標(biāo)題: Titlebook: Crisis on the Coast and Hinterland; Assessing India’s Ea Ashis Kumar Paul,Anurupa Paul Book 2023 The Editor(s) (if applicable) and The Auth [打印本頁(yè)] 作者: obdurate 時(shí)間: 2025-3-21 18:13
書(shū)目名稱Crisis on the Coast and Hinterland影響因子(影響力)
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書(shū)目名稱Crisis on the Coast and Hinterland讀者反饋
書(shū)目名稱Crisis on the Coast and Hinterland讀者反饋學(xué)科排名
作者: LATHE 時(shí)間: 2025-3-21 22:32 作者: 高爾夫 時(shí)間: 2025-3-22 03:49
Geomorphological Diversity and Sea Level Rise Vulnerabilities on India’s East Coasteplain of the eastern ghats with discontinuous ridges parallel to the shoreline. The entire coast is again separated into many physiographic units from north to south by the number of east flowing rivers into the Bay of Bengal, cutting across the bands of coastal zones with geomorphic diversity. The作者: 極肥胖 時(shí)間: 2025-3-22 05:39
Nearshore Morphological Alteration through Sediment Dynamics: An Integrated Software Based (Coastal ch morphodynamics. The Coastal Modelling System (SMC) integrates a series of appliances and numerical models with spatio-temporal scales of different dynamics upsetting in littoral and beach morphology based on various thematic and reference information. The present study has been contented with the作者: 小歌劇 時(shí)間: 2025-3-22 11:45 作者: 圓桶 時(shí)間: 2025-3-22 16:34
Estimation of Seasonal Sediment Budget of Chandrabhaga Beach-Dune System, Bay of Bengal, Indiaa laser total station. In step two, the raw data is adjusted and pre-processed before the preliminary map production, which constitutes step three. Step four involves the geo-statistical analysis and DEM generation in the GIS environment, and finally, step five highlights the procedure for sediment 作者: 圓桶 時(shí)間: 2025-3-22 17:56 作者: 不給啤 時(shí)間: 2025-3-22 23:16
Beach Stage and Dune Stage Modelling Approach in the Geomorphological Evolution of Beach Dune Landscicial features under consideration and to showcase the relationship between fluvio-tidal and marine processes. For this purpose, we have used the Shuttle Radar Topography Mission (SRTM) Digital Elevation Model (DEM) and various field-based data to generate a DEM for the study area and apply differen作者: 貞潔 時(shí)間: 2025-3-23 04:39 作者: freight 時(shí)間: 2025-3-23 08:12 作者: 承認(rèn) 時(shí)間: 2025-3-23 12:59
The Degradation of Coastal Habitats in Andhra Pradesh and Tamil Nadu: An Environmental Approachmainly on the review of general characteristics, processes, and biota of the coastal habitat stressors that shape the regional coastal settings of Andhra Pradesh and how far they will be vulnerable to cyclones and sea level rise processes in the decades to come. The coastal drainage systems, wetland作者: kindred 時(shí)間: 2025-3-23 17:27
Mangrove Sensitivity to the Ephemeral Rise of Sea Waters in the Western Sundarbanin the interior of the islands, overflowing or occasionally breaching the extensive dykes along the banks of the creeks or the coastal ridges along the beach. This inundation and the subsequent drop in the water level trap saline water in the inland areas, which leads to the evaporative deposition o作者: 輕率的你 時(shí)間: 2025-3-23 18:59 作者: Armory 時(shí)間: 2025-3-23 23:37
Issues and Management Strategies of the Riparian Corridor of the Dulung River Basin, Indiamiddle, and lower, and each sector represents the differential nature of the terrain, hydrology, vegetation, agricultural practices, and human intervention. The present work focuses on the systemic study of the riparian area along with the uniqueness of the corridor based on morphometric parameters 作者: 擔(dān)心 時(shí)間: 2025-3-24 03:44
The Importance of Shoreline Beaches for Coastal Tourism Potential and Their Diversities on the Odishsociety, and economy of the coastal districts. The study highlights diminishing beach environs, conflicts between tourists and locals, and the evolution of natural beaches into “city by the sea (crowdy)”, economic impacts, and sustainable management of beach resources. The present study is conducted作者: 堅(jiān)毅 時(shí)間: 2025-3-24 09:14 作者: Anticoagulant 時(shí)間: 2025-3-24 12:57
An Assessment of the Changing Environmental Factors of Estuarine Tidal Flats in Sagar Islandis to observe the dynamic morphological features of the tidal flats, to demarcate the continuous shifting of HTL and LTL, and to time scale the changes from sea level to soil property. Erosion and accretion are the continuous processes of the islands of the Hugli estuary by strong natural hydrologic作者: callous 時(shí)間: 2025-3-24 18:37
Temporal and Spatial Changes in the Hugli Estuarine Environment: A Review of Nayachara Islandface, bank margin tidal flats, and the tidal creek banks. The temporal changes of area as well as the changes in length and width of islands and bank margin tidal flats will be estimated by temporal satellite images. The areal change of mangroves and salt marshes, as well as their habitats and diver作者: 讓空氣進(jìn)入 時(shí)間: 2025-3-24 20:45 作者: 云狀 時(shí)間: 2025-3-25 02:58
Book 2023sment through Environmental Approaches addresses various environmental assessmenttechniques of mangrove sensitivity to the sea level rise process in the Sundarban, land degradation of the hinterland drainage basins, the riparian environment of the coastal drainage basins, agricultural adaptability i作者: ARIA 時(shí)間: 2025-3-25 05:59 作者: 語(yǔ)言學(xué) 時(shí)間: 2025-3-25 08:18
Psychologische Grundlagen der Wahrnehmung,ch morphodynamics. The Coastal Modelling System (SMC) integrates a series of appliances and numerical models with spatio-temporal scales of different dynamics upsetting in littoral and beach morphology based on various thematic and reference information. The present study has been contented with the作者: Cryptic 時(shí)間: 2025-3-25 15:28
Letzte Etappe – die Schatzkartea estuary associated with the strengthening monsoon phases, the dominance of southwestern and northeastern monsoons, and relative sea level positions in the deltaic region. The topographic expressions and width of inter-dune swales illustrate the relative strength of regression phases in the differe作者: Contort 時(shí)間: 2025-3-25 18:23
Zweite Etappe – Standortbetrachtunga laser total station. In step two, the raw data is adjusted and pre-processed before the preliminary map production, which constitutes step three. Step four involves the geo-statistical analysis and DEM generation in the GIS environment, and finally, step five highlights the procedure for sediment 作者: hieroglyphic 時(shí)間: 2025-3-25 22:24 作者: Comprise 時(shí)間: 2025-3-26 02:34 作者: 絕緣 時(shí)間: 2025-3-26 07:29
Zweite Etappe – Standortbetrachtung at present. The southern spit is accreted and the north-eastern spit is eroded. The use of multi-date high resolution Landsat images and Google Earth images of the last 38?years examines the spit dynamics and hydrogeomorphic processes of the lagoon in the present study. It has been observed that th作者: Flu表流動(dòng) 時(shí)間: 2025-3-26 10:59 作者: AMOR 時(shí)間: 2025-3-26 13:25 作者: 不發(fā)音 時(shí)間: 2025-3-26 18:55
,Die Beobachtung: St?dte sind Marken,in the interior of the islands, overflowing or occasionally breaching the extensive dykes along the banks of the creeks or the coastal ridges along the beach. This inundation and the subsequent drop in the water level trap saline water in the inland areas, which leads to the evaporative deposition o作者: Antagonism 時(shí)間: 2025-3-26 22:35 作者: ORBIT 時(shí)間: 2025-3-27 01:17
Theorizing Socio-Spatial Practices,middle, and lower, and each sector represents the differential nature of the terrain, hydrology, vegetation, agricultural practices, and human intervention. The present work focuses on the systemic study of the riparian area along with the uniqueness of the corridor based on morphometric parameters 作者: 想象 時(shí)間: 2025-3-27 05:25
,Forschungslücke und Forschungsfragen,society, and economy of the coastal districts. The study highlights diminishing beach environs, conflicts between tourists and locals, and the evolution of natural beaches into “city by the sea (crowdy)”, economic impacts, and sustainable management of beach resources. The present study is conducted作者: Credence 時(shí)間: 2025-3-27 11:43 作者: SENT 時(shí)間: 2025-3-27 16:45
,Forschungslücke und Forschungsfragen,is to observe the dynamic morphological features of the tidal flats, to demarcate the continuous shifting of HTL and LTL, and to time scale the changes from sea level to soil property. Erosion and accretion are the continuous processes of the islands of the Hugli estuary by strong natural hydrologic作者: visual-cortex 時(shí)間: 2025-3-27 18:08
Psychologische Grundlagen der Wahrnehmung,face, bank margin tidal flats, and the tidal creek banks. The temporal changes of area as well as the changes in length and width of islands and bank margin tidal flats will be estimated by temporal satellite images. The areal change of mangroves and salt marshes, as well as their habitats and diver作者: Granular 時(shí)間: 2025-3-28 00:52 作者: ARK 時(shí)間: 2025-3-28 03:44
s of mangrove sensitivity to the sea level rise process in the Sundarban, land degradation of the hinterland drainage basins, the riparian environment of the coastal drainage basins, agricultural adaptability i978-3-031-42233-1978-3-031-42231-7作者: 諷刺 時(shí)間: 2025-3-28 06:58
Psychologische Grundlagen der Wahrnehmung,f Bengal. The islands of the Andaman and Nicobar Group are distributed on the eastern part of ‘Ninety Degree East Ridge’ bordering between the Andaman Sea and the Bay of Bengal in the sub-continent. From a geomorphological and topographical point of view, the main land coast extended from the presen作者: 中世紀(jì) 時(shí)間: 2025-3-28 14:16
Psychologische Grundlagen der Wahrnehmung,adjustments of the nearshore beach morphology via hydrodynamic and nearshore sediment dynamic processes. Choumukh and Rasalpur coastal sites within the extension of 21°20′25″N. 85°50′45″E and 21°39′55″N 87°12′37″E of the low-lying deltaic Balasore coast have been adopted for this present study. Subs作者: 尊嚴(yán) 時(shí)間: 2025-3-28 17:38
Letzte Etappe – die Schatzkartents in the Bay of Bengal region. The river carries sediment outlets into the shallow sea region of the Subarnarekha estuary mouth, which is further redistributed along the shoreline by the different reworking agents like waves, tides, currents, longshore drifts, and storm surges. Depending on the sh作者: ATP861 時(shí)間: 2025-3-28 21:23
Zweite Etappe – Standortbetrachtung the beach and dune sediment exchange. The established process-response models fail to predict the integral pattern of change due to the complexity of the system. Therefore, an alternate method, such as repeatedly measuring the topography with respect to a fixpoint/landmark to develop a comprehensiv作者: Colonoscopy 時(shí)間: 2025-3-29 01:12 作者: assail 時(shí)間: 2025-3-29 03:05
The Framework, An Introduction, of the shoreline influences the rate of accumulation and erosion in the study area, which is classified into multiple stages of the beach dune development process. The beach stage and dune stage modelling approach is based on the mutual co-adjustment of intertidal seashore surf-zone morphology, hyd作者: 清洗 時(shí)間: 2025-3-29 07:31
Zweite Etappe – Standortbetrachtungcal Asia. Due to climate change coupled with anthropogenic factors, the discharge of floodwater and sediments in the lagoon has been reduced, resulting in a low flow of water and sediments into the sea through the lagoon outlet. The longshore drift along the east coast of India is from south to nort作者: Insulin 時(shí)間: 2025-3-29 14:12
Erste Etappe – Was erwartet mich?dy beach berm and a surface layer of shells. Active swash wave energy accumulated sands on the backshores and pushed them landward by repeated overwash processes during high energy marine wave environments. The storm and non-storm conditions with steeper waves and less steep long-period swell waves 作者: 過(guò)于平凡 時(shí)間: 2025-3-29 18:36
For the Conditions of An Analysisds, lagoons, embayments, beach ridges and sand dunes, spits and bars, tidal mudflats and mangroves, sandy sea beaches, and rocky headlands. They harbour a large number of flora and other organisms in the regional coastal system and act as natural buffers against the tropical storms and high energy m作者: PACK 時(shí)間: 2025-3-29 23:10 作者: MILL 時(shí)間: 2025-3-30 02:37
Psychologische Grundlagen der Wahrnehmung,gradation is a process that can come into action in any physiographic environment. But its type, intensity, and magnitude vary from place to place. Land degradation is caused by anthropogenic factors as well as natural phenomena in the middle and lower courses of the Subarnarekha River basin. Defore作者: minaret 時(shí)間: 2025-3-30 06:41
Theorizing Socio-Spatial Practices,d play a significant role in providing a new dimension to the river continuum concept. It is the buffer zone where vegetation acts as a filter to maintain the health of the entire riparian area. The riparian corridor includes all perennial streams with defined channel flow. It also encompasses adjac作者: Gastric 時(shí)間: 2025-3-30 11:47 作者: 親愛(ài) 時(shí)間: 2025-3-30 14:56
roperties are considered the limiting factors for the successful growth of agriculture. The poor moisture retention capacity of the coarse-grained soil, high aridity, occasional and sporadic rainfall, and speedy surface run-off are the other limiting factors for steady agricultural production. The p作者: FUSC 時(shí)間: 2025-3-30 18:53 作者: calorie 時(shí)間: 2025-3-30 23:34 作者: 破裂 時(shí)間: 2025-3-31 04:23 作者: 音樂(lè)學(xué)者 時(shí)間: 2025-3-31 07:23 作者: Fulminate 時(shí)間: 2025-3-31 10:48
http://image.papertrans.cn/c/image/239866.jpg作者: faculty 時(shí)間: 2025-3-31 13:42
https://doi.org/10.1007/978-3-031-42231-7Geomorphological approaches; Emergent and submergent features; Hinterland plains; Laterite uplands; Crat作者: carotenoids 時(shí)間: 2025-3-31 17:33 作者: 擋泥板 時(shí)間: 2025-4-1 01:42 作者: Pelago 時(shí)間: 2025-4-1 03:23 作者: 橫截,橫斷 時(shí)間: 2025-4-1 07:43
Shoreline Change and Associated Beach Ridge Chenier Formations in the Subarnarekha Delta Region, Indnts in the Bay of Bengal region. The river carries sediment outlets into the shallow sea region of the Subarnarekha estuary mouth, which is further redistributed along the shoreline by the different reworking agents like waves, tides, currents, longshore drifts, and storm surges. Depending on the sh
