000755101 000__ 04718cam\a2200505Ii\4500 000755101 001__ 755101 000755101 005__ 20230306141831.0 000755101 006__ m\\\\\o\\d\\\\\\\\ 000755101 007__ cr\cn\nnnunnun 000755101 008__ 160505s2016\\\\sz\a\\\\ob\\\\000\0\eng\d 000755101 019__ $$a948632369$$a950463765 000755101 020__ $$a9783319335759$$q(electronic book) 000755101 020__ $$a3319335758$$q(electronic book) 000755101 020__ $$z9783319335742 000755101 020__ $$z331933574X 000755101 0247_ $$a10.1007/978-3-319-33575-9$$2doi 000755101 035__ $$aSP(OCoLC)ocn948747122 000755101 035__ $$aSP(OCoLC)948747122$$z(OCoLC)948632369$$z(OCoLC)950463765 000755101 040__ $$aGW5XE$$beng$$erda$$epn$$cGW5XE$$dAZU$$dIDEBK$$dYDXCP$$dOCLCF$$dEBLCP 000755101 049__ $$aISEA 000755101 050_4 $$aGB451.2 000755101 08204 $$a551.45/7$$223 000755101 1001_ $$aBarman, Nilay Kanti,$$eauthor. 000755101 24510 $$aCoastal morphodynamics$$h[electronic resource] :$$bintegrated spatial modeling on the Deltaic Balasore Coast, India /$$cNilay Kanti Barman, Soumendu Chatterjee, Ashis Kumar Paul. 000755101 264_1 $$aSwitzerland :$$bSpringer,$$c2016. 000755101 300__ $$a1 online resource (xix, 110 pages) :$$bcolor illustrations. 000755101 336__ $$atext$$btxt$$2rdacontent 000755101 337__ $$acomputer$$bc$$2rdamedia 000755101 338__ $$aonline resource$$bcr$$2rdacarrier 000755101 4901_ $$aSpringerBriefs in geography,$$x2211-4165 000755101 504__ $$aIncludes bibliographical references. 000755101 5050_ $$aIntroduction to the Study -- Context and Background of the Subarnarekha Delta Plain -- Materials and Methods: A framework for the Coastal Morphodynamics -- Shoreline Dynamics in Subarnarekha Delta Plain -- Beach morphodynamics in Subarnarekha Delta Plain -- Conclusion, Findings and Recommendations. 000755101 506__ $$aAccess limited to authorized users. 000755101 520__ $$aThis book discusses the perceptions and sketches, geological background, materials and coastal processes of the East Coast of India. It also suggests strategies for effectively managing natural coastal processes in these areas. India has a coastline of about 7,516 km with a variety of coastal extensions, which developed at different time scales, producing permanent variations in the morphologies of the coastal areas through hydrodynamic, fluvial, aeolian and terrestrial processes. The book focuses on the Balasore coast, an area drained by three main rivers (the Subarnarekha, the Dugdeugi and the Burahbolong), which impacts the coastal morphodynamic processes of the area and accounts for their multifaceted nature. Large drops or increases in the sediment supply within a short time span or over prolonged periods cause shoreline shifting. Eight satellite images from 1975, 1980, 1990, 1995, 2000, 2005, 2010 and 2013 were used to measure the shoreline dynamics, and a reference line was established using first order polynomial model with base data with 0.5 pixel root mean square error (RMSE) accuracy. The end point rate (EPR) model was adopted for estimating the future position of the shoreline. In order to assess the beach morphodynamics, the coastal modeling system (SMC) was used, which incorporates with a series of appliances and numerical models structured consistent with the space and time scale of the different dynamics affecting the littoral and beach morphology based on diverse thematic and reference documents. This study employed short-term analysis using the MOPLA module of the SMC system, which consists of three attached modules: the wave transformation module (Oluca), the depth-averaged currents module (Copla) and the sediment transport and morphological evolution module (Eros). The shoreline dynamics findings show that the magnitude of erosion is higher in the northern part of the coastline in the left bank area of the Subarnarekha river estuary and in the estuarine part of the Dugdugi and Burahbalang rivers. The southern part of the shoreline near Rasalpur and Joydevkasba is relatively stable, and the study suggests that the current shoreline shift trend will continue in the future. The SMC model indicates that the wave height, significant wave height, current velocity and the potential transport of sediment at the Kirtaniya study point are high, while at Choumukh they are low and at the Rasalpur study point they are intermediate. 000755101 588__ $$aOnline resource; title from PDF title page (SpringerLink, viewed May 5, 2016). 000755101 650_0 $$aCoasts. 000755101 650_0 $$aEnvironmental geomorphology. 000755101 7001_ $$aChatterjee, Soumendu,$$eauthor. 000755101 7001_ $$aPaul, Ashis Kr.,$$eauthor. 000755101 77608 $$iPrint version:$$z9783319335742$$z331933574X$$w(OCoLC)945949345 000755101 830_0 $$aSpringerBriefs in geography. 000755101 852__ $$bebk 000755101 85640 $$3SpringerLink$$uhttps://univsouthin.idm.oclc.org/login?url=http://link.springer.com/10.1007/978-3-319-33575-9$$zOnline Access$$91397441.1 000755101 909CO $$ooai:library.usi.edu:755101$$pGLOBAL_SET 000755101 980__ $$aEBOOK 000755101 980__ $$aBIB 000755101 982__ $$aEbook 000755101 983__ $$aOnline 000755101 994__ $$a92$$bISE