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         </gmd:citation>            <gmd:abstract>                <gco:CharacterString>La cartografia rappresenta la vulnerabilità della costa in occasione di eventi di mareggiata caratterizzati da tempi di ritorno di una anno (T1) , 10 anni (T10) e 100 anni (T100).Sono disponibili due tipologie di rappresentazione: Quella puntuale che evidenzia l'impatto stimato lungo profili ortogonali a riva e spaziati circa 500m, e quella lineare nella quale si è effettuata una interpolazione per tratti di costa omogenei ai quali è stato attribuito un grado di vulnerabilità secondo la scala a semafori (Alto, Medio, Basso). La cartografia della vulnerabilità alle mareggiate è stata prodotta nell'ambito dei progetti Europei Cadsealand (2004-2006) e Micore (Morphological Impact and COastal Risks induced by Extreme storm events ) grazie alla collaborazione con il Dipartimento di Scienze della Terra  dell'Università di Ferrara che ha sviluppato una procedura di analisi innovativa e specifica per i litorali dell'Emilia-Romagna.Vedi pubblicazioni: Ciavola P. et al.,2008; Atti 12° Conferenza Nazionale ASITA -  Armaroli et al. 2007, Ambiente e Territorio n. 127 - Armaroli et al. 2009 - Journal of Coastal Research Sp.Issue 56; Perini et al. 2009; in: Il Sistema Informativo Mare-Costa dell'Emilia-Romagna). Armaroli, C., Ciavola, P., Perini, L., Calabrese, L., Lorito, S., Valentini, A., Masina, M., 2012. Critical storm thresholds for significant morphological changes and damage along the Emilia-Romagna coastline, Italy. Geomorphology, 143-144, pp. 34-51. Armaroli, C., Ciavola, P., Masina, M., Perini, L., 2009. Run-up computation behind emerged breakwaters for marine storm risk assessment. Journal of Coastal Research, SI 56, pp. 1612- 1616 Armaroli, C., Perini, L., 2012. A simplified methodology for the estimation of wave runup on armored rubble slopes for vulnerability assessment. 7th Euregeo 2012 Conference, Giugno 2012, Bologna, vol. I, pp. 355-356.</gco:CharacterString>            </gmd:abstract>            <gmd:purpose>                <gco:CharacterString>- Identificazione delle aree potenzialmente a rischio per eventi di tempesta marina.- Elaborazione di una cartografia a scala regionale della vulnerabilità da erosione e/o inondazione e/o danneggiamento strutture antropiche presenti sulla spiaggia o nell'immediato retro-spiaggia. 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          <gmd:level>                        <gmd:MD_ScopeCode codeList="https://standards.iso.org/iso/19139/resources/gmxCodelists.xml#MD_ScopeCode" codeListValue="dataset">Dataset</gmd:MD_ScopeCode>                    </gmd:level>                </gmd:DQ_Scope>            </gmd:scope>            <gmd:report>                <gmd:DQ_DomainConsistency>                    <gmd:result>                        <gmd:DQ_ConformanceResult>                            <gmd:specification>                                <gmd:CI_Citation>                                    <gmd:title>                                        <gco:CharacterString>REGOLAMENTO (UE) N. 1089/2010 DELLA COMMISSIONE del 23 novembre 2010 recante attuazione della direttiva 2007/2/CE del Parlamento europeo e del Consiglio per quanto riguarda l'interoperabilità dei set di dati territoriali e dei servizi di dati territoriali</gco:CharacterString>                                    </gmd:title>                                    <gmd:date>                                        <gmd:CI_Date>                                            <gmd:date>                                                <gco:Date>2010-12-08</gco:Date>                                            </gmd:date>                                            <gmd:dateType>                                                <gmd:CI_DateTypeCode codeList="https://standards.iso.org/iso/19139/resources/gmxCodelists.xml#CI_DateTypeCode" codeListValue="publication">Pubblicazione</gmd:CI_DateTypeCode>                                            </gmd:dateType>                                        </gmd:CI_Date>                                    </gmd:date>                                </gmd:CI_Citation>                            </gmd:specification>                            <gmd:explanation>                                <gco:CharacterString>Fare riferimento alle specifiche indicate</gco:CharacterString>                            </gmd:explanation>                            <gmd:pass xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance"><gco:Boolean>false</gco:Boolean></gmd:pass>                        </gmd:DQ_ConformanceResult>                    </gmd:result>                </gmd:DQ_DomainConsistency>            </gmd:report>            <gmd:report>                <gmd:DQ_AbsoluteExternalPositionalAccuracy>                    <gmd:result>                        <gmd:DQ_QuantitativeResult>                            <gmd:valueUnit>                                <gml:BaseUnit gml:id="m">                                    <gml:identifier codeSpace="http://www.bipm.org/en/si/base_units">m</gml:identifier>                                    <gml:unitsSystem xlink:href="http://www.bipm.org/en/si"/>                                </gml:BaseUnit>                            </gmd:valueUnit>                            <gmd:value>                                <gco:Record xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:type="gco:Real_PropertyType">                                    <gco:Real>1.0</gco:Real>                                </gco:Record>                            </gmd:value>                        </gmd:DQ_QuantitativeResult>                    </gmd:result>                </gmd:DQ_AbsoluteExternalPositionalAccuracy>            </gmd:report>            <gmd:lineage>                <gmd:LI_Lineage>                    <gmd:statement>                        <gco:CharacterString>La cartografia è realizzata tramite approccio di tipo statistico-modellistico, analizzando gli effetti prodotti da mareggiate con tempi di ritorno di 1anno, e simulando le condizioni peggiori: concomitanza di sovralzo atmosferico, alta marea sizigiale e run-up (risalita della lama d'acqua). Per la metodologia di dettaglio, si rimanda agli articoli menzionati in Descrizione.Valutazione degli effetti eseguita confrontando le quote topografiche massime (da DTM Lidar) con quota di risalita del mare per ciascuna sezione. Nel caso delle dune si è fatto un calcolo aggiuntivo, tenendo conto del volume di sabbia che le compone e che può assorbire l'effetto della mareggiata.Possibili impatti aree naturali: intersezione del profilo di spiaggia, inondazione del retro-spiaggia, scavalcamento/erosione duna.Possibili impatti aree antropizzate: danneggiamento delle strutture, intersezione spiaggia/fronte dunale/antropizzato.</gco:CharacterString>                    </gmd:statement>                </gmd:LI_Lineage>            </gmd:lineage>        </gmd:DQ_DataQuality>    </gmd:dataQualityInfo>    <gmd:metadataMaintenance>        <gmd:MD_MaintenanceInformation>            <gmd:maintenanceAndUpdateFrequency>                <gmd:MD_MaintenanceFrequencyCode codeList="https://standards.iso.org/iso/19139/resources/gmxCodelists.xml#MD_MaintenanceFrequencyCode" codeListValue="unknown">Sconosciuta</gmd:MD_MaintenanceFrequencyCode>            </gmd:maintenanceAndUpdateFrequency>        </gmd:MD_MaintenanceInformation>    </gmd:metadataMaintenance>
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