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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

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樓主: obdurate
21#
發(fā)表于 2025-3-25 05:59:34 | 只看該作者
22#
發(fā)表于 2025-3-25 08:18:22 | 只看該作者
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
23#
發(fā)表于 2025-3-25 15:28:36 | 只看該作者
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
24#
發(fā)表于 2025-3-25 18:23:31 | 只看該作者
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
25#
發(fā)表于 2025-3-25 22:24:30 | 只看該作者
26#
發(fā)表于 2025-3-26 02:34:06 | 只看該作者
27#
發(fā)表于 2025-3-26 07:29:00 | 只看該作者
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
28#
發(fā)表于 2025-3-26 10:59:26 | 只看該作者
29#
發(fā)表于 2025-3-26 13:25:54 | 只看該作者
30#
發(fā)表于 2025-3-26 18:55:18 | 只看該作者
,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
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