Parametric acoustic antenna in the atmosphere
Abstract We consider the principles of development of a parametric antenna in the atmosphere. It is shown that to excite an infrasound at a frequency lower than 1 Hz in the atmosphere, one can use an acoustic system emitting simultaneously two waves whose frequencies differ by the infrasound frequen...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Mityakov, N. A. [verfasserIn] |
|---|
| Format: |
Artikel |
|---|---|
| Sprache: |
Englisch |
| Erschienen: |
2006 |
|---|
| Schlagwörter: |
|---|
| Anmerkung: |
© Springer Science+Business Media, Inc. 2006 |
|---|
| Übergeordnetes Werk: |
Enthalten in: Radiophysics and quantum electronics - Kluwer Academic Publishers-Consultants Bureau, 1969, 49(2006), 7 vom: Juli, Seite 514-519 |
|---|---|
| Übergeordnetes Werk: |
volume:49 ; year:2006 ; number:7 ; month:07 ; pages:514-519 |
| Links: |
|---|
| DOI / URN: |
10.1007/s11141-006-0084-3 |
|---|
| Katalog-ID: |
OLC2063580642 |
|---|
| LEADER | 01000caa a22002652 4500 | ||
|---|---|---|---|
| 001 | OLC2063580642 | ||
| 003 | DE-627 | ||
| 005 | 20230504021529.0 | ||
| 007 | tu | ||
| 008 | 200820s2006 xx ||||| 00| ||eng c | ||
| 024 | 7 | |a 10.1007/s11141-006-0084-3 |2 doi | |
| 035 | |a (DE-627)OLC2063580642 | ||
| 035 | |a (DE-He213)s11141-006-0084-3-p | ||
| 040 | |a DE-627 |b ger |c DE-627 |e rakwb | ||
| 041 | |a eng | ||
| 082 | 0 | 4 | |a 530 |a 620 |q VZ |
| 100 | 1 | |a Mityakov, N. A. |e verfasserin |4 aut | |
| 245 | 1 | 0 | |a Parametric acoustic antenna in the atmosphere |
| 264 | 1 | |c 2006 | |
| 336 | |a Text |b txt |2 rdacontent | ||
| 337 | |a ohne Hilfsmittel zu benutzen |b n |2 rdamedia | ||
| 338 | |a Band |b nc |2 rdacarrier | ||
| 500 | |a © Springer Science+Business Media, Inc. 2006 | ||
| 520 | |a Abstract We consider the principles of development of a parametric antenna in the atmosphere. It is shown that to excite an infrasound at a frequency lower than 1 Hz in the atmosphere, one can use an acoustic system emitting simultaneously two waves whose frequencies differ by the infrasound frequency. In the pump-wave frequency range 20–500 Hz, the main contribution to infrasound emission is given by the region located at altitudes from 30 to 75 km, in which the oscillatory velocity in the pump wave is maximum. We propose an algorithm for calculation of the infrasound amplitude in the E and F layers of the ionosphere. Realization of a parametric antenna in the atmosphere makes it possible to broaden the capabilities of experiments based on the modification of the ionosphere by an infrasound. | ||
| 650 | 4 | |a Mach Number | |
| 650 | 4 | |a Acoustic Wave | |
| 650 | 4 | |a Pump Wave | |
| 650 | 4 | |a Oscillatory Velocity | |
| 650 | 4 | |a Nonlinear Acoustics | |
| 773 | 0 | 8 | |i Enthalten in |t Radiophysics and quantum electronics |d Kluwer Academic Publishers-Consultants Bureau, 1969 |g 49(2006), 7 vom: Juli, Seite 514-519 |w (DE-627)130499560 |w (DE-600)760167-0 |w (DE-576)016080793 |x 0033-8443 |7 nnns |
| 773 | 1 | 8 | |g volume:49 |g year:2006 |g number:7 |g month:07 |g pages:514-519 |
| 856 | 4 | 1 | |u https://doi.org/10.1007/s11141-006-0084-3 |z lizenzpflichtig |3 Volltext |
| 912 | |a GBV_USEFLAG_A | ||
| 912 | |a SYSFLAG_A | ||
| 912 | |a GBV_OLC | ||
| 912 | |a SSG-OLC-TEC | ||
| 912 | |a SSG-OLC-PHY | ||
| 912 | |a SSG-OPC-AST | ||
| 912 | |a GBV_ILN_70 | ||
| 951 | |a AR | ||
| 952 | |d 49 |j 2006 |e 7 |c 07 |h 514-519 | ||
| author_variant |
n a m na nam |
|---|---|
| matchkey_str |
article:00338443:2006----::aaerccutcnenite |
| hierarchy_sort_str |
2006 |
| publishDate |
2006 |
| allfields |
10.1007/s11141-006-0084-3 doi (DE-627)OLC2063580642 (DE-He213)s11141-006-0084-3-p DE-627 ger DE-627 rakwb eng 530 620 VZ Mityakov, N. A. verfasserin aut Parametric acoustic antenna in the atmosphere 2006 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer Science+Business Media, Inc. 2006 Abstract We consider the principles of development of a parametric antenna in the atmosphere. It is shown that to excite an infrasound at a frequency lower than 1 Hz in the atmosphere, one can use an acoustic system emitting simultaneously two waves whose frequencies differ by the infrasound frequency. In the pump-wave frequency range 20–500 Hz, the main contribution to infrasound emission is given by the region located at altitudes from 30 to 75 km, in which the oscillatory velocity in the pump wave is maximum. We propose an algorithm for calculation of the infrasound amplitude in the E and F layers of the ionosphere. Realization of a parametric antenna in the atmosphere makes it possible to broaden the capabilities of experiments based on the modification of the ionosphere by an infrasound. Mach Number Acoustic Wave Pump Wave Oscillatory Velocity Nonlinear Acoustics Enthalten in Radiophysics and quantum electronics Kluwer Academic Publishers-Consultants Bureau, 1969 49(2006), 7 vom: Juli, Seite 514-519 (DE-627)130499560 (DE-600)760167-0 (DE-576)016080793 0033-8443 nnns volume:49 year:2006 number:7 month:07 pages:514-519 https://doi.org/10.1007/s11141-006-0084-3 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-TEC SSG-OLC-PHY SSG-OPC-AST GBV_ILN_70 AR 49 2006 7 07 514-519 |
| spelling |
10.1007/s11141-006-0084-3 doi (DE-627)OLC2063580642 (DE-He213)s11141-006-0084-3-p DE-627 ger DE-627 rakwb eng 530 620 VZ Mityakov, N. A. verfasserin aut Parametric acoustic antenna in the atmosphere 2006 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer Science+Business Media, Inc. 2006 Abstract We consider the principles of development of a parametric antenna in the atmosphere. It is shown that to excite an infrasound at a frequency lower than 1 Hz in the atmosphere, one can use an acoustic system emitting simultaneously two waves whose frequencies differ by the infrasound frequency. In the pump-wave frequency range 20–500 Hz, the main contribution to infrasound emission is given by the region located at altitudes from 30 to 75 km, in which the oscillatory velocity in the pump wave is maximum. We propose an algorithm for calculation of the infrasound amplitude in the E and F layers of the ionosphere. Realization of a parametric antenna in the atmosphere makes it possible to broaden the capabilities of experiments based on the modification of the ionosphere by an infrasound. Mach Number Acoustic Wave Pump Wave Oscillatory Velocity Nonlinear Acoustics Enthalten in Radiophysics and quantum electronics Kluwer Academic Publishers-Consultants Bureau, 1969 49(2006), 7 vom: Juli, Seite 514-519 (DE-627)130499560 (DE-600)760167-0 (DE-576)016080793 0033-8443 nnns volume:49 year:2006 number:7 month:07 pages:514-519 https://doi.org/10.1007/s11141-006-0084-3 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-TEC SSG-OLC-PHY SSG-OPC-AST GBV_ILN_70 AR 49 2006 7 07 514-519 |
| allfields_unstemmed |
10.1007/s11141-006-0084-3 doi (DE-627)OLC2063580642 (DE-He213)s11141-006-0084-3-p DE-627 ger DE-627 rakwb eng 530 620 VZ Mityakov, N. A. verfasserin aut Parametric acoustic antenna in the atmosphere 2006 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer Science+Business Media, Inc. 2006 Abstract We consider the principles of development of a parametric antenna in the atmosphere. It is shown that to excite an infrasound at a frequency lower than 1 Hz in the atmosphere, one can use an acoustic system emitting simultaneously two waves whose frequencies differ by the infrasound frequency. In the pump-wave frequency range 20–500 Hz, the main contribution to infrasound emission is given by the region located at altitudes from 30 to 75 km, in which the oscillatory velocity in the pump wave is maximum. We propose an algorithm for calculation of the infrasound amplitude in the E and F layers of the ionosphere. Realization of a parametric antenna in the atmosphere makes it possible to broaden the capabilities of experiments based on the modification of the ionosphere by an infrasound. Mach Number Acoustic Wave Pump Wave Oscillatory Velocity Nonlinear Acoustics Enthalten in Radiophysics and quantum electronics Kluwer Academic Publishers-Consultants Bureau, 1969 49(2006), 7 vom: Juli, Seite 514-519 (DE-627)130499560 (DE-600)760167-0 (DE-576)016080793 0033-8443 nnns volume:49 year:2006 number:7 month:07 pages:514-519 https://doi.org/10.1007/s11141-006-0084-3 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-TEC SSG-OLC-PHY SSG-OPC-AST GBV_ILN_70 AR 49 2006 7 07 514-519 |
| allfieldsGer |
10.1007/s11141-006-0084-3 doi (DE-627)OLC2063580642 (DE-He213)s11141-006-0084-3-p DE-627 ger DE-627 rakwb eng 530 620 VZ Mityakov, N. A. verfasserin aut Parametric acoustic antenna in the atmosphere 2006 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer Science+Business Media, Inc. 2006 Abstract We consider the principles of development of a parametric antenna in the atmosphere. It is shown that to excite an infrasound at a frequency lower than 1 Hz in the atmosphere, one can use an acoustic system emitting simultaneously two waves whose frequencies differ by the infrasound frequency. In the pump-wave frequency range 20–500 Hz, the main contribution to infrasound emission is given by the region located at altitudes from 30 to 75 km, in which the oscillatory velocity in the pump wave is maximum. We propose an algorithm for calculation of the infrasound amplitude in the E and F layers of the ionosphere. Realization of a parametric antenna in the atmosphere makes it possible to broaden the capabilities of experiments based on the modification of the ionosphere by an infrasound. Mach Number Acoustic Wave Pump Wave Oscillatory Velocity Nonlinear Acoustics Enthalten in Radiophysics and quantum electronics Kluwer Academic Publishers-Consultants Bureau, 1969 49(2006), 7 vom: Juli, Seite 514-519 (DE-627)130499560 (DE-600)760167-0 (DE-576)016080793 0033-8443 nnns volume:49 year:2006 number:7 month:07 pages:514-519 https://doi.org/10.1007/s11141-006-0084-3 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-TEC SSG-OLC-PHY SSG-OPC-AST GBV_ILN_70 AR 49 2006 7 07 514-519 |
| allfieldsSound |
10.1007/s11141-006-0084-3 doi (DE-627)OLC2063580642 (DE-He213)s11141-006-0084-3-p DE-627 ger DE-627 rakwb eng 530 620 VZ Mityakov, N. A. verfasserin aut Parametric acoustic antenna in the atmosphere 2006 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer Science+Business Media, Inc. 2006 Abstract We consider the principles of development of a parametric antenna in the atmosphere. It is shown that to excite an infrasound at a frequency lower than 1 Hz in the atmosphere, one can use an acoustic system emitting simultaneously two waves whose frequencies differ by the infrasound frequency. In the pump-wave frequency range 20–500 Hz, the main contribution to infrasound emission is given by the region located at altitudes from 30 to 75 km, in which the oscillatory velocity in the pump wave is maximum. We propose an algorithm for calculation of the infrasound amplitude in the E and F layers of the ionosphere. Realization of a parametric antenna in the atmosphere makes it possible to broaden the capabilities of experiments based on the modification of the ionosphere by an infrasound. Mach Number Acoustic Wave Pump Wave Oscillatory Velocity Nonlinear Acoustics Enthalten in Radiophysics and quantum electronics Kluwer Academic Publishers-Consultants Bureau, 1969 49(2006), 7 vom: Juli, Seite 514-519 (DE-627)130499560 (DE-600)760167-0 (DE-576)016080793 0033-8443 nnns volume:49 year:2006 number:7 month:07 pages:514-519 https://doi.org/10.1007/s11141-006-0084-3 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-TEC SSG-OLC-PHY SSG-OPC-AST GBV_ILN_70 AR 49 2006 7 07 514-519 |
| language |
English |
| source |
Enthalten in Radiophysics and quantum electronics 49(2006), 7 vom: Juli, Seite 514-519 volume:49 year:2006 number:7 month:07 pages:514-519 |
| sourceStr |
Enthalten in Radiophysics and quantum electronics 49(2006), 7 vom: Juli, Seite 514-519 volume:49 year:2006 number:7 month:07 pages:514-519 |
| format_phy_str_mv |
Article |
| institution |
findex.gbv.de |
| topic_facet |
Mach Number Acoustic Wave Pump Wave Oscillatory Velocity Nonlinear Acoustics |
| dewey-raw |
530 |
| isfreeaccess_bool |
false |
| container_title |
Radiophysics and quantum electronics |
| authorswithroles_txt_mv |
Mityakov, N. A. @@aut@@ |
| publishDateDaySort_date |
2006-07-01T00:00:00Z |
| hierarchy_top_id |
130499560 |
| dewey-sort |
3530 |
| id |
OLC2063580642 |
| language_de |
englisch |
| fullrecord |
<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a22002652 4500</leader><controlfield tag="001">OLC2063580642</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230504021529.0</controlfield><controlfield tag="007">tu</controlfield><controlfield tag="008">200820s2006 xx ||||| 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1007/s11141-006-0084-3</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)OLC2063580642</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-He213)s11141-006-0084-3-p</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-627</subfield><subfield code="b">ger</subfield><subfield code="c">DE-627</subfield><subfield code="e">rakwb</subfield></datafield><datafield tag="041" ind1=" " ind2=" "><subfield code="a">eng</subfield></datafield><datafield tag="082" ind1="0" ind2="4"><subfield code="a">530</subfield><subfield code="a">620</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Mityakov, N. A.</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Parametric acoustic antenna in the atmosphere</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2006</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">Text</subfield><subfield code="b">txt</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">ohne Hilfsmittel zu benutzen</subfield><subfield code="b">n</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Band</subfield><subfield code="b">nc</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="500" ind1=" " ind2=" "><subfield code="a">© Springer Science+Business Media, Inc. 2006</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Abstract We consider the principles of development of a parametric antenna in the atmosphere. It is shown that to excite an infrasound at a frequency lower than 1 Hz in the atmosphere, one can use an acoustic system emitting simultaneously two waves whose frequencies differ by the infrasound frequency. In the pump-wave frequency range 20–500 Hz, the main contribution to infrasound emission is given by the region located at altitudes from 30 to 75 km, in which the oscillatory velocity in the pump wave is maximum. We propose an algorithm for calculation of the infrasound amplitude in the E and F layers of the ionosphere. Realization of a parametric antenna in the atmosphere makes it possible to broaden the capabilities of experiments based on the modification of the ionosphere by an infrasound.</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Mach Number</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Acoustic Wave</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Pump Wave</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Oscillatory Velocity</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Nonlinear Acoustics</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="t">Radiophysics and quantum electronics</subfield><subfield code="d">Kluwer Academic Publishers-Consultants Bureau, 1969</subfield><subfield code="g">49(2006), 7 vom: Juli, Seite 514-519</subfield><subfield code="w">(DE-627)130499560</subfield><subfield code="w">(DE-600)760167-0</subfield><subfield code="w">(DE-576)016080793</subfield><subfield code="x">0033-8443</subfield><subfield code="7">nnns</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:49</subfield><subfield code="g">year:2006</subfield><subfield code="g">number:7</subfield><subfield code="g">month:07</subfield><subfield code="g">pages:514-519</subfield></datafield><datafield tag="856" ind1="4" ind2="1"><subfield code="u">https://doi.org/10.1007/s11141-006-0084-3</subfield><subfield code="z">lizenzpflichtig</subfield><subfield code="3">Volltext</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_USEFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SYSFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_OLC</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-TEC</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-PHY</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OPC-AST</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_70</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">49</subfield><subfield code="j">2006</subfield><subfield code="e">7</subfield><subfield code="c">07</subfield><subfield code="h">514-519</subfield></datafield></record></collection>
|
| author |
Mityakov, N. A. |
| spellingShingle |
Mityakov, N. A. ddc 530 misc Mach Number misc Acoustic Wave misc Pump Wave misc Oscillatory Velocity misc Nonlinear Acoustics Parametric acoustic antenna in the atmosphere |
| authorStr |
Mityakov, N. A. |
| ppnlink_with_tag_str_mv |
@@773@@(DE-627)130499560 |
| format |
Article |
| dewey-ones |
530 - Physics 620 - Engineering & allied operations |
| delete_txt_mv |
keep |
| author_role |
aut |
| collection |
OLC |
| remote_str |
false |
| illustrated |
Not Illustrated |
| issn |
0033-8443 |
| topic_title |
530 620 VZ Parametric acoustic antenna in the atmosphere Mach Number Acoustic Wave Pump Wave Oscillatory Velocity Nonlinear Acoustics |
| topic |
ddc 530 misc Mach Number misc Acoustic Wave misc Pump Wave misc Oscillatory Velocity misc Nonlinear Acoustics |
| topic_unstemmed |
ddc 530 misc Mach Number misc Acoustic Wave misc Pump Wave misc Oscillatory Velocity misc Nonlinear Acoustics |
| topic_browse |
ddc 530 misc Mach Number misc Acoustic Wave misc Pump Wave misc Oscillatory Velocity misc Nonlinear Acoustics |
| format_facet |
Aufsätze Gedruckte Aufsätze |
| format_main_str_mv |
Text Zeitschrift/Artikel |
| carriertype_str_mv |
nc |
| hierarchy_parent_title |
Radiophysics and quantum electronics |
| hierarchy_parent_id |
130499560 |
| dewey-tens |
530 - Physics 620 - Engineering |
| hierarchy_top_title |
Radiophysics and quantum electronics |
| isfreeaccess_txt |
false |
| familylinks_str_mv |
(DE-627)130499560 (DE-600)760167-0 (DE-576)016080793 |
| title |
Parametric acoustic antenna in the atmosphere |
| ctrlnum |
(DE-627)OLC2063580642 (DE-He213)s11141-006-0084-3-p |
| title_full |
Parametric acoustic antenna in the atmosphere |
| author_sort |
Mityakov, N. A. |
| journal |
Radiophysics and quantum electronics |
| journalStr |
Radiophysics and quantum electronics |
| lang_code |
eng |
| isOA_bool |
false |
| dewey-hundreds |
500 - Science 600 - Technology |
| recordtype |
marc |
| publishDateSort |
2006 |
| contenttype_str_mv |
txt |
| container_start_page |
514 |
| author_browse |
Mityakov, N. A. |
| container_volume |
49 |
| class |
530 620 VZ |
| format_se |
Aufsätze |
| author-letter |
Mityakov, N. A. |
| doi_str_mv |
10.1007/s11141-006-0084-3 |
| dewey-full |
530 620 |
| title_sort |
parametric acoustic antenna in the atmosphere |
| title_auth |
Parametric acoustic antenna in the atmosphere |
| abstract |
Abstract We consider the principles of development of a parametric antenna in the atmosphere. It is shown that to excite an infrasound at a frequency lower than 1 Hz in the atmosphere, one can use an acoustic system emitting simultaneously two waves whose frequencies differ by the infrasound frequency. In the pump-wave frequency range 20–500 Hz, the main contribution to infrasound emission is given by the region located at altitudes from 30 to 75 km, in which the oscillatory velocity in the pump wave is maximum. We propose an algorithm for calculation of the infrasound amplitude in the E and F layers of the ionosphere. Realization of a parametric antenna in the atmosphere makes it possible to broaden the capabilities of experiments based on the modification of the ionosphere by an infrasound. © Springer Science+Business Media, Inc. 2006 |
| abstractGer |
Abstract We consider the principles of development of a parametric antenna in the atmosphere. It is shown that to excite an infrasound at a frequency lower than 1 Hz in the atmosphere, one can use an acoustic system emitting simultaneously two waves whose frequencies differ by the infrasound frequency. In the pump-wave frequency range 20–500 Hz, the main contribution to infrasound emission is given by the region located at altitudes from 30 to 75 km, in which the oscillatory velocity in the pump wave is maximum. We propose an algorithm for calculation of the infrasound amplitude in the E and F layers of the ionosphere. Realization of a parametric antenna in the atmosphere makes it possible to broaden the capabilities of experiments based on the modification of the ionosphere by an infrasound. © Springer Science+Business Media, Inc. 2006 |
| abstract_unstemmed |
Abstract We consider the principles of development of a parametric antenna in the atmosphere. It is shown that to excite an infrasound at a frequency lower than 1 Hz in the atmosphere, one can use an acoustic system emitting simultaneously two waves whose frequencies differ by the infrasound frequency. In the pump-wave frequency range 20–500 Hz, the main contribution to infrasound emission is given by the region located at altitudes from 30 to 75 km, in which the oscillatory velocity in the pump wave is maximum. We propose an algorithm for calculation of the infrasound amplitude in the E and F layers of the ionosphere. Realization of a parametric antenna in the atmosphere makes it possible to broaden the capabilities of experiments based on the modification of the ionosphere by an infrasound. © Springer Science+Business Media, Inc. 2006 |
| collection_details |
GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-TEC SSG-OLC-PHY SSG-OPC-AST GBV_ILN_70 |
| container_issue |
7 |
| title_short |
Parametric acoustic antenna in the atmosphere |
| url |
https://doi.org/10.1007/s11141-006-0084-3 |
| remote_bool |
false |
| ppnlink |
130499560 |
| mediatype_str_mv |
n |
| isOA_txt |
false |
| hochschulschrift_bool |
false |
| doi_str |
10.1007/s11141-006-0084-3 |
| up_date |
2024-07-03T19:29:36.744Z |
| _version_ |
1803587395775365120 |
| fullrecord_marcxml |
<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a22002652 4500</leader><controlfield tag="001">OLC2063580642</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230504021529.0</controlfield><controlfield tag="007">tu</controlfield><controlfield tag="008">200820s2006 xx ||||| 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1007/s11141-006-0084-3</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)OLC2063580642</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-He213)s11141-006-0084-3-p</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-627</subfield><subfield code="b">ger</subfield><subfield code="c">DE-627</subfield><subfield code="e">rakwb</subfield></datafield><datafield tag="041" ind1=" " ind2=" "><subfield code="a">eng</subfield></datafield><datafield tag="082" ind1="0" ind2="4"><subfield code="a">530</subfield><subfield code="a">620</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Mityakov, N. A.</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Parametric acoustic antenna in the atmosphere</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2006</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">Text</subfield><subfield code="b">txt</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">ohne Hilfsmittel zu benutzen</subfield><subfield code="b">n</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Band</subfield><subfield code="b">nc</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="500" ind1=" " ind2=" "><subfield code="a">© Springer Science+Business Media, Inc. 2006</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Abstract We consider the principles of development of a parametric antenna in the atmosphere. It is shown that to excite an infrasound at a frequency lower than 1 Hz in the atmosphere, one can use an acoustic system emitting simultaneously two waves whose frequencies differ by the infrasound frequency. In the pump-wave frequency range 20–500 Hz, the main contribution to infrasound emission is given by the region located at altitudes from 30 to 75 km, in which the oscillatory velocity in the pump wave is maximum. We propose an algorithm for calculation of the infrasound amplitude in the E and F layers of the ionosphere. Realization of a parametric antenna in the atmosphere makes it possible to broaden the capabilities of experiments based on the modification of the ionosphere by an infrasound.</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Mach Number</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Acoustic Wave</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Pump Wave</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Oscillatory Velocity</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Nonlinear Acoustics</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="t">Radiophysics and quantum electronics</subfield><subfield code="d">Kluwer Academic Publishers-Consultants Bureau, 1969</subfield><subfield code="g">49(2006), 7 vom: Juli, Seite 514-519</subfield><subfield code="w">(DE-627)130499560</subfield><subfield code="w">(DE-600)760167-0</subfield><subfield code="w">(DE-576)016080793</subfield><subfield code="x">0033-8443</subfield><subfield code="7">nnns</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:49</subfield><subfield code="g">year:2006</subfield><subfield code="g">number:7</subfield><subfield code="g">month:07</subfield><subfield code="g">pages:514-519</subfield></datafield><datafield tag="856" ind1="4" ind2="1"><subfield code="u">https://doi.org/10.1007/s11141-006-0084-3</subfield><subfield code="z">lizenzpflichtig</subfield><subfield code="3">Volltext</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_USEFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SYSFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_OLC</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-TEC</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-PHY</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OPC-AST</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_70</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">49</subfield><subfield code="j">2006</subfield><subfield code="e">7</subfield><subfield code="c">07</subfield><subfield code="h">514-519</subfield></datafield></record></collection>
|
| score |
7.4013443 |