The cross correlation method response prior to earthquakes using foF2 data from various ionospheric stations
Considering the non-systematic aspect in detection of seismo-ionospheric precursors; we propose an attempt to characterize the nature of the perturbations in the F2 ionospheric layer prior to earthquakes using cross-correlation method. The effectiveness of cross-correlation method is not questioned;...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Benghanem, K. [verfasserIn] |
|---|
| Format: |
E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2019 |
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| Schlagwörter: |
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| Umfang: |
21 |
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| Übergeordnetes Werk: |
Enthalten in: Posttranscriptional actions of triiodothyronine on - Bargi-Souza, Paula ELSEVIER, 2018, including COSPAR information bulletin : the official journal of the Committee on Space Research (COSPAR), a scientific committee of the International Council of Scientific Unions (ICSU), Amsterdam [u.a.] |
|---|---|
| Übergeordnetes Werk: |
volume:63 ; year:2019 ; number:8 ; day:15 ; month:04 ; pages:2638-2658 ; extent:21 |
| Links: |
|---|
| DOI / URN: |
10.1016/j.asr.2019.01.016 |
|---|
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ELV046094652 |
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| 520 | |a Considering the non-systematic aspect in detection of seismo-ionospheric precursors; we propose an attempt to characterize the nature of the perturbations in the F2 ionospheric layer prior to earthquakes using cross-correlation method. The effectiveness of cross-correlation method is not questioned; but could the use of more than two observation points undergoing identical influence of solar activity reveal the same perturbations for the same earthquake? | ||
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Considering the non-systematic aspect in detection of seismo-ionospheric precursors; we propose an attempt to characterize the nature of the perturbations in the F2 ionospheric layer prior to earthquakes using cross-correlation method. The effectiveness of cross-correlation method is not questioned; but could the use of more than two observation points undergoing identical influence of solar activity reveal the same perturbations for the same earthquake? |
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Considering the non-systematic aspect in detection of seismo-ionospheric precursors; we propose an attempt to characterize the nature of the perturbations in the F2 ionospheric layer prior to earthquakes using cross-correlation method. The effectiveness of cross-correlation method is not questioned; but could the use of more than two observation points undergoing identical influence of solar activity reveal the same perturbations for the same earthquake? |
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Considering the non-systematic aspect in detection of seismo-ionospheric precursors; we propose an attempt to characterize the nature of the perturbations in the F2 ionospheric layer prior to earthquakes using cross-correlation method. The effectiveness of cross-correlation method is not questioned; but could the use of more than two observation points undergoing identical influence of solar activity reveal the same perturbations for the same earthquake? |
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The cross correlation method response prior to earthquakes using foF2 data from various ionospheric stations |
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<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a22002652 4500</leader><controlfield tag="001">ELV046094652</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230624121647.0</controlfield><controlfield tag="007">cr uuu---uuuuu</controlfield><controlfield tag="008">191021s2019 xx |||||o 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1016/j.asr.2019.01.016</subfield><subfield code="2">doi</subfield></datafield><datafield tag="028" ind1="5" ind2="2"><subfield code="a">GBV00000000000682.pica</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)ELV046094652</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(ELSEVIER)S0273-1177(19)30024-9</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">610</subfield><subfield code="a">570</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">44.89</subfield><subfield code="2">bkl</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Benghanem, K.</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="4"><subfield code="a">The cross correlation method response prior to earthquakes using foF2 data from various ionospheric stations</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2019</subfield></datafield><datafield tag="300" ind1=" " ind2=" "><subfield code="a">21</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">nicht spezifiziert</subfield><subfield code="b">zzz</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">nicht spezifiziert</subfield><subfield code="b">z</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">nicht spezifiziert</subfield><subfield code="b">zu</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Considering the non-systematic aspect in detection of seismo-ionospheric precursors; we propose an attempt to characterize the nature of the perturbations in the F2 ionospheric layer prior to earthquakes using cross-correlation method. 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