1956/04/01 by Norman A. Phillips · 4 citations
Environmental Science · Earth and Planetary Sciences · #Climate variability and models #Oceanographic and Atmospheric Processes #Meteorological Phenomena and Simulations
paper · doi:10.1002/qj.49708235202
openalex publication_date 1956/04/01 · openalex created_date 2025/10/10 · openalex updated_date 2026/07/23
Abstract A long‐period numerical forecast is made with a two‐level quasi‐geostrophic model, starting with an atmosphere in relative rest. Both friction and non‐adiabatic effects are included in the equations, the latter as a linear function of latitude. Principal empirical elements in the experiment are the intensity of the heating, the value of the vertical stability, and the type of frictional dissipation. The flow patterns which develop are quite realistic, including a jet and zonal surface westerlies in middle latitudes, and the growth of a large disturbance. The associated energy transformations are investigated, and demonstrate the important role of the disturbance in the development of the zonal currents. The meridional circulation is also studied, together with its contribution to the zonal momentum budgets of the lower and upper halves of the atmosphere. Truncation errors eventually put an end to the forecast by producing a large fictitious increase in energy.