Abstract

In regions of complex topography, local flows are difficult to forecast on a routine basis, especially in stable conditions, due to the coarse resolution of operational models. The Cadarache valley (southeastern France) features this sort of complex topography. The Weather Research and Forecasting (WRF) model is run daily to forecast the weather in this region with a horizontal resolution of 3 km. Such a resolution cannot resolve all topography details of the small Cadarache valley, and therefore its local wind patterns. Other variables, however, that are less dependent on the subgrid topography, are satisfactorily forecasted, and used as inputs to an artificial neural network (ANN) designed to reproduce wind observations inside the valley from WRF forecasts. A variable selection procedure identified 5 key input variables that best drive the ANN. With respect to the WRF output, the ANN significantly improves forecasted low-level winds, both for speed and direction. This study demonstrates the potential for the ANN technique to be used as a correcting tool to forecast weather conditions at the local scale when numerical modeling is performed at a resolution too coarse to take into account the effect of local topography.

Highlights

  • Published: 20 January 2021Low-level winds must be well described when studying atmospheric dispersion.Over complex terrain, winds can be deviated or channeled by the topography

  • While decoupling occurs frequently in observations, especially under stable conditions leading to Cadarache down-valley (CDV) winds at 2 m, it is underpredicted in Weather Research and Forecasting (WRF)

  • This is striking for CDV 2 m winds associated with 110 m winds coming from the West

Read more

Summary

Introduction

Low-level winds must be well described when studying atmospheric dispersion. Winds can be deviated or channeled by the topography. Spatial thermal differences over sloping terrain can generate slope winds. Described four mechanisms of low and high level wind interaction in a valley, which are a combination of thermal and topographical effects, showing the complexity of flow over complex terrain. Flow in a steep alpine valley was documented during the Passy project [9], and the KASCADE (Katabatic winds and Stability over CAdarache for Dispersion of Effluents) experiment [10] was conducted in winter 2013 in the Cadarache region (in south east France) which features complex topography

Objectives
Methods
Results
Conclusion
Full Text
Published version (Free)

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call