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Titlebook: Science, Policies and Conflicts of Climate Change; An Indian Perspectiv Neloy Khare Book 2022 The Editor(s) (if applicable) and The Author(

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發(fā)表于 2025-3-25 07:20:22 | 只看該作者
978-3-031-16256-5The Editor(s) (if applicable) and The Author(s), under exclusive license to Springer Nature Switzerl
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發(fā)表于 2025-3-25 11:33:48 | 只看該作者
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發(fā)表于 2025-3-25 14:57:14 | 只看該作者
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發(fā)表于 2025-3-25 18:10:17 | 只看該作者
Climate Changes over the Indian Subcontinent: Scenarios and Impactsd droughts, and its impact on some of the important sectors. The chapter shows clear evidence of a decline in crop production and productivity of some of the important crops such as wheat, rice, sugarcane, maize, potato, tomato, etc. The recent studies established an increase in morbidity and mortal
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發(fā)表于 2025-3-25 21:12:44 | 只看該作者
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發(fā)表于 2025-3-26 04:12:28 | 只看該作者
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發(fā)表于 2025-3-26 08:22:40 | 只看該作者
Vulnerability Analysis of Sea Level Rise (SLR) on a Micro-tidal Coast: A Case Study of Nagapattinam o, impacts of storm surges, tsunamis, coastal floods, and coastal erosion in the low-lying coastal area cause gradual loss of coastal land. In the present study, the impact of sea level rise on the sandy coast of the Nagapattinam sector is assessed to understand the devastation incurred in both phys
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發(fā)表于 2025-3-26 11:55:20 | 只看該作者
Lacustrine Records of Anthropogenic Change and Precipitation in the Monsoonal Core Zone of Central Irtilizers (K, P) are mainly derived other than soil particles of the catchment. Similarly, deforestation in the region was evident during ~1967–1975 coinciding with the period of the highest soil erosion. Another major phase of soil erosion caused by anthropogenic activities was noticed during ~1992
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發(fā)表于 2025-3-26 16:01:26 | 只看該作者
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發(fā)表于 2025-3-26 17:50:38 | 只看該作者
Manganese Mineralization in Manganiferous Quartzite in the Boringpadar-Amath Area, Eastern Ghats Mob fractured and brecciated which occurs at the contact of khondalite. Braunite, bixbyite, jacobsite, manganite, pyrolusite and todorokite are primary minerals that are associated with host rocks like quartzite and these minerals occur as inclusions and anhedral in shape. Secondary minerals are formed
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