Planetary Wave Periods in foF2 Time Variations Based on Winter Data from Kaliningrad Station in 2008−2010
The study presents the results of the analysis of the F 2-layer critical frequency variations obtained for the winter periods of 2008–2010, during which sudden stratospheric warmings were observed. The data were obtained at Kaliningrad ionospheric station (54.6° N, 20° E) with the Parus digital iono...
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| Veröffentlicht in: | Geomagnetism and Aeronomy 2018-05, Vol.58 (3), p.420-429 |
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| container_title | Geomagnetism and Aeronomy |
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| creator | Koren’kov, Yu. N. Bessarab, F. S. Koren’kova, N. A. Leshchenko, V. S. |
| description | The study presents the results of the analysis of the
F
2-layer critical frequency variations obtained for the winter periods of 2008–2010, during which sudden stratospheric warmings were observed. The data were obtained at Kaliningrad ionospheric station (54.6° N, 20° E) with the
Parus
digital ionosonde in standard sounding mode. The mean daily
foF2
values were used in the analysis. The results of spectral analysis based on continuous wavelet transform showed that, during all of the warmings that occurred in 2008–2010, the
foF2
time variations demonstrated the presence of wave processes with periods of approximately 5−6 days, as well as more extended processes with periods of ~10−13 and 23−30 days. These periods coincide with the characteristic periods of planetary waves observed in the mesosphere during sudden stratospheric warmings, while the 13- and 30-day periods can be conditioned by the influence of the Sun. |
| doi_str_mv | 10.1134/S0016793218030088 |
| format | Article |
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F
2-layer critical frequency variations obtained for the winter periods of 2008–2010, during which sudden stratospheric warmings were observed. The data were obtained at Kaliningrad ionospheric station (54.6° N, 20° E) with the
Parus
digital ionosonde in standard sounding mode. The mean daily
foF2
values were used in the analysis. The results of spectral analysis based on continuous wavelet transform showed that, during all of the warmings that occurred in 2008–2010, the
foF2
time variations demonstrated the presence of wave processes with periods of approximately 5−6 days, as well as more extended processes with periods of ~10−13 and 23−30 days. These periods coincide with the characteristic periods of planetary waves observed in the mesosphere during sudden stratospheric warmings, while the 13- and 30-day periods can be conditioned by the influence of the Sun.</description><identifier>ISSN: 0016-7932</identifier><identifier>EISSN: 1555-645X</identifier><identifier>EISSN: 0016-7940</identifier><identifier>DOI: 10.1134/S0016793218030088</identifier><language>eng</language><publisher>Moscow: Pleiades Publishing</publisher><subject>Conditioning ; Continuous wavelet transform ; Earth and Environmental Science ; Earth Sciences ; F 2 region ; foF2 ; Geophysics/Geodesy ; Ionosondes ; Mesosphere ; Planetary waves ; Spectral analysis ; Stratosphere ; Stratospheric warming ; Wave period ; Wavelet analysis ; Wavelet transforms</subject><ispartof>Geomagnetism and Aeronomy, 2018-05, Vol.58 (3), p.420-429</ispartof><rights>Pleiades Publishing, Ltd. 2018</rights><rights>Geomagnetism and Aeronomy is a copyright of Springer, (2018). All Rights Reserved.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c316t-b708db943b71e95f591d7d0b248452ff5ed55b11b0ae9ff073321b8e3c5a8983</citedby><cites>FETCH-LOGICAL-c316t-b708db943b71e95f591d7d0b248452ff5ed55b11b0ae9ff073321b8e3c5a8983</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1134/S0016793218030088$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1134/S0016793218030088$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,776,780,27901,27902,41464,42533,51294</link.rule.ids></links><search><creatorcontrib>Koren’kov, Yu. N.</creatorcontrib><creatorcontrib>Bessarab, F. S.</creatorcontrib><creatorcontrib>Koren’kova, N. A.</creatorcontrib><creatorcontrib>Leshchenko, V. S.</creatorcontrib><title>Planetary Wave Periods in foF2 Time Variations Based on Winter Data from Kaliningrad Station in 2008−2010</title><title>Geomagnetism and Aeronomy</title><addtitle>Geomagn. Aeron</addtitle><description>The study presents the results of the analysis of the
F
2-layer critical frequency variations obtained for the winter periods of 2008–2010, during which sudden stratospheric warmings were observed. The data were obtained at Kaliningrad ionospheric station (54.6° N, 20° E) with the
Parus
digital ionosonde in standard sounding mode. The mean daily
foF2
values were used in the analysis. The results of spectral analysis based on continuous wavelet transform showed that, during all of the warmings that occurred in 2008–2010, the
foF2
time variations demonstrated the presence of wave processes with periods of approximately 5−6 days, as well as more extended processes with periods of ~10−13 and 23−30 days. These periods coincide with the characteristic periods of planetary waves observed in the mesosphere during sudden stratospheric warmings, while the 13- and 30-day periods can be conditioned by the influence of the Sun.</description><subject>Conditioning</subject><subject>Continuous wavelet transform</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>F 2 region</subject><subject>foF2</subject><subject>Geophysics/Geodesy</subject><subject>Ionosondes</subject><subject>Mesosphere</subject><subject>Planetary waves</subject><subject>Spectral analysis</subject><subject>Stratosphere</subject><subject>Stratospheric warming</subject><subject>Wave period</subject><subject>Wavelet analysis</subject><subject>Wavelet transforms</subject><issn>0016-7932</issn><issn>1555-645X</issn><issn>0016-7940</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2018</creationdate><recordtype>article</recordtype><sourceid>BENPR</sourceid><recordid>eNp1kMFKAzEQhoMoWKsP4C3geXUm2XSzR61WxYJCi_W2ZLtJSW2TmmwF38Czj-iTmFrBg3iaw3z_P_P_hBwjnCLy_GwEgL2i5AwlcAApd0gHhRBZLxdPu6SzWWeb_T45iHEOCRICO-T5YaGcblV4oxP1qumDDtY3kVpHjR8wOrZLTR9VsKq13kV6oaJuqHd0Yl2rA71UraIm-CW9UwvrrJsF1dBR-41vXFh65vP9gwHCIdkzahH10c_skvHgaty_yYb317f982E25dhrs7oA2dRlzusCdSmMKLEpGqhZLnPBjBG6EaJGrEHp0hgoeEpdS82nQslS8i452dqugn9Z69hWc78OLl2sGIg82aXsicItNQ0-xqBNtQp2mXqoEKpNpdWfSpOGbTUxsW6mw6_z_6Ivnz12uQ</recordid><startdate>20180501</startdate><enddate>20180501</enddate><creator>Koren’kov, Yu. 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S. ; Koren’kova, N. A. ; Leshchenko, V. S.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c316t-b708db943b71e95f591d7d0b248452ff5ed55b11b0ae9ff073321b8e3c5a8983</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2018</creationdate><topic>Conditioning</topic><topic>Continuous wavelet transform</topic><topic>Earth and Environmental Science</topic><topic>Earth Sciences</topic><topic>F 2 region</topic><topic>foF2</topic><topic>Geophysics/Geodesy</topic><topic>Ionosondes</topic><topic>Mesosphere</topic><topic>Planetary waves</topic><topic>Spectral analysis</topic><topic>Stratosphere</topic><topic>Stratospheric warming</topic><topic>Wave period</topic><topic>Wavelet analysis</topic><topic>Wavelet transforms</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Koren’kov, Yu. N.</creatorcontrib><creatorcontrib>Bessarab, F. S.</creatorcontrib><creatorcontrib>Koren’kova, N. A.</creatorcontrib><creatorcontrib>Leshchenko, V. 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N.</au><au>Bessarab, F. S.</au><au>Koren’kova, N. A.</au><au>Leshchenko, V. S.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Planetary Wave Periods in foF2 Time Variations Based on Winter Data from Kaliningrad Station in 2008−2010</atitle><jtitle>Geomagnetism and Aeronomy</jtitle><stitle>Geomagn. Aeron</stitle><date>2018-05-01</date><risdate>2018</risdate><volume>58</volume><issue>3</issue><spage>420</spage><epage>429</epage><pages>420-429</pages><issn>0016-7932</issn><eissn>1555-645X</eissn><eissn>0016-7940</eissn><abstract>The study presents the results of the analysis of the
F
2-layer critical frequency variations obtained for the winter periods of 2008–2010, during which sudden stratospheric warmings were observed. The data were obtained at Kaliningrad ionospheric station (54.6° N, 20° E) with the
Parus
digital ionosonde in standard sounding mode. The mean daily
foF2
values were used in the analysis. The results of spectral analysis based on continuous wavelet transform showed that, during all of the warmings that occurred in 2008–2010, the
foF2
time variations demonstrated the presence of wave processes with periods of approximately 5−6 days, as well as more extended processes with periods of ~10−13 and 23−30 days. These periods coincide with the characteristic periods of planetary waves observed in the mesosphere during sudden stratospheric warmings, while the 13- and 30-day periods can be conditioned by the influence of the Sun.</abstract><cop>Moscow</cop><pub>Pleiades Publishing</pub><doi>10.1134/S0016793218030088</doi><tpages>10</tpages></addata></record> |
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| subjects | Conditioning Continuous wavelet transform Earth and Environmental Science Earth Sciences F 2 region foF2 Geophysics/Geodesy Ionosondes Mesosphere Planetary waves Spectral analysis Stratosphere Stratospheric warming Wave period Wavelet analysis Wavelet transforms |
| title | Planetary Wave Periods in foF2 Time Variations Based on Winter Data from Kaliningrad Station in 2008−2010 |
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