A method for assessing the coastline recession due to the sea level rise by assuming stationary wind-wave climate

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Fältnamn	Indikatorer	Metadata
000		03066naa a2200409 4500
001		oai:DiVA.org:su-122343
003		SwePub
008		151029s2015 \| \|\|\|\|\|\|\|\|\|\|\|000 \|\|eng\|
024	7	a https://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-1223432 URI
024	7	a https://doi.org/10.1515/ohs-2015-00352 DOI
040		a (SwePub)su
041		a engb eng
042		9 SwePub
072	7	a ref2 swepub-contenttype
072	7	a art2 swepub-publicationtype
100	1	a Deng, Junjie4 aut
245	1 0	a A method for assessing the coastline recession due to the sea level rise by assuming stationary wind-wave climate
264		c 2015-09-30
264	1	b Uniwersytet Gdanski,c 2015
338		a print2 rdacarrier
520		a The method introduced in this study for future projection of coastline changes hits the vital need of communicating the potential climate change impact on the coast in the 21th century. A quantitative method called the Dynamic Equilibrium Shore Model (DESM) has been developed to hindcast historical sediment mass budgets and to reconstruct a paleo Digital Elevation Model (DEM). The forward mode of the DESM model relies on paleo-scenarios reconstructed by the DESM model assuming stationary wind-wave climate. A linear relationship between the sea level, coastline changes and sediment budget is formulated and proven by the least square regression method. In addition to its forward prediction of coastline changes, this linear relationship can also estimate the sediment budget by using the information on the coastline and relative sea level changes. Wind climate change is examined based on regional climate model data. Our projections for the end of the 21st century suggest that the wind and wave climates in the southern Baltic Sea may not change compared to present conditions and that the investigated coastline along the Pomeranian Bay may retreat from 10 to 100 m depending on the location and on the sea level rise which was assumed to be in the range of 0.12 to 0.24 m.
650	7	a NATURVETENSKAPx Biologi0 (SwePub)1062 hsv//swe
650	7	a NATURAL SCIENCESx Biological Sciences0 (SwePub)1062 hsv//eng
650	7	a NATURVETENSKAPx Geovetenskap och miljövetenskap0 (SwePub)1052 hsv//swe
650	7	a NATURAL SCIENCESx Earth and Related Environmental Sciences0 (SwePub)1052 hsv//eng
653		a modelling
653		a coastline changes
653		a dynamic equilibrium
653		a sediment budget estimation
653		a climate change
700	1	a Harff, Jan4 aut
700	1	a Schimanke, Semjon4 aut
700	1	a Meier, H. E. Markusu Stockholms universitet,Meteorologiska institutionen (MISU),Swedish Meteorological and Hydrological Institute, Sweden4 aut
710	2	a Stockholms universitetb Meteorologiska institutionen (MISU)4 org
773	0	t Oceanological and Hydrobiological Studiesd : Uniwersytet Gdanskig 44:3, s. 362-380q 44:3<362-380x 1730-413Xx 1897-3191
856	4 8	u https://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-122343
856	4 8	u https://doi.org/10.1515/ohs-2015-0035

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Av författaren/redakt...: Deng, Junjie; Harff, Jan; Schimanke, Semjo ...; Meier, H. E. Mar ...

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