Abstract

Abstract. Within the Innsbruck Box project, a ground-based microwave radiometer (RPG-HATPRO) was operated in the Inn Valley (Austria), in very complex terrain, between September 2012 and May 2013 to obtain temperature and humidity vertical profiles of the full troposphere with a specific focus on the valley boundary layer. In order to assess its performance in a deep alpine valley, the profiles obtained by the radiometer with different retrieval algorithms based on different climatologies are compared to local radiosonde data. A retrieval that is improved with respect to the one provided by the manufacturer, based on better resolved data, shows a significantly smaller root mean square error (RMSE), both for the temperature and humidity profiles. The improvement is particularly substantial at the heights close to the mountaintop level and in the upper troposphere. Lower-level inversions, common in an alpine valley, are resolved to a satisfactory degree. On the other hand, upper-level inversions (above 1200 m) still pose a significant challenge for retrieval. For this purpose, specialized retrieval algorithms were developed by classifying the radiosonde climatologies into specialized categories according to different criteria (seasons, daytime, nighttime) and using additional regressors (e.g., measurements from mountain stations). The training and testing on the radiosonde data for these specialized categories suggests that a classification of profiles that reproduces meaningful physical characteristics can yield improved targeted specialized retrievals. A novel and very promising method of improving the profile retrieval in a mountainous region is adding further information in the retrieval, such as the surface temperature at fixed levels along a topographic slope or from nearby mountaintops.

Highlights

  • Precise knowledge of the temperature and humidity structure of the atmosphere is essential for numerical weather prediction and for the study of small-scale phenomena within the atmospheric boundary layer

  • In order to give a first impression of the performance we present a temperature profile comparison between radiosonde and microwave radiometer profiles using the original RPG-algorithm with both scanning and zenith modes

  • The scanning mode gives a better shape of the temperature profile than the zenith mode

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Summary

Introduction

Precise knowledge of the temperature and humidity structure of the atmosphere is essential for numerical weather prediction and for the study of small-scale phenomena within the atmospheric boundary layer. In complex terrain the boundary layers are still a topic of intense research, and the information about the vertical profiles, such as temperature and humidity, as well as their temporal evolution is valuable (e.g., Rotach and Zardi, 2007). For this latter topic the temporal scales of minutes and spatial scales on the order of few tens to hundreds of meters are required. Divakarla et al (2006) compared temperature profiles from an atmospheric infrared sounder (AIRS) with global radiosonde

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