منابع مشابه
Transport of Sulfur Oxides within the Los Angeles Sea Breeze/land Breeze Circulation System
The sea breeze/land breeze circulation system in the Los Angeles area results in transport of pollutants seaward at night followed by return of aged material inland the next day. This characteristic wind reversal pattern both increases the retention time available for the oxidation of S02 to for m sulfates and causes individual air parcels to make multiple passes over large coastal emissions so...
متن کاملTRANSPORT OF SULFUR OXIDES lHTHIN THE LOS ANGELES SEA BREEZE/LAND BREEZE CIRCULATION SYSTEM
The sea breeze/land breeze circulation system in the Los Angeles a r ea results in transport of pollutants seaward at nigh t followed by return of aged material inland the next day . This characteristic wind reversal pattern both increases the r etention time available for the oxidation of S02 to form sulfates and causes individual a ir parcels to make mul tiple passes over large coas tal emiss...
متن کاملAerosol-cloud-land surface interactions within tropical sea breeze convection
In this study, the influence of aerosols, surface roughness length, soil moisture, and synergistic interactions among these factors on tropical convective rainfall focused along a sea breeze front are explored within idealized cloud-resolving modeling simulations using the Regional Atmospheric Modeling System (RAMS). The idealized RAMS domain setup is representative of the coastal Cameroon rain...
متن کاملNumerical simulations of the impacts of land-cover change on a southern sea-breeze in south-west Western Australia
A sea-breeze event in south-west Western Australia is simulated using the Regional Atmospheric Modelling System (RAMS) version 6.0. The model is evaluated against high resolution soundings as well as station observations and is shown to reproduce the qualitative features of the sea-breeze well. Sensitivity tests are carried out to investigate the effects of historical land-cover change and chan...
متن کاملA Numerical Modeling Study of the Propagation of Idealized Sea-Breeze Density Currents*
Sea breezes are often modeled as a wave response to transient heating in a stratified environment. They occur, however, as density currents with well-defined fronts, the understanding of which rests primarily on experiments and theory that do not include the stratification within and above the current and the steady heat input at the land surface. These gaps are investigated here via a sequence...
متن کاملذخیره در منابع من
با ذخیره ی این منبع در منابع من، دسترسی به آن را برای استفاده های بعدی آسان تر کنید
ژورنال
عنوان ژورنال: Papers in Meteorology and Geophysics
سال: 1976
ISSN: 0031-126X
DOI: 10.2467/mripapers1950.27.4_99