Wind regime peculiarities in the lower thermosphere in the winter of 1983/84
Temporal variations of prevailing winds at 90 to 100 km obtained from measurements carried out in winter 1983 to 1984 at three sites in the USSR and two sites in East Germany are reported. These variations are compared with those of the thermal stratospheric regime. Measurements were carried out usi...
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| creator | Lysenko, I. A. Makarov, N. A. Portnyagin, Yu. I. Petrov, B. I. Greisiger, K. M. Schminder, R. Kurschner, D. |
| description | Temporal variations of prevailing winds at 90 to 100 km obtained from measurements carried out in winter 1983 to 1984 at three sites in the USSR and two sites in East Germany are reported. These variations are compared with those of the thermal stratospheric regime. Measurements were carried out using the drifts D2 method (meteor wind radar) and the D1 method (ionospheric drifts). Temporal variations of zonal and meridional prevailing wind components for all the sites are given. Also presented are zonal wind data obtained using the partial reflection wind radar. Wind velocity values were obtained by averaging data recorded at between 105 and 91 km altitude. Wind velocity data averaged in such a way can be related to about the same height interval to which the data obtained by the meteor radar and ionospheric methods at other sites, i.e., the mean height of the meteor zone (about 95 km). The results presented show that there are significant fluctuations about the seasonal course of both zonal and meridional prevailing winds. |
| format | Conference Proceeding |
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I. ; Greisiger, K. M. ; Schminder, R. ; Kurschner, D.</creatorcontrib><description>Temporal variations of prevailing winds at 90 to 100 km obtained from measurements carried out in winter 1983 to 1984 at three sites in the USSR and two sites in East Germany are reported. These variations are compared with those of the thermal stratospheric regime. Measurements were carried out using the drifts D2 method (meteor wind radar) and the D1 method (ionospheric drifts). Temporal variations of zonal and meridional prevailing wind components for all the sites are given. Also presented are zonal wind data obtained using the partial reflection wind radar. Wind velocity values were obtained by averaging data recorded at between 105 and 91 km altitude. Wind velocity data averaged in such a way can be related to about the same height interval to which the data obtained by the meteor radar and ionospheric methods at other sites, i.e., the mean height of the meteor zone (about 95 km). The results presented show that there are significant fluctuations about the seasonal course of both zonal and meridional prevailing winds.</description><language>eng</language><publisher>Legacy CDMS</publisher><subject>Geophysics</subject><creationdate>1987</creationdate><rights>Copyright Determination: GOV_PUBLIC_USE_PERMITTED</rights><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>309,780,800</link.rule.ids><linktorsrc>$$Uhttps://ntrs.nasa.gov/citations/19880005129$$EView_record_in_NASA$$FView_record_in_$$GNASA$$Hfree_for_read</linktorsrc></links><search><creatorcontrib>Lysenko, I. A.</creatorcontrib><creatorcontrib>Makarov, N. A.</creatorcontrib><creatorcontrib>Portnyagin, Yu. I.</creatorcontrib><creatorcontrib>Petrov, B. I.</creatorcontrib><creatorcontrib>Greisiger, K. M.</creatorcontrib><creatorcontrib>Schminder, R.</creatorcontrib><creatorcontrib>Kurschner, D.</creatorcontrib><title>Wind regime peculiarities in the lower thermosphere in the winter of 1983/84</title><description>Temporal variations of prevailing winds at 90 to 100 km obtained from measurements carried out in winter 1983 to 1984 at three sites in the USSR and two sites in East Germany are reported. These variations are compared with those of the thermal stratospheric regime. Measurements were carried out using the drifts D2 method (meteor wind radar) and the D1 method (ionospheric drifts). Temporal variations of zonal and meridional prevailing wind components for all the sites are given. Also presented are zonal wind data obtained using the partial reflection wind radar. Wind velocity values were obtained by averaging data recorded at between 105 and 91 km altitude. Wind velocity data averaged in such a way can be related to about the same height interval to which the data obtained by the meteor radar and ionospheric methods at other sites, i.e., the mean height of the meteor zone (about 95 km). The results presented show that there are significant fluctuations about the seasonal course of both zonal and meridional prevailing winds.</description><subject>Geophysics</subject><fulltext>true</fulltext><rsrctype>conference_proceeding</rsrctype><creationdate>1987</creationdate><recordtype>conference_proceeding</recordtype><sourceid>CYI</sourceid><recordid>eNrjZPAJz8xLUShKTc_MTVUoSE0uzclMLMosyUwtVsjMUyjJSFXIyS9PLQKxinLziwuAVCpMpjwzrwQolZ-mYGhpYaxvYcLDwJqWmFOcyguluRlk3FxDnD108xKLE-PzSoqK44EqLQwMDEwNjSyNCUgDAPbGMGI</recordid><startdate>19870801</startdate><enddate>19870801</enddate><creator>Lysenko, I. A.</creator><creator>Makarov, N. A.</creator><creator>Portnyagin, Yu. I.</creator><creator>Petrov, B. I.</creator><creator>Greisiger, K. M.</creator><creator>Schminder, R.</creator><creator>Kurschner, D.</creator><scope>CYE</scope><scope>CYI</scope></search><sort><creationdate>19870801</creationdate><title>Wind regime peculiarities in the lower thermosphere in the winter of 1983/84</title><author>Lysenko, I. A. ; Makarov, N. A. ; Portnyagin, Yu. I. ; Petrov, B. I. ; Greisiger, K. M. ; Schminder, R. ; Kurschner, D.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-nasa_ntrs_198800051293</frbrgroupid><rsrctype>conference_proceedings</rsrctype><prefilter>conference_proceedings</prefilter><language>eng</language><creationdate>1987</creationdate><topic>Geophysics</topic><toplevel>online_resources</toplevel><creatorcontrib>Lysenko, I. A.</creatorcontrib><creatorcontrib>Makarov, N. A.</creatorcontrib><creatorcontrib>Portnyagin, Yu. I.</creatorcontrib><creatorcontrib>Petrov, B. I.</creatorcontrib><creatorcontrib>Greisiger, K. M.</creatorcontrib><creatorcontrib>Schminder, R.</creatorcontrib><creatorcontrib>Kurschner, D.</creatorcontrib><collection>NASA Scientific and Technical Information</collection><collection>NASA Technical Reports Server</collection></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext_linktorsrc</fulltext></delivery><addata><au>Lysenko, I. A.</au><au>Makarov, N. A.</au><au>Portnyagin, Yu. I.</au><au>Petrov, B. I.</au><au>Greisiger, K. M.</au><au>Schminder, R.</au><au>Kurschner, D.</au><format>book</format><genre>proceeding</genre><ristype>CONF</ristype><atitle>Wind regime peculiarities in the lower thermosphere in the winter of 1983/84</atitle><date>1987-08-01</date><risdate>1987</risdate><abstract>Temporal variations of prevailing winds at 90 to 100 km obtained from measurements carried out in winter 1983 to 1984 at three sites in the USSR and two sites in East Germany are reported. These variations are compared with those of the thermal stratospheric regime. Measurements were carried out using the drifts D2 method (meteor wind radar) and the D1 method (ionospheric drifts). Temporal variations of zonal and meridional prevailing wind components for all the sites are given. Also presented are zonal wind data obtained using the partial reflection wind radar. Wind velocity values were obtained by averaging data recorded at between 105 and 91 km altitude. Wind velocity data averaged in such a way can be related to about the same height interval to which the data obtained by the meteor radar and ionospheric methods at other sites, i.e., the mean height of the meteor zone (about 95 km). The results presented show that there are significant fluctuations about the seasonal course of both zonal and meridional prevailing winds.</abstract><cop>Legacy CDMS</cop><oa>free_for_read</oa></addata></record> |
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| title | Wind regime peculiarities in the lower thermosphere in the winter of 1983/84 |
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