Moist Baroclinic Instability and Macroturbulence of the Midlatitude Atmosphere

Water and its change of phase greatly enrich the dynamics of the midlatitude atmosphere and challenge us to extend our theories of baroclinic instability and macroturbulence beyond dry adiabatic dynamics. Two specific phenomena in which latent heating plays a key role and that are poorly understood...

Deskribapen osoa

Xehetasun bibliografikoak
Egile nagusia: Kohl, Matthieu
Beste egile batzuk: O'Gorman, Paul A.
Formatua: Thesis
Argitaratua: Massachusetts Institute of Technology 2023
Sarrera elektronikoa:https://hdl.handle.net/1721.1/150203