SPRAY DROPLET MODELING .1. LAGRANGIAN MODEL SIMULATION OF THE TURBULENT TRANSPORT OF EVAPORATING DROPLETS

Citation
Jb. Edson et Cw. Fairall, SPRAY DROPLET MODELING .1. LAGRANGIAN MODEL SIMULATION OF THE TURBULENT TRANSPORT OF EVAPORATING DROPLETS, J GEO RES-O, 99(C12), 1994, pp. 25295-25311
Citations number
63
Categorie Soggetti
Oceanografhy
Journal title
JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS
ISSN journal
21699275 → ACNP
Volume
99
Issue
C12
Year of publication
1994
Pages
25295 - 25311
Database
ISI
SICI code
2169-9275(1994)99:C12<25295:SDM.LM>2.0.ZU;2-Q
Abstract
The investigation of aerosol production and transport over the world's oceans is of importance in studies concerning cloud physics, air poll ution, atmospheric optics, and air-sea interaction in general. However , the contribution of sea spray droplets to the transfer of moisture a nd latent heat from the sea to the atmosphere is not well known. In li ght of this, the Humidity Exchange Over the Sea Experiment in Simulati on Tunnel and Couche Limite Unidimensionelle Stationnaire d'Embrums (o ne dimensional stationary droplet boundary layer) programs were design ed to investigate the generation, turbulent transport, and evaporation of droplets ejected by bursting bubbles within the air-sea simulation tunnel at Institut de Mecanique Statistique de la Turbulence (IMST), Luminy, France. This first part describes the Lagrangian model develop ed as part of these programs to simulate the turbulent transport of ev aporating droplets. The model relies on a form of the Langevin equatio n, which has been modified to account for the effects of gravity and t he inertia of the droplets. The comparisons between the model and meas urements show good agreement, particularly within the surface layer at IMST. Part 2 will describe the coupling of the model with an Eulerian k-epsilon model, which allows for improved simulation of the velocity and scaler fields, as well as a means for interaction between the dro plets and these fields. The model is designed to provide a better unde rstanding of the influence of these droplets on the near surface energ y budget.