Zobrazeno 1 - 10
of 18
pro vyhledávání: '"Costanza Rodda"'
Publikováno v:
Scientific Reports, Vol 13, Iss 1, Pp 1-13 (2023)
Abstract Using two laboratory-scale conceptual fluid dynamic models of the mid-latitude atmospheric circulation we investigate the statistical properties of pointwise temperature signals obtained in long experiment runs. We explore how the average
Externí odkaz:
https://doaj.org/article/f6ec7cd4279c47cab7787c1cd400586e
Autor:
Miklós Vincze, Tamás Bozóki, Mátyás Herein, Ion Dan Borcia, Uwe Harlander, Attila Horicsányi, Anita Nyerges, Costanza Rodda, András Pál, József Pálfy
Publikováno v:
Scientific Reports, Vol 11, Iss 1, Pp 1-11 (2021)
Abstract Pronounced global cooling around the Eocene–Oligocene transition (EOT) was a pivotal event in Earth’s climate history, controversially associated with the opening of the Drake Passage. Using a physical laboratory model we revisit the flu
Externí odkaz:
https://doaj.org/article/d9dac58e531c45aa98610cc6c8b262e4
Autor:
Uwe Harlander, Andrei Sukhanovskii, Stéphane Abide, Ion Dan Borcia, Elena Popova, Costanza Rodda, Andrei Vasiliev, Miklos Vincze
Publikováno v:
Atmosphere, Vol 14, Iss 5, p 836 (2023)
The large-scale flows of the oceans and the atmosphere are driven by a non-uniform surface heating over latitude, and rotation. For many years scientists try to understand these flows by doing laboratory experiments. In the present paper we discuss t
Externí odkaz:
https://doaj.org/article/7b6b49a40b4b42549094d620c8bf715f
Publikováno v:
Fluids, Vol 7, Iss 8, p 274 (2022)
Atmospheric westerly jet streams are driven by temperature differences between low and high latitudes and the rotation of the Earth. Meandering jet streams and propagating Rossby waves are responsible for the variable weather in the mid-latitudes. Mo
Externí odkaz:
https://doaj.org/article/dc97f74508794351b4a9794e7e966d9e
Publikováno v:
eISSN
We report on a set of laboratory experiments to investigate the effect of polar warming on the mid-latitude jet stream. Our results show that a progressive decrease of the meridional temperature difference slows down the eastward propagation of the j
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::78a4f71d622633e24d1f297c749f5049
https://doi.org/10.5194/egusphere-2022-148
https://doi.org/10.5194/egusphere-2022-148
Laboratory experiments are used to study the effect of Arctic warming on the amplitude and zonal phase speed of mid-latitude jet meanders. Our results show that a progressive decrease of the meridional temperature difference 1) slows down the eastwar
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::adc9870cb3c37aacdb11177d27304baa
https://doi.org/10.5194/egusphere-egu22-5050
https://doi.org/10.5194/egusphere-egu22-5050
Autor:
Costanza Rodda, Clément Savaro, Géraldine Davis, Jason Reneuve, Pierre Augier, Joël Sommeria, Thomas Valran, Samuel Viboud, Nicolas Mordant
Recent developments of the weak turbulence theory applied to internal waves exhibit a power-law solution of the kinetic energy equation close to the oceanic Garrett \& Munk spectrum, confirming weakly nonlinear wave interactions as a likely explanati
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::090561aef31872a72a4c814463b31274
Autor:
Uwe Harlander, András Pál, Mátyás Herein, Attila Horicsányi, Miklos Vincze, Tamás Bozóki, Ion Dan Borcia, Anita Nyerges, Costanza Rodda, József Pálfy
Publikováno v:
Scientific Reports
Scientific Reports, Vol 11, Iss 1, Pp 1-11 (2021)
Scientific Reports, Vol 11, Iss 1, Pp 1-11 (2021)
Pronounced global cooling around the Eocene–Oligocene transition (EOT) was a pivotal event in Earth’s climate history, controversially associated with the opening of the Drake Passage. Using a physical laboratory model we revisit the fluid dynami
Autor:
Pierre Augier, Clément Savaro, Miguel Calpe Linares, Thomas Valran, Samuel Viboud, Antoine Campagne, Joël Sommeria, Nicolas Mordant, Costanza Rodda
Atmospheric and oceanic energy spectra are characterized by global scaling laws, suggesting a common mechanism driving the energy route to dissipation. Although several possible theories have been proposed, it is not clear yet what the phenomena cont
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::18921048ff05a3f23f2dbb79a4eac88e
https://doi.org/10.5194/egusphere-egu21-10904
https://doi.org/10.5194/egusphere-egu21-10904