Add to ORKGTropical cyclones (TCs) are fundamentally diabatic systems. The dominant component of diabatic heating is associated with the phase changes of wate
Diabatic experiments with a multi-level primitive equation model were performed using three latent h...
Subtropical cyclones (STCs) derive a considerable portion of their energy from baroclinic and diabat...
Latent cooling by evaporating or melting hydrometeors has recently been shown to contribute to the p...
Extratropical cyclones develop because of baroclinic instability, but their intensification is often...
The effects of latent heat release on the development of extratropical cyclones are proposed to be o...
The influence of convective heating on movement and vertical coupling of tropical cyclones (TCs) is ...
The role of diabatic heating in the development and maintenance of persistent, upper-tropospheric, l...
Midlatitude cyclones play an important role in midlatitude weather and global climate. While barocli...
Diabatic heating from deep moist convection in the hurricane eyewall produces a towering annular str...
An understanding of the processess that generate the atmospheric diabatic heating rates is basic to ...
Potential vorticity (PV) succinctly describes the evolution of large-scale atmospheric flow because ...
Through the use of physical initialization, which relates to precipitation and precipitable water in...
Diabatic processes significantly affect the development and structure of extratropical cyclones. Pre...
It is well established that the diabatic heating distribution in both space and time represents an i...
Latent heating and cooling rates have a critical role in predicting tropical cyclone formation and i...
Diabatic experiments with a multi-level primitive equation model were performed using three latent h...
Subtropical cyclones (STCs) derive a considerable portion of their energy from baroclinic and diabat...
Latent cooling by evaporating or melting hydrometeors has recently been shown to contribute to the p...
Extratropical cyclones develop because of baroclinic instability, but their intensification is often...
The effects of latent heat release on the development of extratropical cyclones are proposed to be o...
The influence of convective heating on movement and vertical coupling of tropical cyclones (TCs) is ...
The role of diabatic heating in the development and maintenance of persistent, upper-tropospheric, l...
Midlatitude cyclones play an important role in midlatitude weather and global climate. While barocli...
Diabatic heating from deep moist convection in the hurricane eyewall produces a towering annular str...
An understanding of the processess that generate the atmospheric diabatic heating rates is basic to ...
Potential vorticity (PV) succinctly describes the evolution of large-scale atmospheric flow because ...
Through the use of physical initialization, which relates to precipitation and precipitable water in...
Diabatic processes significantly affect the development and structure of extratropical cyclones. Pre...
It is well established that the diabatic heating distribution in both space and time represents an i...
Latent heating and cooling rates have a critical role in predicting tropical cyclone formation and i...
Diabatic experiments with a multi-level primitive equation model were performed using three latent h...
Subtropical cyclones (STCs) derive a considerable portion of their energy from baroclinic and diabat...
Latent cooling by evaporating or melting hydrometeors has recently been shown to contribute to the p...