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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 />

Features of Spatial Structure of Tropospheric Response to Solar <strong>an</strong>d Geomagnetic<br />

Activity Level Variations<br />

Zherebtsov Geliy , Vasilyeva Larisa , Kovalenko Vladimir , Molodyh Sergey<br />

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

We have carried out a multifactor correlation <strong>an</strong>alysis of the connection<br />

between the heat content of various tropospheric layers <strong>an</strong>d solar (f 10.7 cm) <strong>an</strong>d<br />

geomagnetic (AA-index) activity level variations over the period of 1950–2007.<br />

To calculate the heat content, we used NCEP/NCAR re<strong>an</strong>alysis data. We<br />

<strong>an</strong>alyzed the influence of volc<strong>an</strong>oes, El-Nino, <strong>an</strong>d Arctic sea ice area on<br />

characteristics of the connection un<strong>der</strong> study.<br />

The degree of the connection between tropospheric heat content ch<strong>an</strong>ges <strong>an</strong>d<br />

solar <strong>an</strong>d geomagnetic activity variations was demonstrated to depend<br />

essentially on the period of smoothing of time series. When the time scale is<br />

increased to 5 years, the correlation coefficient rises consi<strong>der</strong>ably (to 0.6–0.7) in<br />

most regions.<br />

We have found that the heat content correlates with geomagnetic activity in<br />

most of the troposphere. But in some regions one c<strong>an</strong> see a signific<strong>an</strong>t<br />

<strong>an</strong>ticorrelation decreasing with dist<strong>an</strong>ce from the un<strong>der</strong>lying surface.<br />

The tropospheric heat content response to the geomagnetic activity influence<br />

is characterized by a signific<strong>an</strong>t spatial inhomogeneity which is most<br />

pronounced near the un<strong>der</strong>lying surface <strong>an</strong>d consi<strong>der</strong>ably ch<strong>an</strong>ges with height.<br />

The spatial structure of the response enlarges with increasing height, <strong>an</strong>d the<br />

region of the peak positive response shifts to low latitudes.

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