{"title":"Shoreline Change of the Mucuripe Harbour Zones (Fortaleza-Ceará, Northeast of Brazil) 1972 - 2003","authors":"M.O. Bezerra, L. Pinheiro, J.O. Morais","doi":"10.2112/jcr-si50-210.1","DOIUrl":null,"url":null,"abstract":"BEZERRA, M.O., PINHEIRO, L. and MORAIS, J.O. 2007. Shoreline Change of the Mucuripe Harbour Zones (Fortaleza-Ceará, Northeast of Brazil) 1972 2003. Journal of Coastal Research, SI 50 (Proceedings of the 9th International Coastal Symposium), 1163 – 1167. Gold Coast, Australia, ISSN 0749.0208 This study analyses the space-time evolution along the Fortaleza coast over the past 31 years (1972-2003) with a special emphasis on the Mucuripe port area (Fortaleza, Ceará, Brazil) examining changes in the coastal dynamics produced by the building of the city’s port. The construction of the port’s jetty interrupted the natural feeding process of the beaches with sediment moving east to west. Sediment was blocked east of this structure leading to an erosion process to the west. This multi-temporal study is based on the analysis of aerial photographs and images from the Quickbird satellite. The objective is to determine the recent evolution of this coastline through calculation of the variation in retrograding and prograding areas. The variation of the city of Fortaleza's dunebeach interface shoreline, which concerns an extension of approximately 30 km of shoreline, revealed a prograding rate of 0.8284 km/31 years (1972/2003) and a retrograding rate of 0.0701 km/31 years (1972/2003). Analysis of images of Mansa Beach, located in the Mucuripe port basin, showed that in 1972 Mansa Beach had an area of 0.13843 km, in 1998 it increased to 0.15307 km and in 2003 it reached 0.15455 km. The analysis revealed that the changes in the shoreline are more subject to shoreline accretion. The analysed period shows a 92% accretion rate and an 8% erosion rate. The results contribute to the improved management of the Fortaleza coast. ADDITIONAL INDEX WORDS: Changes in the shoreline, Prograding, Multi-temporal study","PeriodicalId":51078,"journal":{"name":"Journal of Coastal Research","volume":"57 2","pages":""},"PeriodicalIF":0.0000,"publicationDate":"2024-03-29","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"6","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Journal of Coastal Research","FirstCategoryId":"89","ListUrlMain":"https://doi.org/10.2112/jcr-si50-210.1","RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q3","JCRName":"Earth and Planetary Sciences","Score":null,"Total":0}
引用次数: 6
Abstract
BEZERRA, M.O., PINHEIRO, L. and MORAIS, J.O. 2007. Shoreline Change of the Mucuripe Harbour Zones (Fortaleza-Ceará, Northeast of Brazil) 1972 2003. Journal of Coastal Research, SI 50 (Proceedings of the 9th International Coastal Symposium), 1163 – 1167. Gold Coast, Australia, ISSN 0749.0208 This study analyses the space-time evolution along the Fortaleza coast over the past 31 years (1972-2003) with a special emphasis on the Mucuripe port area (Fortaleza, Ceará, Brazil) examining changes in the coastal dynamics produced by the building of the city’s port. The construction of the port’s jetty interrupted the natural feeding process of the beaches with sediment moving east to west. Sediment was blocked east of this structure leading to an erosion process to the west. This multi-temporal study is based on the analysis of aerial photographs and images from the Quickbird satellite. The objective is to determine the recent evolution of this coastline through calculation of the variation in retrograding and prograding areas. The variation of the city of Fortaleza's dunebeach interface shoreline, which concerns an extension of approximately 30 km of shoreline, revealed a prograding rate of 0.8284 km/31 years (1972/2003) and a retrograding rate of 0.0701 km/31 years (1972/2003). Analysis of images of Mansa Beach, located in the Mucuripe port basin, showed that in 1972 Mansa Beach had an area of 0.13843 km, in 1998 it increased to 0.15307 km and in 2003 it reached 0.15455 km. The analysis revealed that the changes in the shoreline are more subject to shoreline accretion. The analysed period shows a 92% accretion rate and an 8% erosion rate. The results contribute to the improved management of the Fortaleza coast. ADDITIONAL INDEX WORDS: Changes in the shoreline, Prograding, Multi-temporal study
期刊介绍:
The Journal of Coastal Research (JCR) is one of the leading international journals for coastal studies and processes, and is published bi-monthly by the Coastal Education & Research Foundation [CERF]. By covering the entire field of coastal research, the JCR encompasses all subjects relevant to natural and engineered environments (freshwater, brackish, or marine) and the protection/management of their resources in the vicinity of coastlines of the world. Even though the journal broadly focuses on immediate shoreline zones, the JCR also embraces those coastal environments that either reach some indefinite distance inland or that extend seaward beyond the outer margins of the sublittoral (neritic) zone. The JCR disseminates accurate information to both the public and research specialists around the world on all aspects of coastal issues in an effort to maintain or improve the quality of our planet''s shoreline resources.