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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Chapter 5 Geodesics and Jacobi Fields,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 relev

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,Symmetric Spaces and K?hler Manifolds,low chart, focusing on the Pacific region. It discussed hypotheses and evidence relating the combined influences of the Quasi-Biennial Oscillation, the El Ni?o–Southern Oscillation, and the solar cycle on the Walker and Hadley circulations in the context of ocean–atmosphere coupling. It suggests, in

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Chapter 6 Geodesics and Jacobi Fields,iscussed solar ‘top-down’ vs. ‘bottom-up’ mechanism. Then it addressed some limitations related to methodology and discussed solar peak year compositing method. Solar NAO connection as captured by multiple linear regression was also attended. It also discussed the solar lag relationship. At the end,

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Climate Variability and Sunspot Activity978-3-319-77107-6Series ISSN 2194-5217 Series E-ISSN 2194-5225

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Sectional Curvature Comparison II,d sea surface temperature (SST) which was followed by defining north-south Hadley and east-west Walker circulation. It also defined and described Ferrel cell, Polar cell and various jets. It explained thermal-wind balance relationship and its relevance to jet formation.

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Sectional Curvature Comparison II,signal on tropical Pacific SST-active solar years and ENSO and . solar signal on tropical Pacific SST?– El Ni?o or La Ni?a. It reconciled those contradictions and additionally proposed two different mechanisms. The mechanisms differ in the earlier period to that from the later.