing scenarios. It is currently
Externí odkaz:
https://doaj.org/article/f0be17f8f7e7402891a276a949d98f0e
Publikováno v:
Earth System Dynamics
The El Niño–Southern Oscillation (ENSO) occurs in three phases: neutral, warm (El Niño), and cool (La Niña). While classifying El Niño and La Niña is relatively straightforward, El Niño events can be broadly classified into two types: central
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::82df077354063fc2aab14b76630623b5
https://doi.org/10.5194/esd-13-1289-2022
https://doi.org/10.5194/esd-13-1289-2022
Projecting how temperature variability is likely to change in the future is important for understanding future extreme events. This comes from the fact that such extremes can change due to both changes in the mean climate and its variability. The rec
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d3f8a0ba6e33f76d248cbf5a21707170
https://doi.org/10.5194/egusphere-egu23-10531
https://doi.org/10.5194/egusphere-egu23-10531
Autor:
Thomas Rackow, Xabier Pedruzo Bagazgoitia, Tobias Becker, Sebastian Milinski, Irina Sandu, Michail Diamantakis, Helge F. Goessling, Ioan Hadade, Jan Hegewald, Nikolay Koldunov, Alexei Koldunov, Tobias Kölling, Kristian Mogensen, Dmitry Sidorenko, Jan Streffing, Nils Wedi, Lorenzo Zampieri, Florian Ziemen
Global coupled simulations that can resolve atmospheric storms and mesoscale oceanic features at the kilometre-scale have recently become possible to run over short time slices, for example on a seasonal timescale. Here we give an overview of the fir
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::10926403a942d1c9a08e6da53ade08df
https://doi.org/10.5194/egusphere-egu23-16453
https://doi.org/10.5194/egusphere-egu23-16453
Autor:
Dirk Olonscheck, Sebastian Brune, Laura Suarez-Gutierrez, Goratz Beobide-Arsuaga, Johanna Baehr, Friederike Fröb, Lara Hellmich, Tatiana Ilyina, Christopher Kadow, Daniel Krieger, Hongmei Li, Jochem Marotzke, Étienne Plésiat, Martin Schupfner, Fabian Wachsmann, Karl-Hermann Wieners, Sebastian Milinski
We present the CMIP6 version of the Max Planck Institute-Grand Ensemble (MPI-GE CMIP6) with 30 realisations for the historical period and five emission scenarios. The power of MPI-GE CMIP6 goes beyond its predecessor ensemble MPI-GE by providing high
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::36a4833eb9ea3869ba33da225d68f31c
https://doi.org/10.5194/egusphere-egu23-14556
https://doi.org/10.5194/egusphere-egu23-14556
Autor:
Nicola Maher, Robert C. Jnglin Wills, Pedro DiNezio, Jeremy Klavans, Sebastian Milinski, Sara C. Sanchez, Samantha Stevenson, Malte F. Stuecker, Xian Wu
Future changes in the El Niño–Southern Oscillation (ENSO) are uncertain, both because future projections differ between climate models and because the large internal variability of ENSO clouds the diagnosis of forced changes in observations and in
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::ea436243f4212b030f774ed12182a7f8
https://esd.copernicus.org/preprints/esd-2022-26/
https://esd.copernicus.org/preprints/esd-2022-26/
Autor:
Nicola Maher, Robert C. Jnglin Wills, Pedro DiNezio, Jeremy Klavans, Sebastian Milinski, Sara C. Sanchez, Samantha Stevenson, Malte F. Stuecker, Xian Wu
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b2661b90bc0afdcabcb81da4dcbe91ee
https://doi.org/10.5194/esd-2022-26-supplement
https://doi.org/10.5194/esd-2022-26-supplement
Publikováno v:
Earth System Dynamics, Vol 12, Pp 401-418 (2021)
Earth System Dynamics
Earth System Dynamics
Single model initial-condition large ensembles (SMILEs) are valuable tools that can be used to investigate the climate system. SMILEs allow scientists to quantify and separate the internal variability of the climate system and its response to externa
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::74e4ac40878de6fe5bff0fb3571cbf85
https://doi.org/10.5194/esd-12-401-2021
https://doi.org/10.5194/esd-12-401-2021
Publikováno v:
Earth System Dynamics, Vol 11, Pp 885-901 (2020)
Earth System Dynamics
Earth System Dynamics
Initial-condition large ensembles with ensemble sizes ranging from 30 to 100 members have become a commonly used tool to quantify the forced response and internal variability in various components of the climate system. However, there is no consensus
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::01421bb52d2534931c88e31ea9bfdcad
https://doi.org/10.5194/esd-11-885-2020
https://doi.org/10.5194/esd-11-885-2020