A software package (OZO, Omega-Zwack-Okossi) was developed to diagnose the processes that affect vertical motions and geopotential height tendencies in weather systems simulated by the Weather Research and Forecasting (WRF) model. First, this software solves a generalised omega equation to calculate the vertical motions associated with different physical forcings: vorticity advection, thermal advection, friction, diabatic heating, and an imbalance term between vorticity and temperature tendencies. After this, the corresponding height tendencies are calculated with the Zwack-Okossi tendency equation. The resulting height tendency components thus contain both the direct effect from the forcing itself and the indirect effects (related to the v...
An equatorial beta-plane model of the middle atmosphere is used to analytically examine the effects ...
International audienceThe Weather Research and Forecasting (WRF) Model has been designed to be an ef...
Aimed at reducing deficiencies in representing the Madden-Julian oscillation (MJO) in general circul...
A software package (OZO, Omega-Zwack-Okossi) was developed to diagnose the processes that affect ver...
A software package (OZO, Omega–Zwack–Okossi) was developed to diagnose the processes that affect ver...
A statistical analysis of the physical causes of atmospheric vertical motions is conducted using a g...
Treballs Finals de Grau de Física, Facultat de Física, Universitat de Barcelona, Curs: 2022, Tutora:...
The role of the ageostrophic vorticity tendencies in the Zwack-Okossi vorticity tendency equation ha...
The diagnostic tool DIONYSOS is presented in this paper. DIONYSOS is a diagnostic package specifical...
Two fundamental perspectives on the dynamics of midlatitude weather systems are provided by potentia...
In this study, the development of a warm-core and cold-core extratropical cyclone over North Atlanti...
The role of the ageostrophic vorticity tendencies in the Zwack–Okossi vorticity tendency equation ha...
The effects of wave and zonal mean ozone heating on the evolution of the quasi-biennial oscillation ...
Hurricane Ophelia was a category 3 hurricane which underwent extratropical transition and made landf...
Two Madden‐Julian Oscillation (MJO) events, observed during October and November 2011 in the equator...
An equatorial beta-plane model of the middle atmosphere is used to analytically examine the effects ...
International audienceThe Weather Research and Forecasting (WRF) Model has been designed to be an ef...
Aimed at reducing deficiencies in representing the Madden-Julian oscillation (MJO) in general circul...
A software package (OZO, Omega-Zwack-Okossi) was developed to diagnose the processes that affect ver...
A software package (OZO, Omega–Zwack–Okossi) was developed to diagnose the processes that affect ver...
A statistical analysis of the physical causes of atmospheric vertical motions is conducted using a g...
Treballs Finals de Grau de Física, Facultat de Física, Universitat de Barcelona, Curs: 2022, Tutora:...
The role of the ageostrophic vorticity tendencies in the Zwack-Okossi vorticity tendency equation ha...
The diagnostic tool DIONYSOS is presented in this paper. DIONYSOS is a diagnostic package specifical...
Two fundamental perspectives on the dynamics of midlatitude weather systems are provided by potentia...
In this study, the development of a warm-core and cold-core extratropical cyclone over North Atlanti...
The role of the ageostrophic vorticity tendencies in the Zwack–Okossi vorticity tendency equation ha...
The effects of wave and zonal mean ozone heating on the evolution of the quasi-biennial oscillation ...
Hurricane Ophelia was a category 3 hurricane which underwent extratropical transition and made landf...
Two Madden‐Julian Oscillation (MJO) events, observed during October and November 2011 in the equator...
An equatorial beta-plane model of the middle atmosphere is used to analytically examine the effects ...
International audienceThe Weather Research and Forecasting (WRF) Model has been designed to be an ef...
Aimed at reducing deficiencies in representing the Madden-Julian oscillation (MJO) in general circul...