Convective storms and atmospheric vertical structure in Uranus and Neptune.

Neptune Uranus atmospheric dynamics icy planets

Journal

Philosophical transactions. Series A, Mathematical, physical, and engineering sciences
ISSN: 1471-2962
Titre abrégé: Philos Trans A Math Phys Eng Sci
Pays: England
ID NLM: 101133385

Informations de publication

Date de publication:
25 Dec 2020
Historique:
entrez: 9 11 2020
pubmed: 10 11 2020
medline: 10 11 2020
Statut: ppublish

Résumé

The ice giants Uranus and Neptune have hydrogen-based atmospheres with several constituents that condense in their cold upper atmospheres. A small number of bright cloud systems observed in both planets are good candidates for moist convective storms, but their observed properties (size, temporal scales and cycles of activity) differ from moist convective storms in the gas giants. These clouds and storms are possibly due to methane condensation and observations also suggest deeper clouds of hydrogen sulfide (H

Identifiants

pubmed: 33161859
doi: 10.1098/rsta.2019.0476
pmc: PMC7658788
doi:

Types de publication

Journal Article

Langues

eng

Sous-ensembles de citation

IM

Pagination

20190476

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Auteurs

R Hueso (R)

Física Aplicada I, Escuela de Ingeniería de Bilbao, UPV/EHU, 48013 Bilbao, Spain.

T Guillot (T)

Université Côte d'Azur, Laboratoire Lagrange, OCA, CNRS UMR 7293, Nice, France.

A Sánchez-Lavega (A)

Física Aplicada I, Escuela de Ingeniería de Bilbao, UPV/EHU, 48013 Bilbao, Spain.

Classifications MeSH