Revisiting the latent heat nudging scheme for the rainfall assimilation of a simulated convective storm

• Published in: Meteorology and atmospheric physics Vol. 98; no. 3-4; pp. 195 - 215
• Main Authors: Leuenberger, D., Rossa, A.
• Format: Journal Article
• Language: English
• Published: Wien Springer 01.12.2007; New York, NY Springer Nature B.V
• Subjects: Earth, ocean, space; Environmental degradation; Exact sciences and technology; External geophysics; Latent heat; Meteorology; Physics; Prediction models; Rain; Rainfall; Simulation; Storms; Water in the atmosphere (humidity, clouds, evaporation, precipitation); Weather analysis and prediction; Weather forecasting; Wind; rainfall; Weather forecast; atmospheric precipitation; Mesoscale convective system; sensitivity analysis; Rainfall rate; parametrization; Radar observation; Observation data; Numerical forecast; Supercell; uncertainties; storms; Data assimilation; latent heat; high resolution
• ISSN: 0177-7971; 1436-5065
• DOI: 10.1007/s00703-007-0260-9

Next-generation, operational, high-resolution numerical weather prediction models require economical assimilation schemes for radar data. In the present study we evaluate and characterise the latent heat nudging (LHN) rainfall assimilation scheme within a meso-gamma scale NWP model in the framework of identical twin simulations of an idealised supercell storm. Consideration is given to the model's dynamical response to the forcing as well as to the sensitivity of the LHN scheme to uncertainty in the observations and the environment. The results indicate that the LHN scheme is well able to capture the dynamical structure and the right rainfall amount of the storm in a perfect environment. This holds true even in degraded environments but a number of important issues arise. In particular, changes in the low-level humidity field are found to affect mainly the precipitation amplitude during the assimilation with a fast adaptation of the storm to the system dynamics determined by the environment during the free forecast. A constant bias in the environmental wind field, on the other hand, has the potential to render a successful assimilation with the LHN scheme difficult, as the velocity of the forcing is not consistent with the system propagation speed determined by the wind. If the rainfall forcing moves too fast, the system propagation is supported and the assimilated storm and forecasts initialised therefrom develop properly. A too slow forcing, on the other hand, can decelerate the system and eventually disturb the system dynamics by decoupling the low-level moisture inflow from the main updrafts during the assimilation. This distortion is sustained in the free forecast. It has further been found that a sufficient temporal resolution of the rainfall input is crucial for the successful assimilation of a fast moving, coherent convective storm and that the LHN scheme, when applied to a convective storm, appears to necessitate a careful tuning. [PUBLICATION ABSTRACT]