Zobrazeno 1 - 10
of 24
pro vyhledávání: '"Gábor Drótos"'
Publikováno v:
Frontiers in Earth Science, Vol 12 (2024)
We address the hypothetical question of whether an increasing total solar irradiance (TSI) trend, without anthropogenic contributions, could be sufficient to explain the ongoing global warming. To this end, the intermediate-complexity climate model P
Externí odkaz:
https://doaj.org/article/653fad3644384cc88129336b9241aceb
Publikováno v:
New Journal of Physics, Vol 26, Iss 6, p 063012 (2024)
Self-testing is a promising approach to certifying quantum states or measurements. Originally, it relied solely on the outcome statistics of the measurements involved in a device-independent (DI) setup. Extra physical assumptions about the system mak
Externí odkaz:
https://doaj.org/article/88a679e541a44f5881deb2f6269341c6
Publikováno v:
Frontiers in Earth Science, Vol 8 (2021)
We study the forced response of the teleconnection between the El Niño–Southern Oscillation (ENSO) and the Indian summer monsoon (IM) in the Max Planck Institute Grand Ensemble, a set of Earth system ensemble simulations under historical and Repre
Externí odkaz:
https://doaj.org/article/0ce46a420b154974b3bb904200c8c933
Publikováno v:
Journal of Climate
Digital.CSIC. Repositorio Institucional del CSIC
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Digital.CSIC. Repositorio Institucional del CSIC
instname
We study the teleconnection between El Niño–Southern Oscillation (ENSO) and the Indian summer monsoon (IM) in large ensemble simulations, the Max Planck Institute Earth System Model (MPI-ESM), and the Community Earth System Model (CESM1). We chara
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::7bd8314ec52b3cc905e9f25dbcd65ee9
https://doi.org/10.1175/jcli-d-19-0341.1
https://doi.org/10.1175/jcli-d-19-0341.1
Publikováno v:
Digital.CSIC. Repositorio Institucional del CSIC
instname
instname
We consider transport in a fluid flow of arbitrary complexity but with a dominant flow direction. One of the situations in which this occurs is when describing by an effective flow the dynamics of sufficiently small particles immersed in a turbulent
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::d0a7ade8c88bb825923b2030c1a994ec
http://arxiv.org/abs/2108.11191
http://arxiv.org/abs/2108.11191
Publikováno v:
Digital.CSIC. Repositorio Institucional del CSIC
instname
Digital.CSIC: Repositorio Institucional del CSIC
Consejo Superior de Investigaciones Científicas (CSIC)
instname
Digital.CSIC: Repositorio Institucional del CSIC
Consejo Superior de Investigaciones Científicas (CSIC)
To characterize local finite-time properties associated with transient chaos in open dynamical systems, we introduce an escape rate and fractal dimensions suitable for this purpose in a coarse-grained description. We numerically illustrate that these
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::a6217dc6156a16876061f5835b9e2d95
http://hdl.handle.net/10261/240430
http://hdl.handle.net/10261/240430
Different teleconnection index time series are obtained even within a single member of a large ensemble simulation if different base periods are chosen. This also has an effect on the apparent strength of teleconnections. In this study, the reasons b
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e1eb1ed92f56059ae19f9a4a71034b1e
https://doi.org/10.5194/egusphere-egu2020-2894
https://doi.org/10.5194/egusphere-egu2020-2894
We study the teleconnection between the El Niño–Southern Oscillation (ENSO) and the Indian summer monsoon (IM) in large ensemble simulations, the Max Planck Institute Earth System Model (MPI-ESM) and the Community Earth System Model (CESM1). We ch
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::fa3abe140a66e7a7bf4d0028e4b82220
https://doi.org/10.5194/egusphere-egu2020-12061
https://doi.org/10.5194/egusphere-egu2020-12061
Publikováno v:
Digital.CSIC. Repositorio Institucional del CSIC
instname
instname
In an incompressible flow, fluid density remains invariant along fluid element trajectories. This implies that the spatial distribution of non-interacting noninertial particles in such flows cannot develop density inhomogeneities beyond those that ar
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::38634cf93ac795b18ca4f4514c07da22
http://hdl.handle.net/10261/189704
http://hdl.handle.net/10261/189704
Publikováno v:
Digital.CSIC. Repositorio Institucional del CSIC
instname
instname
Data generated in this study are available from the URL https://doi.org/10.20350/digitalCSIC/8630
Sedimentation of particles in the ocean leads to inhomogeneous horizontal distributions at depth, even if the release process is homogeneous. We st
Sedimentation of particles in the ocean leads to inhomogeneous horizontal distributions at depth, even if the release process is homogeneous. We st
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::ce810d8bc33b1f80440f6364bf8e8fc5
http://hdl.handle.net/10261/189482
http://hdl.handle.net/10261/189482