Regional tropospheric responses to long-term solar activity variations

被引：15

作者：

Raspopov, O. M. ^{[1
]}

Dergachev, V. A. ^{[2
]}

Kuzmin, A. V. ^{[6
]}

Kozyreva, O. V. ^{[5
]}

Ogurtsov, M. G. ^{[2
]}

Kolstrom, T. ^{[4
]}

Lopatin, E. ^{[3
,4
]}

机构：

[1] Russian Acad Sci, Pushkov Inst Terr Magnetism Ionosphere & Radiowav, St Petersburg Branch Filial, St Petersburg 123032, Russia

[2] Russian Acad Sci, AF Ioffe Phys Tech Inst, St Petersburg 194021, Russia

[3] Russian Acad Sci, Biol inst KomiSC, Ural Branch, Syktyvkar, Russia

[4] Univ Joensuu, Mekrijarvi Res Stn, FIN-82900 Joensuu, Finland

[5] Russian Acad Sci, Inst Phys Earth, Moscow 123810, Russia

[6] Russian Acad Sci, Polar Alpian Bot Garden Inst, Kola Sci Ctr, Murmansk Region 184000, Russia

来源：

ADVANCES IN SPACE RESEARCH | 2007年 / 40卷 / 07期

基金：

俄罗斯基础研究基金会;

关键词：

solar activity; climate variability; de Vries solar cycle; ICE CORE; MODEL; VARIABILITY; CIRCULATION; RADIOCARBON; ATMOSPHERE; GREENLAND;

D O I：

10.1016/j.asr.2007.01.081

中图分类号：

V [航空、航天];

学科分类号：

08 ; 0825 ;

摘要：

The influence of similar to 200-year solar activity variations (de Vries cyclicity) on climatic parameters has been analyzed. Analysis of palaeoclimatic data from different regions of the Earth for the last millennium has shown that similar to 200-year variations in solar activity give rise to a pronounced climatic response. Owing to a nonlinear character of the processes in the atmosphere-ocean system and the inertia of this system, the climatic response to the global influence of solar activity variations has been found to have a regional character. The regions where the climatic response to long-term solar activity variations is stable and the regions where the climatic response is unstable, both in time and space, have been revealed. It has also been found that a considerable lag of the climatic response and reversal of its sign with respect to the solar signal can occur. Comparison of the obtained results with the simulation predictions of the atmosphere-ocean system response to long-term solar irradiance variations (T > 40 years) has shown that there is a good agreement between experimental and simulation results. (c) 2007 COSPAR. Published by Elsevier Ltd. All rights reserved.

引用

页码：1167 / 1172

页数：6

共 18 条

[1]

DELWORTH T, 1993, J CLIMATE, V6, P1993, DOI 10.1175/1520-0442(1993)006<1993:IVOTTC>2.0.CO

[2]

[3] Multidecadal climate variability in the Greenland Sea and surrounding regions: A coupled model simulation [J].

Delworth, TL ;

Manabe, S ;

Stouffer, RJ .

GEOPHYSICAL RESEARCH LETTERS, 1997, 24 (03) :257-260

[4] MAUNDER MINIMUM [J].

EDDY, JA .

SCIENCE, 1976, 192 (4245) :1189-1202

[5] Temperature-sensitive Tien Shan tree ring chronologies show multi-centennial growth trends [J].

Esper, J ;

Shiyatov, SG ;

Mazepa, VS ;

Wilson, RJS ;

Graybill, DA ;

Funkhouser, G .

CLIMATE DYNAMICS, 2003, 21 (7-8) :699-706

[6]

Haeberli W., 2003, PAGES NEWS, V1, P13, DOI DOI 10.22498/PAGES.11.1.13

[7] Climate oscillations as recorded in Svalbard ice core δ18O records between AD 1200 and 1997 [J].

Isaksson, E ;

Divine, D ;

Kohler, J ;

Martma, T ;

Pohjola, V ;

Motoyama, H ;

Watanabe, O .

GEOGRAFISKA ANNALER SERIES A-PHYSICAL GEOGRAPHY, 2005, 87A (01) :203-214

[8] A reconstruction of mid-summer temperatures from ring-widths of Scots pine since AD 50 in northern Fennoscandia [J].

Lindholm, M ;

Eronen, M .

GEOGRAFISKA ANNALER SERIES A-PHYSICAL GEOGRAPHY, 2000, 82A (04) :527-535

[9]

Maksimov E.B., 1972, IZVESTIYA USSR ACAD, V2, P105

[10] A 1400-year high-resolution record of atmospheric circulation over the North Atlantic and Asia [J].

Meeker, LD ;

Mayewski, PA .

HOLOCENE, 2002, 12 (03) :257-266

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