Abstract

This paper addresses the forecasts of latent heat fluxes from five different formulations of the planetary boundary layer (PBL). Different formulations are deployed within the Florida State University global spectral model. Hundreds of short range forecast experiments are carried out using daily data sets for summer 2002 with each model. The primary goal of this study is to compare the performance of the diverse family of PBL algorithms for the latent heat fluxes within the PBL. Benchmark fluxes are calculated from the vertical integrals of Yanai’s formulation of the apparent moisture sink and a precipitation using Physical Initialization. This provides indirectly observed estimates of the vertical fluxes of latent heat in the PBL. This comparison reveals that no single scheme shows a global spread of improvement over other models for forecasts of latent heat fluxes in the PBL. Among these diverse models the turbulent kinetic energy based closure provides somewhat better results. The construction of a multimodel superensemble provides a synthesis of these different PBL formulations and shows improved forecasts of the surface fluxes.Asingle unified model utilizing weighted PBL algorithms where all the five schemes are retained within a single model shows some promise for improving a single model.

Highlights

  • The modelling of the planetary boundary layer (PBL) fluxes for heat, moisture and momentum carry many uncertainties

  • The present paper explores the ensemble spreads that arise from the use of five different PBL formulations

  • The purpose of not selecting the surface layer for model flux inter comparison is that all models shared surface similarity flux in the surface layer and are not based on the different PBL theories

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Summary

Introduction

The modelling of the planetary boundary layer (PBL) fluxes for heat, moisture and momentum carry many uncertainties. One can obtain somewhat useful measures of fluxes from the reanalysis data sets by invoking rain rate initialization and performing vertical integrals of the Yanai et al (1973) apparent heat source and moisture sink computations to arrive at some consistent measures of PBL fluxes. These fluxes are consistent in the sense that they have seen the best estimates of observed rain rates and the entire tropospheric analysed data sets for winds and moisture. This alternative measure of observed fluxes is used in our study

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