Abstract

Abstract. This study presents a methodology to analyse orographic enhancement of precipitation using sequences of radar images and a digital elevation model. Image processing techniques are applied to extract precipitation cells from radar imagery. DEM is used to derive the topographic indices potentially relevant to orographic precipitation enhancement at different spatial scales, e.g. terrain convexity and slope exposure to mesoscale flows. Two recently developed machine learning algorithms are then used to analyse the relationship between the repeatability of precipitation patterns and the underlying topography. Spectral clustering is first used to characterize stratification of the precipitation cells according to different mesoscale flows and exposure to the crest of the Alps. At a second step, support vector machine classifiers are applied to build a computational model which discriminates persistent precipitation cells from all the others (not showing a relationship to topography) in the space of topographic conditioning factors. Upwind slopes and hill tops were found to be the topographic features leading to precipitation repeatability and persistence. Maps of orographic enhancement susceptibility can be computed for a given flow, topography and forecasted smooth precipitation fields and used to improve nowcasting models or correct windward and leeward biases in numerical weather prediction models.

Highlights

  • The orographic precipitation enhancement is a complex atmospheric phenomenon which is the subject of many numerical (Rotunno and Houze, 2007) and observational studies (Gray and Seed, 2000; Panziera and Germann, 2010)

  • This study introduces an efficient computational alternative to analyse and to model orographic enhancement of precipitation from a sequence of radar images and a digital elevation model (DEM)

  • This study introduced a generic data-driven methodology to study the orographic enhancement of precipitation

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Summary

Introduction

The orographic precipitation enhancement is a complex atmospheric phenomenon which is the subject of many numerical (Rotunno and Houze, 2007) and observational studies (Gray and Seed, 2000; Panziera and Germann, 2010). Expert-based statistical approaches are developed to avoid these flaws Such alternatives are successfully applied for thunderstorm nowcasting (Wilson and Gallant, 2000; Williams et al, 2008), and are appearing in the context of orographic precipitation nowcasting (Panziera et al, 2010). Evidences of high counts of cells repeatability reveal the topographic conditions and locations where the phenomenon is accentuated. This formulation allows characterizing precipitation enhancement using data-driven classification models. The system can be applied to simulate the localized enhancement under given flow and large scale precipitation patterns derived from nowcasting or NWP models. 4. The computational model of orographic enhancement is explained in Sect.

Methodology
Data preparation
Exploration of precipitation cells
Computational model Forecasted precipitation and flow fields
Computational model of orographic precipitation enhancement
Findings
Conclusions
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