Numerical Simulations of the Impacts of Land-Cover Change on a Southern Sea Breeze in South-West Western Australia

• Published in: Boundary-layer meteorology Vol. 135; no. 3; pp. 485 - 503
• Main Authors: Kala, J, Lyons, T. J, Abbs, D. J, Nair, U. S
• Format: Journal Article
• Language: English
• Published: Dordrecht Dordrecht : Springer Netherlands 01-06-2010; Springer Netherlands; Springer; Springer Nature B.V
• Subjects: Analysis; Atmospheric boundary layer; Atmospheric models; Atmospheric Protection/Air Quality Control/Air Pollution; Atmospheric Sciences; Computer simulation; Convection, turbulence, diffusion. Boundary layer structure and dynamics; Dynamics; Earth and Environmental Science; Earth Sciences; Earth, ocean, space; Exact sciences and technology; External geophysics; Grasslands; Land cover; Land-cover change; Mathematical models; Meteorology; Moisture content; Regional Atmospheric Modelling System; Roughness; Scaling analysis; Sea breeze; Sea breezes; Soil moisture; soil water; Soils; Vegetation; Western Australia; Wind; Australia; Western Australia; South Australia; ISW, Australia, Western Australia; Land-cover change; Regional Atmospheric Modelling System; Scaling analysis; Sea breeze; Soil moisture; models; Roughness length; soil moisture; sensitivity analysis; Australasia; Regional scope; vegetation; digital simulation; bare soils; grasslands; Surface wind; high resolution
• ISSN: 0006-8314; 1573-1472
• DOI: 10.1007/s10546-010-9486-z

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 changes in soil moisture on the dynamics of the sea breeze. It is found that land-cover change alone, i.e., a change from wooded grasslands to bare soil, with no change in soil moisture initialisation, does not significantly alter the overall structure of the sea breeze but results in higher surface winds due to the reduced vegetation roughness length, which leads to enhanced surface moisture advection inland. On the other hand, land-cover change in conjunction with increased soil moisture results in a considerably weaker, shallower, and less penetrative sea breeze, and delays its onset and duration. A sea-breeze scaling analysis highlights the impact of increasing soil moisture on reducing the sea-breeze volume flux scale.