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

purulent

書目名稱Climate Variability and Sunspot Activity影響因子(影響力)




書目名稱Climate Variability and Sunspot Activity影響因子(影響力)學(xué)科排名




書目名稱Climate Variability and Sunspot Activity網(wǎng)絡(luò)公開度




書目名稱Climate Variability and Sunspot Activity網(wǎng)絡(luò)公開度學(xué)科排名




書目名稱Climate Variability and Sunspot Activity被引頻次




書目名稱Climate Variability and Sunspot Activity被引頻次學(xué)科排名




書目名稱Climate Variability and Sunspot Activity年度引用




書目名稱Climate Variability and Sunspot Activity年度引用學(xué)科排名




書目名稱Climate Variability and Sunspot Activity讀者反饋




書目名稱Climate Variability and Sunspot Activity讀者反饋學(xué)科排名

decipher

Major Modes of Variability it defined and discussed ENSO (El Ni?o Southern Oscillation), NAO (North Atlantic Oscillation), AO and AAO (Arctic Oscillation, Antarctic Oscillation), Indian Monsoon, Indian Ocean Dipole (IOD), PDO (Pacific Decadal Oscillation) and AMO (Atlantic Multidecadal Oscillation). Later it attended stratos

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Stratosphere-Troposphere Couplinghe Sun and QBO to regulate such coupling. It explores Holton-Tan effect. The combined influence of the Sun and QBO to regulate upper stratospheric polar temperature was also attended. The role of polar annular modes was described that communicate such signal down to the troposphere. Various other ro

LUCY

fastness

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Ocean Couplingveyor belt and global wind-driven ocean circulation. Section . describes ENSO, and focus is on various issues: (i) ENSO, thermocline and upper ocean heat content, (ii) ENSO and delayed oscillator theory, (iii) ENSO and shallow MOC in tropical Pacific and (iv) pycnocline convergence vs. Nino region s

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exhibit

FLOUR

使痛苦

An Overview of Solar Influence on Climatelow 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