作者: 不真 時(shí)間: 2025-3-21 20:14
Book 2016 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作者: Tonometry 時(shí)間: 2025-3-22 04:22
Introduction to the Study,ugdugi and Burahbolong). The presence of these fluvial impacts may causes the coastal morphodynamic processes of these areas are very multifaceted in nature. Mobilization of sediment endow with the time-dependent amalgamation apparatus by which this morphologic modification occurs. Morphological cha作者: ALOFT 時(shí)間: 2025-3-22 07:56
Context and Background of the Subarnarekha Delta Plain, during the periods of erosional winnowing. The present studied coast extends from Rasalpur to Udaipur. The study area covers an area of about 142,519.76 hector Stretching between 21° 20′ 25?N. 86° 52′ 45?E and 22° 07′ 55?N 87° 31′ 37″E. This area is geomorphologically productive, reach in habitat d作者: 焦慮 時(shí)間: 2025-3-22 08:54
Materials and Methods: A Framework for the Coastal Morphodynamics,horeline and its future positions based on empirical observations at 67 transects along the Balasore coast. The rate of shoreline movement calculated from the fixed base line to shoreline position of 1975, 1980, 1990, 1995, 2000, 2005 and 2010 were applied and based on this, the estimated shoreline 作者: predict 時(shí)間: 2025-3-22 16:18
Shoreline Dynamics in Subarnarekha Delta Plain,each sample points (Transects) is observed. The positional error varies from ?4.82 to 212.41?m. It has been found that model prediction error is higher in the mouth of river Subarnarekha. The overall error for the entire predicted shoreline was found to be 41.88?m by .. In addition, further it was t作者: predict 時(shí)間: 2025-3-22 18:49 作者: prostatitis 時(shí)間: 2025-3-22 23:24 作者: allergen 時(shí)間: 2025-3-23 04:50
Book 2016 2000, 2005, 2010 and 2013 were used to measure the shoreline dynamics, and a reference linewas 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 sh作者: 合法 時(shí)間: 2025-3-23 08:40 作者: Certainty 時(shí)間: 2025-3-23 11:24 作者: ARK 時(shí)間: 2025-3-23 17:30
https://doi.org/10.1007/978-3-319-67346-2horeline and its future positions based on empirical observations at 67 transects along the Balasore coast. The rate of shoreline movement calculated from the fixed base line to shoreline position of 1975, 1980, 1990, 1995, 2000, 2005 and 2010 were applied and based on this, the estimated shoreline 作者: harbinger 時(shí)間: 2025-3-23 20:58 作者: HEDGE 時(shí)間: 2025-3-24 00:23 作者: 概觀 時(shí)間: 2025-3-24 03:47
https://doi.org/10.1007/978-3-319-58871-1vulnerability and dynamics. The intensity and severity of beach morphological alteration are experienced to have increased may be due to recent climate and environment changes. Moreover, river Subarnarekha carries large volume of discharge experiences with gigantic quantity of sediments. This flow o作者: 政府 時(shí)間: 2025-3-24 06:46
2211-4165 newas 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 sh978-3-319-33574-2978-3-319-33575-9Series ISSN 2211-4165 Series E-ISSN 2211-4173 作者: 我不死扛 時(shí)間: 2025-3-24 11:03
https://doi.org/10.1007/978-3-319-33575-9Coastal Geomorphology; Shoreline Morphodynamics; Beach Morphodynamics; Coastal Environment Management; S作者: 安定 時(shí)間: 2025-3-24 17:54
https://doi.org/10.1007/978-3-319-67346-2each rocks, etc. are incorporated with 7516?km lengthy Indian coast. These coastal morphological units have been developed at different time scale. Coastal setting is undergoing uninterrupted alterations through terrestrial and marine systems. Hence the study regarding coastal environments are gaini作者: anthesis 時(shí)間: 2025-3-24 20:42
https://doi.org/10.1007/978-3-319-67346-2plain” of Subarnarekha delta where cuspate arrangement of chenier ridges is significant feature. The entire chenier delta plain was formed by combination of marine and fluvial agencies. The chenier plain of this vicinity has prograded sea ward since the end of the Holocene transgression with the pro作者: Capitulate 時(shí)間: 2025-3-25 01:38 作者: 巫婆 時(shí)間: 2025-3-25 06:53
https://doi.org/10.1007/978-3-319-67346-2 seafloor morphologies and sequences of change dynamics involving the motion of?sediment transports. Hydrodynamic processes include those of waves, tides and wind-induced currents. The present study involves an endeavour to appraise the transect wise investigative model for predicting the future sho作者: 大猩猩 時(shí)間: 2025-3-25 10:38
https://doi.org/10.1007/978-981-15-0932-2t takes a finite time to move, there is a lag in the morphological response to hydrodynamic forcing. Sediment can therefore be considered to be a time-dependent coupling mechanism. Since the boundary conditions of hydrodynamic forcing change regularly this may mean that the beach never attains equil作者: obstinate 時(shí)間: 2025-3-25 15:31 作者: Fester 時(shí)間: 2025-3-25 17:00 作者: 大暴雨 時(shí)間: 2025-3-25 22:54 作者: scrutiny 時(shí)間: 2025-3-26 00:58
SpringerBriefs in Geographyhttp://image.papertrans.cn/c/image/228744.jpg作者: RENIN 時(shí)間: 2025-3-26 06:48 作者: 搖擺 時(shí)間: 2025-3-26 11:08
Context and Background of the Subarnarekha Delta Plain,plain” of Subarnarekha delta where cuspate arrangement of chenier ridges is significant feature. The entire chenier delta plain was formed by combination of marine and fluvial agencies. The chenier plain of this vicinity has prograded sea ward since the end of the Holocene transgression with the pro作者: cluster 時(shí)間: 2025-3-26 15:00 作者: 纖細(xì) 時(shí)間: 2025-3-26 19:02 作者: 難理解 時(shí)間: 2025-3-26 22:17
Beach Morphodynamics in Subarnarekha Delta Plain,t takes a finite time to move, there is a lag in the morphological response to hydrodynamic forcing. Sediment can therefore be considered to be a time-dependent coupling mechanism. Since the boundary conditions of hydrodynamic forcing change regularly this may mean that the beach never attains equil作者: NEG 時(shí)間: 2025-3-27 03:16
Conclusion, Findings and Recommendations,e rich swamping and breeding grounds for marine creatures, feeding grounds for birds, recreational grounds for tourists and available resources for the local communities which have a great importance to modification of coastal morphology. The Balasore district in Odisha, India, is to be found on the作者: 昏迷狀態(tài) 時(shí)間: 2025-3-27 07:38
9樓作者: 同謀 時(shí)間: 2025-3-27 12:56
9樓作者: 我說不重要 時(shí)間: 2025-3-27 13:43
9樓作者: BLA 時(shí)間: 2025-3-27 20:18
9樓作者: obscurity 時(shí)間: 2025-3-28 00:44
10樓作者: Heretical 時(shí)間: 2025-3-28 02:58
10樓作者: 雀斑 時(shí)間: 2025-3-28 10:13
10樓作者: 天空 時(shí)間: 2025-3-28 12:32
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