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

被引：10

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

页码：980 / 986

页数：7

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