Titlebook: Climate Change and Environmental Impacts: Past, Present and Future Perspective; Binita Phartiyal,Rahul Mohan,Anil Kumar Gupta Book 2022 Th

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書(shū)目名稱Climate Change and Environmental Impacts: Past, Present and Future Perspective影響因子(影響力)




書(shū)目名稱Climate Change and Environmental Impacts: Past, Present and Future Perspective影響因子(影響力)學(xué)科排名




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書(shū)目名稱Climate Change and Environmental Impacts: Past, Present and Future Perspective網(wǎng)絡(luò)公開(kāi)度學(xué)科排名




書(shū)目名稱Climate Change and Environmental Impacts: Past, Present and Future Perspective被引頻次




書(shū)目名稱Climate Change and Environmental Impacts: Past, Present and Future Perspective被引頻次學(xué)科排名




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書(shū)目名稱Climate Change and Environmental Impacts: Past, Present and Future Perspective讀者反饋




書(shū)目名稱Climate Change and Environmental Impacts: Past, Present and Future Perspective讀者反饋學(xué)科排名

Mercantile

J. v. Meurs,A. M. Joussen,G. A. Lutty PhDble baseline to analyze the effects of these transcendent climatic changes on the mammalian community structures. The present investigation is an attempt to examine the palaeohabitat of a Neogene (Middle Miocene: ~15–11.5?Ma) geographically distant (i.e., from Spain, China, and India) extinct mammal

Favorable

F. M. A. Heu?en,S. R. Sadda,A. C. Walshte events of the Neogene, MMCO (Mid-Miocene Climate Optimum) that occurred around ~17–15?Ma is considered to be the most recent extreme global warming episode. The global warming during MMCO, created annual surface temperature ~3–4?°C higher than the present, is equivalent to the warming predicted f

Agnosia

Detonate

intention

https://doi.org/10.1007/978-3-642-66435-9edmont Slope, Pediplain) morphological units, of Tawa river basin, Hoshangabad District, Madhya Pradesh was attempted for understanding the Quaternary climate of Narmada Valley. The statistical evaluation and analysis of the chemical data suggests that Narmada alluvium is chemically immature derived

intention

Preclinical Models of Retinitis Pigmentosa,ciers six?major sub-basins (upper Jhelum, Suru and Zanskar, Chandra, Spiti, Satluj and upper Indus?basin) covering parts of western Himalayan region were selected?for?analysis. For this purpose, Landsat images (MSS, TM, ETM+, OLI/TIRS), Survey of India toposheets (SoI), high resolution?Google Earth

背心

Carlos Rodriguez-Galindo,Matthew W. Wilsone Holocene. This rapid warming in the Arctic has a significant impact on the development and evolution of landforms. In glaciated Arctic region (glacial valleys), abrupt climatic shifts are captured in the landforms developed and their modification from glacial to proglacial (through glacier retreat

有惡臭

萬(wàn)神殿

Expression and Purification of CRABPs from ,s very less and very few glaciers are being continuously monitored in Indian Himalayas. The Himalayan cryosphere system is sustained and regulated by the interaction of temperature and precipitation forced through the orographic processes. In this study, an extensive meteorological analysis has been