Calibrated ensemble forecasts of the height of new snow using quantile regression forests and ensemble model output statistics

<p>Height of new snow (HN) forecasts help to prevent critical failures of infrastructures in mountain areas, e.g. transport networks and ski resorts. The French national meteorological service, Météo-France, operates a probabilistic forecasting system based on ensemble meteorological forecasts...

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Main Authors: G. Evin, M. Lafaysse, M. Taillardat, M. Zamo
Format: Article
Language:English
Published: Copernicus Publications 2021-09-01
Series:Nonlinear Processes in Geophysics
Online Access:https://npg.copernicus.org/articles/28/467/2021/npg-28-467-2021.pdf
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spelling doaj-8fe95879f0654e96aa2a1fce52551a0c2021-09-16T11:56:10ZengCopernicus PublicationsNonlinear Processes in Geophysics1023-58091607-79462021-09-012846748010.5194/npg-28-467-2021Calibrated ensemble forecasts of the height of new snow using quantile regression forests and ensemble model output statisticsG. Evin0M. Lafaysse1M. Taillardat2M. Zamo3Univ. Grenoble Alpes, INRAE, UR ETGR, Grenoble, FranceUniv. Grenoble Alpes, Université de Toulouse, Météo-France, CNRS, CNRM, Centre d'Etudes de la Neige, 38000 Grenoble, FranceCNRM, Université de Toulouse, Météo-France, CNRS, Toulouse, FranceCNRM, Université de Toulouse, Météo-France, CNRS, Toulouse, France<p>Height of new snow (HN) forecasts help to prevent critical failures of infrastructures in mountain areas, e.g. transport networks and ski resorts. The French national meteorological service, Météo-France, operates a probabilistic forecasting system based on ensemble meteorological forecasts and a detailed snowpack model to provide ensembles of HN forecasts. These forecasts are, however, biased and underdispersed. As for many weather variables, post-processing methods can be used to alleviate these drawbacks and obtain meaningful 1 to 4 <span class="inline-formula">d</span> HN forecasts. In this paper, we compare the skill of two post-processing methods. The first approach is an ensemble model output statistics (EMOS) method, which can be described as a nonhomogeneous regression with a censored shifted Gamma distribution. The second approach is based on quantile regression forests, using different meteorological and snow predictors. Both approaches are evaluated using a 22 <span class="inline-formula">year</span> reforecast. Thanks to a larger number of predictors, the quantile regression forest is shown to be a powerful alternative to EMOS for the post-processing of HN ensemble forecasts. The gain of performance is large in all situations but is particularly marked when raw forecasts completely miss the snow event. This type of situation happens when the rain–snow transition elevation is overestimated by the raw forecasts (rain instead of snow in the raw forecasts) or when there is no precipitation in the forecast. In that case, quantile regression forests improve the predictions using the other weather predictors (wind, temperature, and specific humidity).</p>https://npg.copernicus.org/articles/28/467/2021/npg-28-467-2021.pdf
collection DOAJ
language English
format Article
sources DOAJ
author G. Evin
M. Lafaysse
M. Taillardat
M. Zamo
spellingShingle G. Evin
M. Lafaysse
M. Taillardat
M. Zamo
Calibrated ensemble forecasts of the height of new snow using quantile regression forests and ensemble model output statistics
Nonlinear Processes in Geophysics
author_facet G. Evin
M. Lafaysse
M. Taillardat
M. Zamo
author_sort G. Evin
title Calibrated ensemble forecasts of the height of new snow using quantile regression forests and ensemble model output statistics
title_short Calibrated ensemble forecasts of the height of new snow using quantile regression forests and ensemble model output statistics
title_full Calibrated ensemble forecasts of the height of new snow using quantile regression forests and ensemble model output statistics
title_fullStr Calibrated ensemble forecasts of the height of new snow using quantile regression forests and ensemble model output statistics
title_full_unstemmed Calibrated ensemble forecasts of the height of new snow using quantile regression forests and ensemble model output statistics
title_sort calibrated ensemble forecasts of the height of new snow using quantile regression forests and ensemble model output statistics
publisher Copernicus Publications
series Nonlinear Processes in Geophysics
issn 1023-5809
1607-7946
publishDate 2021-09-01
description <p>Height of new snow (HN) forecasts help to prevent critical failures of infrastructures in mountain areas, e.g. transport networks and ski resorts. The French national meteorological service, Météo-France, operates a probabilistic forecasting system based on ensemble meteorological forecasts and a detailed snowpack model to provide ensembles of HN forecasts. These forecasts are, however, biased and underdispersed. As for many weather variables, post-processing methods can be used to alleviate these drawbacks and obtain meaningful 1 to 4 <span class="inline-formula">d</span> HN forecasts. In this paper, we compare the skill of two post-processing methods. The first approach is an ensemble model output statistics (EMOS) method, which can be described as a nonhomogeneous regression with a censored shifted Gamma distribution. The second approach is based on quantile regression forests, using different meteorological and snow predictors. Both approaches are evaluated using a 22 <span class="inline-formula">year</span> reforecast. Thanks to a larger number of predictors, the quantile regression forest is shown to be a powerful alternative to EMOS for the post-processing of HN ensemble forecasts. The gain of performance is large in all situations but is particularly marked when raw forecasts completely miss the snow event. This type of situation happens when the rain–snow transition elevation is overestimated by the raw forecasts (rain instead of snow in the raw forecasts) or when there is no precipitation in the forecast. In that case, quantile regression forests improve the predictions using the other weather predictors (wind, temperature, and specific humidity).</p>
url https://npg.copernicus.org/articles/28/467/2021/npg-28-467-2021.pdf
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