Plumes in rotating convection. Part 1. Ensemble statistics and dynamical balances
Atmospheric and oceanic convection often occurs over areas occupied by many localized
circulation elements known as plumes. The convective transports therefore may depend not …
circulation elements known as plumes. The convective transports therefore may depend not …
Plumes in rotating convection. Part 1. Ensemble statistics and dynamical balances
K Julien, S Legg, J McWilliams… - Journal of Fluid …, 1999 - ui.adsabs.harvard.edu
Atmospheric and oceanic convection often occurs over areas occupied by many localized
circulation elements known as plumes. The convective transports therefore may depend not …
circulation elements known as plumes. The convective transports therefore may depend not …
Plumes in rotating convection. Part 1. Ensemble statistics and dynamical balances
K JULIEN, S LEGG - J. Fluid Mech, 1999 - cambridge.org
The combination of efficient lateral mixing and slow vertical movement by the plumes
accounts for the unstable mean temperature gradient that occurs in rotating Rayleigh …
accounts for the unstable mean temperature gradient that occurs in rotating Rayleigh …
[引用][C] Plumes in rotating convection. Part 1. Ensemble statistics and dynamical balances
K JULIEN, S LEGG, J MCWILLIAMS… - Journal of Fluid …, 1999 - pascal-francis.inist.fr
Plumes in rotating convection. Part 1. Ensemble statistics and dynamical balances CNRS Inist
Pascal-Francis CNRS Pascal and Francis Bibliographic Databases Simple search Advanced …
Pascal-Francis CNRS Pascal and Francis Bibliographic Databases Simple search Advanced …
[PDF][PDF] Plumes in rotating convection. Part 1. Ensemble statistics and dynamical balances
K JULIEN, S LEGG - J. Fluid Mech, 1999 - colorado.edu
The combination of efficient lateral mixing and slow vertical movement by the plumes
accounts for the unstable mean temperature gradient that occurs in rotating Rayleigh …
accounts for the unstable mean temperature gradient that occurs in rotating Rayleigh …
Plumes in rotating convection. Part 1. Ensemble statistics and dynamical balances
K JULIEN, S LEGG, J McWILLIAMS, J WERNE… - 1999 - arch.neicon.ru
Atmospheric and oceanic convection often occurs over areas occupied by many localized
circulation elements known as plumes. The convective transports therefore may depend not …
circulation elements known as plumes. The convective transports therefore may depend not …
[PDF][PDF] Plumes in rotating convection. Part 1. Ensemble statistics and dynamical balances
K JULIEN, S LEGG - J. Fluid Mech, 1999 - Citeseer
The combination of efficient lateral mixing and slow vertical movement by the plumes
accounts for the unstable mean temperature gradient that occurs in rotating Rayleigh …
accounts for the unstable mean temperature gradient that occurs in rotating Rayleigh …
[PDF][PDF] Plumes in rotating convection. Part 1. Ensemble statistics and dynamical balances
K JULIEN, S LEGG - J. Fluid Mech, 1999 - academia.edu
The combination of efficient lateral mixing and slow vertical movement by the plumes
accounts for the unstable mean temperature gradient that occurs in rotating Rayleigh …
accounts for the unstable mean temperature gradient that occurs in rotating Rayleigh …
[PDF][PDF] Plumes in rotating convection. Part 1. Ensemble statistics and dynamical balances
K JULIEN, S LEGG - J. Fluid Mech, 1999 - academia.edu
The combination of efficient lateral mixing and slow vertical movement by the plumes
accounts for the unstable mean temperature gradient that occurs in rotating Rayleigh …
accounts for the unstable mean temperature gradient that occurs in rotating Rayleigh …