Influence of the North Atlantic dipole on climate changes over Eurasia

International Conference and Early Career Scientists School on Environmental Observations, Modelling and Information Systems

生态环境科学;计算机科学

Serykh, I.V.^1

Shirshov Institute of Oceanology, Russian Academy of Sciences, Nakhimovsky prospect, 36, Moscow

117997, Russia^1

关键词: Hydrometeorological conditions;    Inter-decadal pacific oscillations;    Internal oscillation;    Near surface temperature;    North Atlantic oscillations;    Ocean-atmosphere interactions;    Pacific decadal oscillation;    Sensible heat flux;   

Others  :  https://iopscience.iop.org/article/10.1088/1755-1315/48/1/012004/pdf
DOI  :  10.1088/1755-1315/48/1/012004

来源: IOP

【 摘 要 】

In this paper, some hydrophysical and meteorological characteristics of negative (1948-1976 and 1999-2015) and positive (1977-1998) phases of the Pacific Decadal Oscillation (PDO) and Interdecadal Pacific Oscillation (IPO) in the North Atlantic and Eurasia are constructed and investigated. Specifically, the near-surface temperature, sea-level atmospheric pressure, wind speed, heat content of the upper 700 m ocean layer, water temperature and salinity at various depths, the latent and sensible heat fluxes from the ocean to the atmosphere are analyzed. The fields obtained are in good agreement and complement each other. This gives important information about the hydrometeorological conditions in the region under study. Analysis of these data has shown that in the upper 1000 m North Atlantic layer there is a thermal dipole which can be interpreted as an oceanic analog of the atmospheric North Atlantic Oscillation (NAO). An index of the North Atlantic Dipole (NAD) as the difference between the mean heat contents in the upper 700 m oceanic layer between the regions (50°-70° N; 60°-10° W) and (20°-40° N; 80°-30° W) is proposed. A possible physical mechanism of the internal oscillations with a quasi-60-year period in the North Atlantics- Eurasia system of ocean-atmosphere interactions is discussed.