<?xml version="1.0" encoding="UTF-8"?><?xml-stylesheet type="text/xsl" href="static/style.xsl"?><OAI-PMH xmlns="http://www.openarchives.org/OAI/2.0/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/ http://www.openarchives.org/OAI/2.0/OAI-PMH.xsd"><responseDate>2026-04-14T14:47:33Z</responseDate><request verb="GetRecord" identifier="oai:uvadoc.uva.es:10324/59637" metadataPrefix="dim">https://uvadoc.uva.es/oai/request</request><GetRecord><record><header><identifier>oai:uvadoc.uva.es:10324/59637</identifier><datestamp>2024-12-04T13:09:00Z</datestamp><setSpec>com_10324_1176</setSpec><setSpec>com_10324_931</setSpec><setSpec>com_10324_894</setSpec><setSpec>col_10324_1359</setSpec></header><metadata><dim:dim xmlns:dim="http://www.dspace.org/xmlns/dspace/dim" xmlns:doc="http://www.lyncode.com/xoai" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.dspace.org/xmlns/dspace/dim http://www.dspace.org/schema/dim.xsd">
<dim:field mdschema="dc" element="contributor" qualifier="author" authority="ce8fbe29c631eb82" confidence="600" orcid_id="0000-0003-2457-9793">Calvo Sancho, Carlos</dim:field>
<dim:field mdschema="dc" element="contributor" qualifier="author" authority="750d1ef9-be3d-4ce1-8583-0e81d627a4c8" confidence="600" orcid_id="">Quitián Hernández, Lara</dim:field>
<dim:field mdschema="dc" element="contributor" qualifier="author" authority="33377fb4-8e2f-40e1-ae0c-b8e05a3b1f3c" confidence="600" orcid_id="">González Alemán, Juan Jesús</dim:field>
<dim:field mdschema="dc" element="contributor" qualifier="author" authority="1e6ed1ef-aa4c-4edc-8d9e-31fb60270782" confidence="600" orcid_id="">Bolgiani, Pedro</dim:field>
<dim:field mdschema="dc" element="contributor" qualifier="author" authority="b7e23160-d8b7-4582-9c61-29bbfce67ac5" confidence="600" orcid_id="">Santos Muñoz, Daniel</dim:field>
<dim:field mdschema="dc" element="contributor" qualifier="author" authority="4070af2cd046443e" confidence="600" orcid_id="0000-0002-8500-8276">Martín Pérez, María Luisa</dim:field>
<dim:field mdschema="dc" element="date" qualifier="accessioned">2023-05-18T08:27:45Z</dim:field>
<dim:field mdschema="dc" element="date" qualifier="available">2023-05-18T08:27:45Z</dim:field>
<dim:field mdschema="dc" element="date" qualifier="issued">2023</dim:field>
<dim:field mdschema="dc" element="identifier" qualifier="citation" lang="es">Atmospheric Research, 2023, vol. 291, 106801</dim:field>
<dim:field mdschema="dc" element="identifier" qualifier="issn" lang="es">0169-8095</dim:field>
<dim:field mdschema="dc" element="identifier" qualifier="uri">https://uvadoc.uva.es/handle/10324/59637</dim:field>
<dim:field mdschema="dc" element="identifier" qualifier="doi" lang="es">10.1016/j.atmosres.2023.106801</dim:field>
<dim:field mdschema="dc" element="identifier" qualifier="publicationfirstpage" lang="es">106801</dim:field>
<dim:field mdschema="dc" element="identifier" qualifier="publicationtitle" lang="es">Atmospheric Research</dim:field>
<dim:field mdschema="dc" element="identifier" qualifier="publicationvolume" lang="es">291</dim:field>
<dim:field mdschema="dc" element="description" lang="es">Producción Científica</dim:field>
<dim:field mdschema="dc" element="description" qualifier="abstract" lang="es">Tropical cyclones (TCs) can develop as a result of the tropical transition (TT) process, which occurs when an extratropical cyclone (EC) begins to exhibit tropical characteristics, forming a TC. In this study, four TT processes that lead to a hurricane structure [Delta (2005), Ophelia (2017), Leslie (2018), and Theta (2020)] are evaluated using two high-resolution numerical models (WRF and HARMONIE-AROME). Both tracks and intensities of the cyclones are assessed by comparing the simulated minimum sea level pressure and maximum wind speed to an observational dataset. Moreover, a spatial verification is performed by comparing the MSG-SEVIRI brightness temperature (BT) and accumulated precipitation (IMERG) to the corresponding simulations accomplished by both models. Analyzing the track results, the WRF model, on average, outstands HARMONIE-AROME. However, it is the HARMONIE-AROME model that performs better than WRF when reproducing the intensity of these cyclones. Concerning the BT spatial validation, HARMONIE-AROME slightly outperformed WRF when reproducing the cyclone's structure but failed when simulating the BT amplitude. Besides, both models achieved a nearly perfect cyclone location. In terms of accumulated precipitation results, the HARMONIE-AROME model overestimates the larger structures while underestimating the smaller ones, whereas the WRF model underestimates the bigger structures, being poorly located by both models. Although it is difficult to establish which numerical model performs better, the overall results show an outstanding of the HARMONIE-AROME model over the WRF model when simulating TT processes.</dim:field>
<dim:field mdschema="dc" element="description" qualifier="project" lang="es">IBERCANES (Project PID2019-105306RB-I00/AEI/10.13039/501100011033)</dim:field>
<dim:field mdschema="dc" element="description" qualifier="project" lang="es">Ministerio de Ciencia e Innovación de España - FPI program (PRE2020-092343)</dim:field>
<dim:field mdschema="dc" element="format" qualifier="mimetype" lang="es">application/pdf</dim:field>
<dim:field mdschema="dc" element="language" qualifier="iso" lang="es">eng</dim:field>
<dim:field mdschema="dc" element="publisher" lang="es">Elsevier</dim:field>
<dim:field mdschema="dc" element="rights" qualifier="accessRights" lang="es">info:eu-repo/semantics/openAccess</dim:field>
<dim:field mdschema="dc" element="rights" qualifier="uri" lang="*">http://creativecommons.org/licenses/by-nc-nd/4.0/</dim:field>
<dim:field mdschema="dc" element="rights" qualifier="holder" lang="es">© 2023 The Authors</dim:field>
<dim:field mdschema="dc" element="rights" lang="*">Attribution-NonCommercial-NoDerivatives 4.0 Internacional</dim:field>
<dim:field mdschema="dc" element="subject" lang="es">Matemáticas</dim:field>
<dim:field mdschema="dc" element="subject" lang="es">Artificial intelligence</dim:field>
<dim:field mdschema="dc" element="subject" qualifier="classification" lang="es">Tropical Transitions</dim:field>
<dim:field mdschema="dc" element="subject" qualifier="classification" lang="es">North Atlantic basin</dim:field>
<dim:field mdschema="dc" element="subject" qualifier="classification" lang="es">Object-based verification</dim:field>
<dim:field mdschema="dc" element="subject" qualifier="classification" lang="es">WRF</dim:field>
<dim:field mdschema="dc" element="subject" qualifier="classification" lang="es">Transiciones tropicales</dim:field>
<dim:field mdschema="dc" element="subject" qualifier="classification" lang="es">Cuenca del Atlántico Norte</dim:field>
<dim:field mdschema="dc" element="subject" qualifier="classification" lang="es">Verificación basada en objetos</dim:field>
<dim:field mdschema="dc" element="subject" qualifier="unesco" lang="es">12 Matemáticas</dim:field>
<dim:field mdschema="dc" element="title" lang="es">Assessing the performance of the HARMONIE-AROME and WRF-ARW numerical models in North Atlantic Tropical Transitions</dim:field>
<dim:field mdschema="dc" element="type" lang="es">info:eu-repo/semantics/article</dim:field>
<dim:field mdschema="dc" element="type" qualifier="hasVersion" lang="es">info:eu-repo/semantics/publishedVersion</dim:field>
<dim:field mdschema="dc" element="relation" qualifier="publisherversion" lang="es">https://www.sciencedirect.com/science/article/pii/S0169809523001989?via%3Dihub</dim:field>
<dim:field mdschema="dc" element="peerreviewed" lang="es">SI</dim:field>
</dim:dim></metadata></record></GetRecord></OAI-PMH>