North Atlantic sea surface temperature, solar activity and the climate of Northern Fennoscandia

被引：11
作者：
Ogurtsov, M. [1 ,3 ]
Lindholm, M. [2 ]
Jalkanen, R. [2 ]
Veretenenko, S. V. [1 ,4 ]
机构：
[1] AF Ioffe Phys Tech Inst, St Petersburg, Russia
[2] Nat Resources Inst Finland Luke, POB 16, FI-96301 Rovaniemi, Finland
[3] Cent Astron Observ Pulkovo, St Petersburg, Russia
[4] St Petersburg Univ, St Petersburg, Russia
来源：
ADVANCES IN SPACE RESEARCH | 2017年 / 59卷 / 04期
关键词：
Solar activity; Climate; North Atlantic; MULTIDECADAL OSCILLATION; RECONSTRUCTION; AD; VARIABILITY; FREQUENCY; BE-10;
D O I：
10.1016/j.asr.2016.11.025
中图分类号：
V [航空、航天];
学科分类号：
08 ; 0825 ;
摘要：
Seven proxies of summer temperature in Northern Fennoscandia, sea surface temperature in the North Atlantic and solar activity were analyzed over AD 1567-1986. A stable and significant positive correlation between summer temperatures in Northern Fennoscandia and sea surface temperature in the North Atlantic is shown to exist during the entire time interval. In addition, a significant correlation between solar activity and (a) summer temperature in Northern Fennoscandia as well as (b) surface temperature in the North Atlantic was found during AD 1715-1986. Throughout 1567-1715 correlation is less significant and has an opposite sign. Thus we show that the variation of sea surface temperature in the North Atlantic could be a physical agent, which transferred solar influence on Northern Fennoscandian temperature at least during AD 1715-1986. (C) 2016 COSPAR. Published by Elsevier Ltd. All rights reserved.
引用
收藏
页码：980 / 986
页数：7
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