Lower ionosphere at middle latitudes: its morphology and response to meteorological and solar-terrestrial activity during the DYANA campaign 1990
Identifieur interne : 002C86 ( Main/Exploration ); précédent : 002C85; suivant : 002C87Lower ionosphere at middle latitudes: its morphology and response to meteorological and solar-terrestrial activity during the DYANA campaign 1990
Auteurs : J. Laštovi Ka [République tchèque] ; L. F. Alberca [Espagne] ; E. A. Benediktov [Russie] ; J. Boška [République tchèque] ; J. Bremer [Allemagne] ; G. Entzian [Allemagne] ; V. Fišer [République tchèque] ; J.-C. Jodogne [Belgique] ; A. K. Knyazev [Russie] ; F. Marcz [Hongrie] ; B. A. De La Morena [Espagne] ; Pl. Mukhtarov [Bulgarie] ; T. Ogawa [Japon] ; D. Pancheva [Bulgarie] ; H. Ranta [Finlande] ; Z. Ts. Rapoport [Russie] ; Xiong Nianlu [République populaire de Chine]Source :
- Journal of Atmospheric and Terrestrial Physics [ 0021-9169 ] ; 1993.
Abstract
A large number of radio wave absorption, ƒmin, and IPHA data measured in Europe and East Asia are investigated over the DYANA campaign period (1 January–31 March 1990) from the point of view of their response to meteorological and solar/geomagnetic forcing, of winter anomaly, and of a brief description of the state of the lower ionosphere on rocket salvo days. European mid-latitudinal measurements of electron density are briefly mentioned.The meteorological/solar control of the mid-latitudinal lower ionosphere during DYANA is considerably weaker than during MAP/WINE (winter 1983/84), but is evidently stronger than during MAP/SINE (summer 1987). The most distinct feature of the DYANA winter is a quite different response of the mid-latitudinal lower ionosphere to meteorological variability (namely to the 10 hPa North Pole temperature— indirect characteristics of a global state of the polar vortex) in the first and second halves of the DYANA period. The winter anomaly displays an expected magnitude and pattern during the DYANA winter. There is an expected weaker response of the lower ionosphere to the strong minor stratospheric warming of the first half of February. All three rocket salvos at Biscarosse (CEL) were carried out when the state of the lower ionosphere was within the range of normal (non-extremal) conditions. Various rocket salvos at Andoya took place on days of considerably different conditions in the lower ionosphere at higher mid-latitudes. Partial reflection measurements at Nizhny Novgorod show a clear tendency to a decrease of the electron density gradient between 70 and 80 km during March 1990.
Url:
DOI: 10.1016/0021-9169(94)90021-3
Affiliations:
- Allemagne, Belgique, Bulgarie, Espagne, Finlande, Hongrie, Japon, Russie, République populaire de Chine, République tchèque
- Andalousie, Catalogne, Sofia-ville (oblast)
- Sofia
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Ranta</name><affiliation wicri:level="1"><country xml:lang="fr">Finlande</country><wicri:regionArea>Geophysical Observatory, SF-99600 Sodankylä</wicri:regionArea><wicri:noRegion>SF-99600 Sodankylä</wicri:noRegion></affiliation></author><author><name sortKey="Rapoport, Z Ts" sort="Rapoport, Z Ts" uniqKey="Rapoport Z" first="Z. Ts." last="Rapoport">Z. Ts. Rapoport</name><affiliation wicri:level="1"><country xml:lang="fr">Russie</country><wicri:regionArea>IZMIRAN, 142092 Troitsk, Moscow region</wicri:regionArea><wicri:noRegion>Moscow region</wicri:noRegion></affiliation></author><author><name sortKey="Nianlu, Xiong" sort="Nianlu, Xiong" uniqKey="Nianlu X" first="Xiong" last="Nianlu">Xiong Nianlu</name><affiliation wicri:level="1"><country xml:lang="fr">République populaire de Chine</country><wicri:regionArea>Wuhan Institute of Physics, Academia Sinica, P.O. Box 72003 Wuchang, Wuhan 430072</wicri:regionArea><wicri:noRegion>Wuhan 430072</wicri:noRegion></affiliation></author></analytic><monogr></monogr><series><title level="j">Journal of Atmospheric and Terrestrial Physics</title><title level="j" type="abbrev">ATPO</title><idno type="ISSN">0021-9169</idno><imprint><publisher>ELSEVIER</publisher><date type="published" when="1993">1993</date><biblScope unit="volume">56</biblScope><biblScope unit="issue">13–14</biblScope><biblScope unit="page" from="1947">1947</biblScope><biblScope unit="page" to="1962">1962</biblScope></imprint><idno type="ISSN">0021-9169</idno></series><idno type="istex">F6B3B34940AA796192B675C1D428E9739880BBDB</idno><idno type="DOI">10.1016/0021-9169(94)90021-3</idno><idno type="PII">0021-9169(94)90021-3</idno></biblStruct></sourceDesc><seriesStmt><idno type="ISSN">0021-9169</idno></seriesStmt></fileDesc><profileDesc><textClass></textClass><langUsage><language ident="en">en</language></langUsage></profileDesc></teiHeader><front><div type="abstract" xml:lang="en">A large number of radio wave absorption, ƒmin, and IPHA data measured in Europe and East Asia are investigated over the DYANA campaign period (1 January–31 March 1990) from the point of view of their response to meteorological and solar/geomagnetic forcing, of winter anomaly, and of a brief description of the state of the lower ionosphere on rocket salvo days. European mid-latitudinal measurements of electron density are briefly mentioned.The meteorological/solar control of the mid-latitudinal lower ionosphere during DYANA is considerably weaker than during MAP/WINE (winter 1983/84), but is evidently stronger than during MAP/SINE (summer 1987). The most distinct feature of the DYANA winter is a quite different response of the mid-latitudinal lower ionosphere to meteorological variability (namely to the 10 hPa North Pole temperature— indirect characteristics of a global state of the polar vortex) in the first and second halves of the DYANA period. The winter anomaly displays an expected magnitude and pattern during the DYANA winter. There is an expected weaker response of the lower ionosphere to the strong minor stratospheric warming of the first half of February. All three rocket salvos at Biscarosse (CEL) were carried out when the state of the lower ionosphere was within the range of normal (non-extremal) conditions. Various rocket salvos at Andoya took place on days of considerably different conditions in the lower ionosphere at higher mid-latitudes. Partial reflection measurements at Nizhny Novgorod show a clear tendency to a decrease of the electron density gradient between 70 and 80 km during March 1990.</div></front></TEI><affiliations><list><country><li>Allemagne</li><li>Belgique</li><li>Bulgarie</li><li>Espagne</li><li>Finlande</li><li>Hongrie</li><li>Japon</li><li>Russie</li><li>République populaire de Chine</li><li>République tchèque</li></country><region><li>Andalousie</li><li>Catalogne</li><li>Sofia-ville (oblast)</li></region><settlement><li>Sofia</li></settlement></list><tree><country name="République tchèque"><noRegion><name sortKey="Lastovi Ka, J" sort="Lastovi Ka, J" uniqKey="Lastovi Ka J" first="J." last="Laštovi Ka">J. Laštovi Ka</name></noRegion><name sortKey="Boska, J" sort="Boska, J" uniqKey="Boska J" first="J." last="Boška">J. Boška</name><name sortKey="Fiser, V" sort="Fiser, V" uniqKey="Fiser V" first="V." last="Fišer">V. Fišer</name></country><country name="Espagne"><region name="Catalogne"><name sortKey="Alberca, L F" sort="Alberca, L F" uniqKey="Alberca L" first="L. F." last="Alberca">L. F. Alberca</name></region><name sortKey="De La Morena, B A" sort="De La Morena, B A" uniqKey="De La Morena B" first="B. A." last="De La Morena">B. A. De La Morena</name></country><country name="Russie"><noRegion><name sortKey="Benediktov, E A" sort="Benediktov, E A" uniqKey="Benediktov E" first="E. A." last="Benediktov">E. A. Benediktov</name></noRegion><name sortKey="Knyazev, A K" sort="Knyazev, A K" uniqKey="Knyazev A" first="A. K." last="Knyazev">A. K. Knyazev</name><name sortKey="Rapoport, Z Ts" sort="Rapoport, Z Ts" uniqKey="Rapoport Z" first="Z. Ts." last="Rapoport">Z. Ts. Rapoport</name></country><country name="Allemagne"><noRegion><name sortKey="Bremer, J" sort="Bremer, J" uniqKey="Bremer J" first="J." last="Bremer">J. Bremer</name></noRegion><name sortKey="Entzian, G" sort="Entzian, G" uniqKey="Entzian G" first="G." last="Entzian">G. Entzian</name></country><country name="Belgique"><noRegion><name sortKey="Jodogne, J C" sort="Jodogne, J C" uniqKey="Jodogne J" first="J.-C." last="Jodogne">J.-C. Jodogne</name></noRegion></country><country name="Hongrie"><noRegion><name sortKey="Marcz, F" sort="Marcz, F" uniqKey="Marcz F" first="F." last="Marcz">F. Marcz</name></noRegion></country><country name="Bulgarie"><region name="Sofia-ville (oblast)"><name sortKey="Mukhtarov, Pl" sort="Mukhtarov, Pl" uniqKey="Mukhtarov P" first="Pl." last="Mukhtarov">Pl. Mukhtarov</name></region><name sortKey="Pancheva, D" sort="Pancheva, D" uniqKey="Pancheva D" first="D." last="Pancheva">D. Pancheva</name></country><country name="Japon"><noRegion><name sortKey="Ogawa, T" sort="Ogawa, T" uniqKey="Ogawa T" first="T." last="Ogawa">T. Ogawa</name></noRegion></country><country name="Finlande"><noRegion><name sortKey="Ranta, H" sort="Ranta, H" uniqKey="Ranta H" first="H." last="Ranta">H. Ranta</name></noRegion></country><country name="République populaire de Chine"><noRegion><name sortKey="Nianlu, Xiong" sort="Nianlu, Xiong" uniqKey="Nianlu X" first="Xiong" last="Nianlu">Xiong Nianlu</name></noRegion></country></tree></affiliations></record>Pour manipuler ce document sous Unix (Dilib)
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