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Titlebook: Climate Variability and Sunspot Activity; Analysis of the Sola Indrani Roy Book 2018 Springer International Publishing AG, part of Springer

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Solar Influence: ‘Top Down’ vs. ‘Bottom Up’wn’ mechanism. In the ‘bottom-up’ pathway, the Sun can directly influence sea surface temperature (SST) without stratospheric feedback, whereas the ‘top-down’ solar influence is generated through the stratosphere without any influence from oceans. Those two routes are discussed in details with relevant supporting studies.
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Chapter 5 Geometry of Submanifolds,This chapter covered Arctic and Antarctic climate. It discussed Arctic warming and focused on various related areas including Arctic Sea ice – last few years and recent decline. Recent behaviour of Antarctic Sea ice was also addressed.
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Riemannian Geometry and Geometric AnalysisThis chapter focused on greenhouse effect and covered various relevant areas. Starting from laws of radiation, it included discussion on solar radiation vs. terrestrial radiation, atmospheric windows for terrestrial radiation, water vapour and carbon dioxide (CO.) as greenhouse gases, radiative forcing and global energy balance, etc.
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The Arctic and Antarctic Sea IceThis chapter covered Arctic and Antarctic climate. It discussed Arctic warming and focused on various related areas including Arctic Sea ice – last few years and recent decline. Recent behaviour of Antarctic Sea ice was also addressed.
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Green House Gas WarmingThis chapter focused on greenhouse effect and covered various relevant areas. Starting from laws of radiation, it included discussion on solar radiation vs. terrestrial radiation, atmospheric windows for terrestrial radiation, water vapour and carbon dioxide (CO.) as greenhouse gases, radiative forcing and global energy balance, etc.
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2194-5217 nic influences, ozone depletion in the stratosphere, Arctic and Antarctic sea ice, etc. At the end of the book, there are few questions and exercises for students. This book is based on the lecture series that 978-3-030-08372-4978-3-319-77107-6Series ISSN 2194-5217 Series E-ISSN 2194-5225
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