Ozone content of the atmosphere. 3. Statistics of extreme values of the total ozone content in the midlatitude atmosphere
Abstract The occurrence frequency of extremely large and extremely small values of the total ozone content (TOC) for Irkutsk, Berlin, and Saskatoon midlatitude stations (located near 52°N but in different climatic zones) are calculated based on the daily satellite measurements in the 1978–2005 perio...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Vergasova, G. V. [verfasserIn] |
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| Format: |
Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2009 |
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| Schlagwörter: |
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| Anmerkung: |
© Pleiades Publishing, Ltd. 2009 |
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| Übergeordnetes Werk: |
Enthalten in: Geomagnetism and aeronomy - SP MAIK Nauka/Interperiodica, 1961, 49(2009), 7 vom: Dez., Seite 1050-1055 |
|---|---|
| Übergeordnetes Werk: |
volume:49 ; year:2009 ; number:7 ; month:12 ; pages:1050-1055 |
| Links: |
|---|
| DOI / URN: |
10.1134/S0016793209070342 |
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OLC207181844X |
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| 520 | |a Abstract The occurrence frequency of extremely large and extremely small values of the total ozone content (TOC) for Irkutsk, Berlin, and Saskatoon midlatitude stations (located near 52°N but in different climatic zones) are calculated based on the daily satellite measurements in the 1978–2005 period. The data for various seasons are presented. The interannual variability and regional differences are demonstrated. The results indicate that the TOC variability is mainly caused by natural atmospheric processes. | ||
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10.1134/S0016793209070342 doi (DE-627)OLC207181844X (DE-He213)S0016793209070342-p DE-627 ger DE-627 rakwb eng 550 VZ 16,13 ssgn Vergasova, G. V. verfasserin aut Ozone content of the atmosphere. 3. Statistics of extreme values of the total ozone content in the midlatitude atmosphere 2009 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Pleiades Publishing, Ltd. 2009 Abstract The occurrence frequency of extremely large and extremely small values of the total ozone content (TOC) for Irkutsk, Berlin, and Saskatoon midlatitude stations (located near 52°N but in different climatic zones) are calculated based on the daily satellite measurements in the 1978–2005 period. The data for various seasons are presented. The interannual variability and regional differences are demonstrated. The results indicate that the TOC variability is mainly caused by natural atmospheric processes. Ozone Spring Period Ozone Content Lower Thermosphere Total Ozone Content Kokourov, V. D. aut Kazimirovsky, E. S. aut Enthalten in Geomagnetism and aeronomy SP MAIK Nauka/Interperiodica, 1961 49(2009), 7 vom: Dez., Seite 1050-1055 (DE-627)129365564 (DE-600)161523-3 (DE-576)014739321 0016-7932 nnns volume:49 year:2009 number:7 month:12 pages:1050-1055 https://doi.org/10.1134/S0016793209070342 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GEO SSG-OPC-GGO GBV_ILN_40 GBV_ILN_70 AR 49 2009 7 12 1050-1055 |
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10.1134/S0016793209070342 doi (DE-627)OLC207181844X (DE-He213)S0016793209070342-p DE-627 ger DE-627 rakwb eng 550 VZ 16,13 ssgn Vergasova, G. V. verfasserin aut Ozone content of the atmosphere. 3. Statistics of extreme values of the total ozone content in the midlatitude atmosphere 2009 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Pleiades Publishing, Ltd. 2009 Abstract The occurrence frequency of extremely large and extremely small values of the total ozone content (TOC) for Irkutsk, Berlin, and Saskatoon midlatitude stations (located near 52°N but in different climatic zones) are calculated based on the daily satellite measurements in the 1978–2005 period. The data for various seasons are presented. The interannual variability and regional differences are demonstrated. The results indicate that the TOC variability is mainly caused by natural atmospheric processes. Ozone Spring Period Ozone Content Lower Thermosphere Total Ozone Content Kokourov, V. D. aut Kazimirovsky, E. S. aut Enthalten in Geomagnetism and aeronomy SP MAIK Nauka/Interperiodica, 1961 49(2009), 7 vom: Dez., Seite 1050-1055 (DE-627)129365564 (DE-600)161523-3 (DE-576)014739321 0016-7932 nnns volume:49 year:2009 number:7 month:12 pages:1050-1055 https://doi.org/10.1134/S0016793209070342 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GEO SSG-OPC-GGO GBV_ILN_40 GBV_ILN_70 AR 49 2009 7 12 1050-1055 |
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10.1134/S0016793209070342 doi (DE-627)OLC207181844X (DE-He213)S0016793209070342-p DE-627 ger DE-627 rakwb eng 550 VZ 16,13 ssgn Vergasova, G. V. verfasserin aut Ozone content of the atmosphere. 3. Statistics of extreme values of the total ozone content in the midlatitude atmosphere 2009 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Pleiades Publishing, Ltd. 2009 Abstract The occurrence frequency of extremely large and extremely small values of the total ozone content (TOC) for Irkutsk, Berlin, and Saskatoon midlatitude stations (located near 52°N but in different climatic zones) are calculated based on the daily satellite measurements in the 1978–2005 period. The data for various seasons are presented. The interannual variability and regional differences are demonstrated. The results indicate that the TOC variability is mainly caused by natural atmospheric processes. Ozone Spring Period Ozone Content Lower Thermosphere Total Ozone Content Kokourov, V. D. aut Kazimirovsky, E. S. aut Enthalten in Geomagnetism and aeronomy SP MAIK Nauka/Interperiodica, 1961 49(2009), 7 vom: Dez., Seite 1050-1055 (DE-627)129365564 (DE-600)161523-3 (DE-576)014739321 0016-7932 nnns volume:49 year:2009 number:7 month:12 pages:1050-1055 https://doi.org/10.1134/S0016793209070342 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GEO SSG-OPC-GGO GBV_ILN_40 GBV_ILN_70 AR 49 2009 7 12 1050-1055 |
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10.1134/S0016793209070342 doi (DE-627)OLC207181844X (DE-He213)S0016793209070342-p DE-627 ger DE-627 rakwb eng 550 VZ 16,13 ssgn Vergasova, G. V. verfasserin aut Ozone content of the atmosphere. 3. Statistics of extreme values of the total ozone content in the midlatitude atmosphere 2009 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Pleiades Publishing, Ltd. 2009 Abstract The occurrence frequency of extremely large and extremely small values of the total ozone content (TOC) for Irkutsk, Berlin, and Saskatoon midlatitude stations (located near 52°N but in different climatic zones) are calculated based on the daily satellite measurements in the 1978–2005 period. The data for various seasons are presented. The interannual variability and regional differences are demonstrated. The results indicate that the TOC variability is mainly caused by natural atmospheric processes. Ozone Spring Period Ozone Content Lower Thermosphere Total Ozone Content Kokourov, V. D. aut Kazimirovsky, E. S. aut Enthalten in Geomagnetism and aeronomy SP MAIK Nauka/Interperiodica, 1961 49(2009), 7 vom: Dez., Seite 1050-1055 (DE-627)129365564 (DE-600)161523-3 (DE-576)014739321 0016-7932 nnns volume:49 year:2009 number:7 month:12 pages:1050-1055 https://doi.org/10.1134/S0016793209070342 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GEO SSG-OPC-GGO GBV_ILN_40 GBV_ILN_70 AR 49 2009 7 12 1050-1055 |
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Abstract The occurrence frequency of extremely large and extremely small values of the total ozone content (TOC) for Irkutsk, Berlin, and Saskatoon midlatitude stations (located near 52°N but in different climatic zones) are calculated based on the daily satellite measurements in the 1978–2005 period. The data for various seasons are presented. The interannual variability and regional differences are demonstrated. The results indicate that the TOC variability is mainly caused by natural atmospheric processes. © Pleiades Publishing, Ltd. 2009 |
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Abstract The occurrence frequency of extremely large and extremely small values of the total ozone content (TOC) for Irkutsk, Berlin, and Saskatoon midlatitude stations (located near 52°N but in different climatic zones) are calculated based on the daily satellite measurements in the 1978–2005 period. The data for various seasons are presented. The interannual variability and regional differences are demonstrated. The results indicate that the TOC variability is mainly caused by natural atmospheric processes. © Pleiades Publishing, Ltd. 2009 |
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Abstract The occurrence frequency of extremely large and extremely small values of the total ozone content (TOC) for Irkutsk, Berlin, and Saskatoon midlatitude stations (located near 52°N but in different climatic zones) are calculated based on the daily satellite measurements in the 1978–2005 period. The data for various seasons are presented. The interannual variability and regional differences are demonstrated. The results indicate that the TOC variability is mainly caused by natural atmospheric processes. © Pleiades Publishing, Ltd. 2009 |
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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">OLC207181844X</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230401080516.0</controlfield><controlfield tag="007">tu</controlfield><controlfield tag="008">200819s2009 xx ||||| 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1134/S0016793209070342</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)OLC207181844X</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-He213)S0016793209070342-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">550</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">16,13</subfield><subfield code="2">ssgn</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Vergasova, G. V.</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Ozone content of the atmosphere. 3. Statistics of extreme values of the total ozone content in the midlatitude atmosphere</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2009</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">© Pleiades Publishing, Ltd. 2009</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Abstract The occurrence frequency of extremely large and extremely small values of the total ozone content (TOC) for Irkutsk, Berlin, and Saskatoon midlatitude stations (located near 52°N but in different climatic zones) are calculated based on the daily satellite measurements in the 1978–2005 period. The data for various seasons are presented. The interannual variability and regional differences are demonstrated. The results indicate that the TOC variability is mainly caused by natural atmospheric processes.</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Ozone</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Spring Period</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Ozone Content</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Lower Thermosphere</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Total Ozone Content</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Kokourov, V. D.</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Kazimirovsky, E. S.</subfield><subfield code="4">aut</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="t">Geomagnetism and aeronomy</subfield><subfield code="d">SP MAIK Nauka/Interperiodica, 1961</subfield><subfield code="g">49(2009), 7 vom: Dez., Seite 1050-1055</subfield><subfield code="w">(DE-627)129365564</subfield><subfield code="w">(DE-600)161523-3</subfield><subfield code="w">(DE-576)014739321</subfield><subfield code="x">0016-7932</subfield><subfield code="7">nnns</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:49</subfield><subfield code="g">year:2009</subfield><subfield code="g">number:7</subfield><subfield code="g">month:12</subfield><subfield code="g">pages:1050-1055</subfield></datafield><datafield tag="856" ind1="4" ind2="1"><subfield code="u">https://doi.org/10.1134/S0016793209070342</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-GEO</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OPC-GEO</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OPC-GGO</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_40</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">2009</subfield><subfield code="e">7</subfield><subfield code="c">12</subfield><subfield code="h">1050-1055</subfield></datafield></record></collection>
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