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scostep 2010 (stp12) - Leibniz-Institut für Atmosphärenphysik an der ...

scostep 2010 (stp12) - Leibniz-Institut für Atmosphärenphysik an der ...

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STP12 Abstracts<br />

Berlin, 12 - 16 July <strong>2010</strong><br />

SCOSTEP Symposium <strong>2010</strong><br />

The solar <strong>an</strong>d geomagnetic activity influence on long-term ch<strong>an</strong>ge of troposphere<br />

characteristics<br />

Molodykh Sergey , Zherebtsov Gely , Kovalenko Vladimir<br />

<strong>Institut</strong>e of Solar-Terrestrial Physics SB RAS<br />

Mech<strong>an</strong>isms of solar activity effects on weather <strong>an</strong>d climate have been discussed. Authors<br />

proposed a physical mech<strong>an</strong>ism of solar activity effects on climatic characteristics <strong>an</strong>d the<br />

atmospheric circulation through the atmospheric electricity. A model of the solar activity<br />

effect on climatic characteristics of the Earth’s troposphere was elaborated on the basis of the<br />

mech<strong>an</strong>ism un<strong>der</strong> consi<strong>der</strong>ation. The model key concept is the heliogeophysical disturb<strong>an</strong>ce<br />

effect on the Earth climatic system’s parameters, which influence energy flux going from the<br />

Earth to space in high-latitude areas. According to our model, when the solar activity<br />

increases, radiation cooling of high-latitude regions decreases, thermobaric field restructures,<br />

average meridi<strong>an</strong> gradient of temperature between polar <strong>an</strong>d equatorial regions decreases,<br />

defining the atmospheric circulation. The energy outflow from low latitude regions falls as a<br />

result of the decrease of meridional temperature gradient; it results in the temperature increase<br />

at middle <strong>an</strong>d low latitude.<br />

In the framework of the model consi<strong>der</strong>ed, the <strong>an</strong>alysis results are presented <strong>an</strong>d discussed<br />

of regularities of variations in geomagnetic activity <strong>an</strong>d troposphere thermobaric<br />

characteristics for 1900–2007. It was shown that observable long-term ch<strong>an</strong>ges in troposphere<br />

characteristics are generally caused by ch<strong>an</strong>ges in the un<strong>der</strong>lying surface. It c<strong>an</strong> be explained<br />

by the fact that the accumulation of individual heliogeophysical disturb<strong>an</strong>ce effects occurs in<br />

the un<strong>der</strong>lying surface (mainly in the oce<strong>an</strong>).<br />

The continuous increase of the Earth climatic system heat content has been observed from<br />

1910 till now. Un<strong>der</strong> the model, we made <strong>an</strong>alysis of regularities, which un<strong>der</strong>lie variations of<br />

geomagnetic activity <strong>an</strong>d troposphere thermobaric characteristics. These results <strong>an</strong>d ch<strong>an</strong>ges<br />

of the global circulation in the atmosphere <strong>an</strong>d oce<strong>an</strong> allow the conclusion that the warming<br />

observed in the 20 th century c<strong>an</strong> be mostly explained by variations of the solar activity level.<br />

Scenario for long-term ch<strong>an</strong>ges of physical processes in the Earth atmosphere, cryosphere<br />

<strong>an</strong>d oce<strong>an</strong> is presented on the basis of the model of the solar activity effect on the troposphere<br />

circulation <strong>an</strong>d thermobaric characteristics.

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