Abstract

Abstract. An evaluation of the upper tropospheric humidity from the European Centre of Medium-Range Weather Forecasts (ECMWF) Integrated Forecast System (IFS) is presented. We first make an analysis of the spinup behaviour of ice supersaturation in weather forecasts. It shows that a spinup period of at least 12 h is necessary before using forecast humidity data from the upper troposphere. We compare the forecasted upper tropospheric humidity with coincident relative humidity fields retrieved from the Atmospheric InfraRed Sounder (AIRS) and with cloud vertical profiles from the Cloud-Aerosol Lidar and Infrared Pathfinder Satellite Observation (CALIPSO). The analysis is made over one year, from October 2006 to September 2007, and we discuss how relative humidity and cloud features appear both in the IFS and in the observations. The comparison with AIRS is made difficult because of the vertical resolution of the sounder and the impossibility to retrieve humidity for high cloudiness. Clear sky relative humidities show a rather good correlation whereas cloudy situations reflect more the effect of a dry bias for AIRS increasing with the relative humidity. The comparison with CALIPSO shows that the IFS predicts high relative humidity where CALIPSO finds high clouds, which supports the good quality of the ECMWF upper tropospheric cloud forecast. In a last part, we investigate the presence of ice supersaturation within low vertical resolution pressure layers by comparing the IFS outputs for high-resolution and low-resolution humidity profiles and by simulating the interpolation of humidity over radiosonde data. A new correction method is proposed and tested with these data.

Highlights

  • Ice supersaturation in the upper troposphere is an explicit feature in the Integrated Forecast System (IFS) of the European Centre of Medium-Range Weather Forecasts (ECMWF), operational since 13 September 2006 (IFS cycle 31r1)

  • Relative humidity of IFS and Atmospheric InfraRed Sounder (AIRS) was compared in different pressure layers, separately for clear and cloudy situations distinguished by AIRS

  • Modes were detected: 1) a dry mode in which IFS predicts RHi from ECMWF (RHiE)

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Summary

Introduction

Ice supersaturation in the upper troposphere is an explicit feature in the Integrated Forecast System (IFS) of the European Centre of Medium-Range Weather Forecasts (ECMWF), operational since 13 September 2006 (IFS cycle 31r1). This new feature, introduced by Tompkins et al (2007), has produced some changes in the statistics of upper tropospheric humidity and cloud fraction in the IFS. To explore the effect of the interpolation further and to assess the occurrence of ice supersaturation using data with low vertical resolution, we compare relative humidity using ECMWF forecasts of high and low resolution, and we simulate the averaging effect by using radiosonde data from Lindenberg, Germany

ECMWF forecasts
A-Train data and collocations with ECMWF
Radiosonde data
Supersaturation spinup
Evaluation of upper tropospheric humidity
Comparison with AIRS relative humidity fields
Comparison with CALIPSO cloud vertical profiles
Influence of vertical resolution on occurrence of ice supersaturation
Conclusions
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