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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 />

Morphology of 557.7 nm dayglow emission un<strong>der</strong> varying solar activity conditions<br />

Sunil Krishna MV , Singh Vir<br />

Indi<strong>an</strong> <strong>Institut</strong>e of Technology Roorkee<br />

The atomic oxygen emission at 557.7 nm is the most widely observed airglow feature in the<br />

upper mesosphere <strong>an</strong>d lower thermospheric regions. The approximation of solar irradi<strong>an</strong>ce<br />

fluxes is very crucial in the modeling of this emission. The recently introduced Solar2000<br />

EUV flux model is a suitable c<strong>an</strong>didate to provide the solar EUV flux for <strong>an</strong>y level of solar<br />

activity on <strong>an</strong>y given day. The Solar2000 EUV flux model has not been tested for its<br />

applicability in the airglow modeling studies. In the present study a comprehensive model has<br />

been developed to study the 557.7 nm dayglow emission using Solar2000 EUV flux model.<br />

This study presents the model results of diurnal <strong>an</strong>d yearly variations of 557.7 nm dayglow<br />

emission un<strong>der</strong> equinox conditions. The effect of varying solar activity on this emission is<br />

studied for a period of five years (2001-2005) at a fixed date of April 3. This date is chosen<br />

due to the fact of large variations in the solar activity during the period of five years. The<br />

volume emission rates obtained from the model in the upper mesospheric region are found<br />

higher th<strong>an</strong> the observed results. This discrep<strong>an</strong>cy is due to the extremely high values of solar<br />

EUV flux generated by the Solar2000 EUV flux model at 102.5 <strong>an</strong>d 103.7 nm wavelengths.<br />

The model is found in good agreement with the measurements in the thermospheric region.<br />

The morphology is presented as a function of F10.7 solar index for five years (2001 – 2005)<br />

equator <strong>an</strong>d 45◦ N at a fixed longitude.

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