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Forecasting radiation fog at climatologically contrasting sites: evaluation of statistical methods and WRF

dc.contributor.authorRomán Cascón, Carlos
dc.contributor.authorSteeneveld, Gert Jan
dc.contributor.authorYagüe Anguis, Carlos
dc.contributor.authorSastre Marugán, Mariano
dc.contributor.authorArrillaga, Jon Ander
dc.contributor.authorMaqueda Burgos, Gregorio
dc.date.accessioned2024-01-16T10:03:18Z
dc.date.available2024-01-16T10:03:18Z
dc.date.issued2016
dc.description.abstractA six-year climatology of radiation fog has been compiled at two sites: the Research Centre for the Lower Atmosphere (CIBA, Spain) and the Cabauw Experimental Site for Atmospheric Research (CESAR, The Netherlands). These sites are contrasted in terms of geographical situation, climate zone, altitude, humidity and soil water availability. Therefore, several climatological differences in fog abundance, onset, dissipation and duration have been quantified between the two sites. The more humid site (CESAR) is characterised by relatively short radiation fog events distributed throughout the year. However, radiation fog at the drier site (CIBA) is more persistent and appears during late autumn/winter months. In general, its formation requires more time after sunset (approximate to 2 h more), since further cooling is required to reach saturation. The forecast of these fog events has been evaluated through two different approaches. First, we extend the statistical method presented by Menut et al. (2014) (M14). This method uses statistics to define threshold values on key variables for fog formation (pre-fog) and verifies its predictability using observations and numerical model output. We present some of the most appropriate threshold values for the forecasting of pre-fog periods at both sites, which differ from those presented in M14 and depend on the optimisation of the hit rate or the false-alarm rate. Additionally, we also extend M14 by suggesting other variables as potential predictors for fog formation (friction velocity and visibility tendency). Finally, we focus on fog simulation by the Weather Research and Forecasting (WRF) model in terms of liquid water content. The WRF model was able to simulate radiation fog when configured with sophisticated physical options and high resolution. However it failed in simulating the onset, dissipation and the vertical extent of fog (which was overestimated). The model results were extremely sensitive to the spin-up time.eng
dc.description.departmentDepto. de Física de la Tierra y Astrofísica
dc.description.facultyFac. de Ciencias Físicas
dc.description.refereedTRUE
dc.description.sponsorshipMinisterio de Economía, Comercio y Empresa (España)
dc.description.sponsorshipNetherlands Organization for Scientific Research
dc.description.statuspub
dc.identifier.citationRomán‐Cascón, C., et al. «Forecasting Radiation Fog at Climatologically Contrasting Sites: Evaluation of Statistical Methods and WRF». Quarterly Journal of the Royal Meteorological Society, vol. 142, n.o 695, enero de 2016, pp. 1048-63. https://doi.org/10.1002/qj.2708.
dc.identifier.doi10.1002/qj.2708
dc.identifier.essn1477-870X
dc.identifier.issn0035-9009
dc.identifier.officialurlhttps://doi.org/10.1002/qj.2708
dc.identifier.urihttps://hdl.handle.net/20.500.14352/93290
dc.issue.number695
dc.journal.titleQuarterly Journal of the Royal Meteorological Society
dc.language.isoeng
dc.page.final1063
dc.page.initial1048
dc.publisherWiley
dc.relation.projectIDinfo:eu-repo/grantAgreement/CGL2012-37416-C04-02
dc.relation.projectIDinfo:eu-repo/grantAgreement/BES-2013 064585
dc.relation.projectIDinfo:eu-repo/grantAgreement/863.10.010
dc.rights.accessRightsrestricted access
dc.subject.cdu551.51
dc.subject.keywordRadiation fog
dc.subject.keywordClimatology
dc.subject.keywordWRF
dc.subject.keywordCESAR
dc.subject.keywordCIBA
dc.subject.keywordStatistics
dc.subject.keywordForecast
dc.subject.keywordNowcasting
dc.subject.ucmFísica atmosférica
dc.subject.unesco2509 Meteorología
dc.titleForecasting radiation fog at climatologically contrasting sites: evaluation of statistical methods and WRFen
dc.typejournal article
dc.type.hasVersionVoR
dc.volume.number142
dspace.entity.typePublication
relation.isAuthorOfPublication9a4cf43f-bd9c-4b5b-9cb2-0c257e7473de
relation.isAuthorOfPublicationcf5cf9ad-8e0e-4c40-966d-58da28c01b49
relation.isAuthorOfPublication873030aa-a296-46f9-883a-7a52a9cd2909
relation.isAuthorOfPublication.latestForDiscovery9a4cf43f-bd9c-4b5b-9cb2-0c257e7473de

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