M.: Modelling the Arctic stable boundary layer and its coupling to the surface, Bound.-Lay

• Main Authors: G. J. Steeneveld, A. A. M. Holtslag
• Other Authors: The Pennsylvania State University CiteSeerX Archives
• Format: Text
• Language: English
• Published: 2006
• Subjects: Decoupling; GABLS; Radiation divergence; Resolution; Stable boundary layer; Surface energy balance; Arctic
• Online Access: http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.519.7148; http://www.met.wau.nl/medewerkers/steeneveld/BOUN2451.pdf

Abstract. The impact of coupling the atmosphere to the surface energy balance is exam-ined for the stable boundary layer, as an extension of the first GABLS (GEWEX Atmo-spheric Boundary-Layer Study) one-dimensional model intercomparison. This coupling is of major importance for the stable boundary-layer structure and its development because cou-pling enables a realistic physical description of the interdependence of the surface tempera-ture and the surface sensible heat flux. In the present case, the incorporation of a surface energy budget results in stronger cooling (surface decoupling), and a more stable and less deep boundary layer. The proper representation of this is a problematic feature in large-scale numerical weather prediction and climate models. To account for the upward heat flux from the ice surface beneath, we solve the diffusion equation for heat in the underlying ice as a first alternative. In that case, we find a clear impact of the vertical resolution in the underlying ice on boundary-layer development: coarse vertical resolution in the ice results in stronger surface cooling than for fine resolution. Therefore, because of this impact on stable boundary-layer development, the discretization in the underlying medium needs spe-cial attention in numerical modelling studies of the nighttime boundary layer. As a second