Zobrazeno 1 - 9
of 9
pro vyhledávání: '"Sophie Abramian"'
Publikováno v:
Journal of Advances in Modeling Earth Systems, Vol 15, Iss 10, Pp n/a-n/a (2023)
Abstract Squall lines are substantially influenced by the interaction of low‐level shear with cold pools associated with convective downdrafts. Beyond an optimal shear amplitude, squall lines tend to orient themselves at an angle with respect to th
Externí odkaz:
https://doaj.org/article/e129fdfff4fd4f86bc0cc8511cad6b39
Autor:
Camille Risi, Caroline Muller, Françoise Vimeux, Peter Blossey, Grégoire Védeau, Clarisse Dufaux, Sophie Abramian
Publikováno v:
Journal of Advances in Modeling Earth Systems, Vol 15, Iss 4, Pp n/a-n/a (2023)
Abstract Water isotopes are tracers of convective processes and are often used as proxies for past precipitation. These applications require a better understanding of the impact of convective processes on the isotopic composition of water vapor and p
Externí odkaz:
https://doaj.org/article/cf422a9d24784f2cbf8579da2c2ab5cf
Autor:
Camille Risi, Caroline Muller, Françoise Vimeux, Peter Blossey, Grégoire Védeau, Clarisse Dufaux, Sophie Abramian
Publikováno v:
Journal of Advances in Modeling Earth Systems
Journal of Advances in Modeling Earth Systems, 2023, 15 (4), pp.e2022MS003331. ⟨10.1029/2022MS003331⟩
Journal of Advances in Modeling Earth Systems, 2023, 15 (4), pp.e2022MS003331. ⟨10.1029/2022MS003331⟩
International audience; Water isotopes are tracers of convective processes and are often used as proxies for past precipitation. These applications require a better understanding of the impact of convective processes on the isotopic composition of wa
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::1c43c1e53a33e60dd7aecc52ec3a722f
https://hal.science/hal-04080289/file/article_SAMiso_cyclone_revised_submit.pdf
https://hal.science/hal-04080289/file/article_SAMiso_cyclone_revised_submit.pdf
Autor:
Caroline Muller, Sophie Abramian
Publikováno v:
Physics Today. 76:28
Through a combination of idealized simulations and real-world data, researchers are uncovering how internal feedbacks and large-scale motions influence cloud dynamics.
Publikováno v:
Journal of Elasticity. 142:1-33
We propose an effective geometrical approach to recover the normal form of a given Elasticity tensor. We produce a rotation which brings an Elasticity tensor onto its normal form, given its components in any orthonormal frame, and this for any tensor
Squall lines are the consequence of the interaction of low-level shear with cold pools associated with convective downdrafts, and beyond a critical shear, squall lines tend to orient themselves. It has been shown that this orientation has the effect
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7363420e67513029cd2f328fe4564082
https://doi.org/10.5194/egusphere-egu22-9649
https://doi.org/10.5194/egusphere-egu22-9649
Autor:
Camille Risi, Françoise Vimeux, Clarisse Dufaux, Grégoire Védeau, Caroline Muller, Sophie Abramian, Peter N. Blossey
One way to test our understanding of the impact of convective processes on the isotopic composition of water vapor and precipitation is to analyze the isotopic mesoscale variations during...
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::21614089ba116b5205095ce62307a797
https://doi.org/10.1002/essoar.10507830.1
https://doi.org/10.1002/essoar.10507830.1
Publikováno v:
Geophysical Research Letters
Squall lines are known to be the consequence of the interaction of low-level shear with cold pools associated with convective downdrafts. Also, as the magnitude of the shear increases beyond a critical shear, squall lines tend to orient themselves. T
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::4ea6ff6f4ad23de865683b562a4d8009
https://doi.org/10.1002/essoar.10507697.1
https://doi.org/10.1002/essoar.10507697.1
Investigating tropical squall lines with a cloud resolving modelUsing a cloud resolving model, we attempt to clarify the physical processes responsible for the organization of deep clouds into squall lines in the tropics. To do so, we impose a vertic
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d6f470fbef589779a2579bdb3d7f5310
https://doi.org/10.5194/egusphere-egu21-4434
https://doi.org/10.5194/egusphere-egu21-4434