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<front>
<journal-meta>
<journal-id journal-id-type="publisher">ANGEO</journal-id>
<journal-title-group>
<journal-title>Annales Geophysicae</journal-title>
<abbrev-journal-title abbrev-type="publisher">ANGEO</abbrev-journal-title>
<abbrev-journal-title abbrev-type="nlm-ta">Ann. Geophys.</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">1432-0576</issn>
<publisher><publisher-name>Copernicus Publications</publisher-name>
<publisher-loc>Göttingen, Germany</publisher-loc>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.5194/angeo-26-3757-2008</article-id>
<title-group>
<article-title>The role of electric field and neutral wind in the generation of polar cap sporadic E</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Nygrén</surname>
<given-names>T.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Voiculescu</surname>
<given-names>M.</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Aikio</surname>
<given-names>A. T.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Department of Physical Sciences, University of Oulu, P.O. Box 3000, 90014, Finland</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Dept. of Physics, Faculty of Sciences, University &quot;Dunărea de Jos&quot; Galati, St. Domnească, No. 47, 800008 Galati, Romania</addr-line>
</aff>
<pub-date pub-type="epub">
<day>26</day>
<month>11</month>
<year>2008</year>
</pub-date>
<volume>26</volume>
<issue>12</issue>
<fpage>3757</fpage>
<lpage>3763</lpage>
<permissions>
<copyright-statement>Copyright: &#x000a9; 2008 T. Nygrén et al.</copyright-statement>
<copyright-year>2008</copyright-year>
<license license-type="open-access">
<license-p>This work is licensed under the Creative Commons Attribution 3.0 Unported License. To view a copy of this licence, visit <ext-link ext-link-type="uri"  xlink:href="https://creativecommons.org/licenses/by/3.0/">https://creativecommons.org/licenses/by/3.0/</ext-link></license-p>
</license>
</permissions>
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<abstract>
<p>This paper investigates the roles of electric field and neutral wind in the
generation of sporadic-E layers within the polar cap. Two Es layers above
Svalbard, observed by the EISCAT Svalbard Radar (ESR), were chosen for
investigation. The radar experiment contains four beam directions, and this
was used for determining the electric field. The neutral wind was obtained
from the HWM93 model. Formation of Es layers was calculated by integrating
the continuity equation under the action of driving forces due to neutral
wind and electric field. A flat height profile of metal ions was assumed in
the beginning. The calculation gives the time variation of the layer, which
can be compared with observations. In one case the electric field was shown
to be the main driving agent in layer generation. In the other case the
electric field was weak and the layer was produced mainly by the neutral
wind, but the electric field had influence on the height of the layer. A
fairly good agreement between the variations of the observed and calculated
layer altitudes was obtained and some agreement between the intensity
variations was also found.</p>
</abstract>
<counts><page-count count="7"/></counts>
</article-meta>
</front>
<body/>
<back>
<ref-list>
<title>References</title>
<ref id="ref1">
<label>1</label><mixed-citation publication-type="other" xlink:type="simple"> Bedey, D. F. and Watkins, B. J.: Simultaneous observations of thin ion layers and the ionospheric electric field over Sondrestrom, J. Geophys. Res., 106(A5), 8169–8183, 2001. </mixed-citation>
</ref>
<ref id="ref2">
<label>2</label><mixed-citation publication-type="other" xlink:type="simple"> Hedin, A. E.: Extension of the MSIS Thermospheric Model into the Middle and Lower Atmosphere, J. Geophys. Res., 96, 1159–1172, 1991. </mixed-citation>
</ref>
<ref id="ref3">
<label>3</label><mixed-citation publication-type="other" xlink:type="simple"> Hedin, A. E., Biondi, M., Burnside,R., Hernandez, G., Johnson, R., Killeen, T., Mazaudier, C., Meriwether, J., Salah,J., Sica, R., Smith, R., Spencer, N., Wickwar, V., and Virdi, T.: Revised Global Model of Thermosphere Winds Using Satellite and Ground-Based Observations, J. Geophys. Res., 96, 7657–7688, 1991. </mixed-citation>
</ref>
<ref id="ref4">
<label>4</label><mixed-citation publication-type="other" xlink:type="simple"> Hedin, A. E., Fleming, E. L., Manson, A. H., Schmidlin, F. J., Avery, S.\ K., Clark, R. R., Franke, S. J., Fraser, G. J., Tsuda, T., Vial, F., and Vincent, R. A.: Empirical wind model for the upper, middle and lower atmosphere, J. Atmos. Terr. Phys. 58, 1421–1447, 1996. </mixed-citation>
</ref>
<ref id="ref5">
<label>5</label><mixed-citation publication-type="other" xlink:type="simple">Kirkwood, S. and Nilsson, H.: High-latitude sporadic-E and other thin layers – the role of magnetospheric electric fields, Space Sci. Rev., 91, 579–613, 2000.</mixed-citation>
</ref>
<ref id="ref6">
<label>6</label><mixed-citation publication-type="other" xlink:type="simple"> MacDougall, J. W., Jayachandran, P. T., and Plane, J. M. C.: Polar cap sporadic E: part 1, Observations, J. Atmos. Solar-Terr. Phys., 62, 1155–1167, 2000a. </mixed-citation>
</ref>
<ref id="ref7">
<label>7</label><mixed-citation publication-type="other" xlink:type="simple"> MacDougall, J. W., Jayachandran, P. T., and Plane, J. M. C.: Polar cap sporadic E: part 2, Modeling, J. Atmos. Solar-Terr. Phys., 62, 1168–1176, 2000b. </mixed-citation>
</ref>
<ref id="ref8">
<label>8</label><mixed-citation publication-type="other" xlink:type="simple"> MacDougall, J. W. and Jayachandran, P. T.: Sporadic E at cusp latitudes, J. Atmos. Solar-Terr. Phys., 67, 1419–1426, 2005. </mixed-citation>
</ref>
<ref id="ref9">
<label>9</label><mixed-citation publication-type="other" xlink:type="simple"> Mathews, J. D.: Sporadic E: current views and recent progress, J. Atmos. Solar-Terr. Phys., 60, 413–435, 1998. </mixed-citation>
</ref>
<ref id="ref10">
<label>10</label><mixed-citation publication-type="other" xlink:type="simple"> Nygrén, T., Jalonen, L., Oksman, J., and Turunen, T.: The role of electric field and neutral wind direction in the formation of sporadic E layers, J. Atmos. Terr. Phys., 46, 373–381, 1984. </mixed-citation>
</ref>
<ref id="ref11">
<label>11</label><mixed-citation publication-type="other" xlink:type="simple"> Nygrén, T., Aikio, A. T., Voiculescu, M., and Ruohoniemi, J. M.: IMF effect on sporadic-E layers at two northern polar cap sites: Part II – Electric field, Ann. Geophys., 24, 901–913, 2006. </mixed-citation>
</ref>
<ref id="ref12">
<label>12</label><mixed-citation publication-type="other" xlink:type="simple"> Parkinson, M. L., Dyson, P. L., Monselesan, D. P., and Morris, R. J.: On the role of electric field direction in the formation of sporadic E-layers in the southern polar cap ionosphere, J. Atmos. Solar-Terr. Phys., 60, 471–491, 1998. </mixed-citation>
</ref>
<ref id="ref13">
<label>13</label><mixed-citation publication-type="other" xlink:type="simple"> Ruohoniemi, M. and Greenwald, R. A.: Statistical patterns of high-latitude convection obtained from Goose Bay HF radar observations, J. Geophys. Res., 101, 21 743–21 763, 1996. </mixed-citation>
</ref>
<ref id="ref14">
<label>14</label><mixed-citation publication-type="other" xlink:type="simple"> Voiculescu M. and Ignat, M.: The role of total wind in the vertical dynamics of ions in the E region at high latitudes, Ann. Geophys., 23, 1191–1197, 2005. </mixed-citation>
</ref>
<ref id="ref15">
<label>15</label><mixed-citation publication-type="other" xlink:type="simple"> Voiculescu, M., Aikio, A. T., Nygrén, T., and Ruohoniemi, J. M.: IMF effect on sporadic-E layers at two northern polar cap sites: Part I – statistical study, Ann. Geophys., 24, 887–900, 2006. </mixed-citation>
</ref>
<ref id="ref16">
<label>16</label><mixed-citation publication-type="other" xlink:type="simple"> Wan, W., Parkinson, M. L., Dyson, P. L., Breed, A. M., and Morris, R. J.: A statistical study of the interplanetary magnetic field control of sporadic E layer occurrence in the southern polar cap ionosphere, J. Atmos. Solar-Terr. Phys., 61, 1357–1366, 1999. </mixed-citation>
</ref>
<ref id="ref17">
<label>17</label><mixed-citation publication-type="other" xlink:type="simple"> Whitehead, J. D.: Recent work on mid-latitude and equatorial sporadic-E, J. Atoms. Terr. Phys., 51, 401–424, 1989. </mixed-citation>
</ref>
<ref id="ref18">
<label>18</label><mixed-citation publication-type="other" xlink:type="simple"> Zhang, S. P., Thayer, J. P., Roble, R. G., Salah, J. E., Shepherd, G.\ G., Goncharenko, L. P., and Zhou, Q. H.: Latitudinal variations of neutral wind structures in the lower thermosphere for the March equinox period, J. Atoms. Solar-Terr. Phys., 66, 105–117, 2004. </mixed-citation>
</ref>
</ref-list>
</back>
</article>