Abstract

AbstractIt is shown that a poor forecast of a midlatitude cyclone developing over the western Atlantic Ocean can be significantly improved by potential vorticity (PV) modifications in the vicinity of the dynamical tropopause in the initial conditions, in order to modify the position of the tropopause. Manually built PV corrections are introduced by using the ARPEGE‐IFS 4D‐Var assimilation system. For that purpose, a PV observation operator, its tangent‐linear and adjoint versions, based on a simplified form of Ertel PV, has been implemented. The impact of the PV pseudo‐observations in an optimal system (i.e. analysed using tuned observation‐error statistics) is positive; the maximum positive improvement of the forecast is obtained over western Europe when the cyclone reaches its maximum amplitude. The forecast is never degraded during the model run, whereas another run forced by the pseudo‐observations is characterized by the development of a forecast error pattern downstream to the main pattern of analysis increment. The conditioning of the minimization problem defined as the sparsity (for the non‐diagonal parts) of the Hessian matrix is weakly affected by the PV observation operator leading to quite good convergence. Copyright © 2006 Royal Meteorological Society.

Full Text
Published version (Free)

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call