Relationship between TEC jumps and auroral substorm in the high-latitude ionosphere
The influence of an auroral substorm on the total electron content (TEC) jumps and cycle slips on Global Positioning System (GPS) at high-latitudes is studied. For the first time, optical data from the all-sky imager, as well as interplanetary magnetic field and magnetometer data are used to complet...
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| Published in | Scientific reports Vol. 10; no. 1; p. 6363 |
|---|---|
| Main Authors | , , , |
| Format | Journal Article |
| Language | English |
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London
Nature Publishing Group UK
14.04.2020
Nature Publishing Group |
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| Online Access | Get full text |
| ISSN | 2045-2322 2045-2322 |
| DOI | 10.1038/s41598-020-63422-9 |
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| Abstract | The influence of an auroral substorm on the total electron content (TEC) jumps and cycle slips on Global Positioning System (GPS) at high-latitudes is studied. For the first time, optical data from the all-sky imager, as well as interplanetary magnetic field and magnetometer data are used to complete the analysis of the slips occurrence and to monitor the substorm evolution. Two types of slips are considered: (i) instrumental slips including losses in the measured phase of the GPS signal and (ii) sharp TEC variations (TEC jumps) It is demonstrated that the jumps in TEC determined from the GPS signals are mainly related to the auroral particle precipitation that normally occurs during geomagnetic substorms in the polar ionosphere. The GPS frequency
L
2
is consistently subject to more slips than frequency
L
1
both for quiet and disturbed conditions. The probability of TEC jumps is higher than for cycle slips in phase at frequencies
L
1
and
L
2
. The maximum of TEC jumps is observed during the recovery phase of the auroral substorm. Our findings are based on a data set obtained for a particular event. A generalization of the obtained numerical estimates to other events requires additional research and further analysis. |
|---|---|
| AbstractList | The influence of an auroral substorm on the total electron content (TEC) jumps and cycle slips on Global Positioning System (GPS) at high-latitudes is studied. For the first time, optical data from the all-sky imager, as well as interplanetary magnetic field and magnetometer data are used to complete the analysis of the slips occurrence and to monitor the substorm evolution. Two types of slips are considered: (i) instrumental slips including losses in the measured phase of the GPS signal and (ii) sharp TEC variations (TEC jumps) It is demonstrated that the jumps in TEC determined from the GPS signals are mainly related to the auroral particle precipitation that normally occurs during geomagnetic substorms in the polar ionosphere. The GPS frequency
L
2
is consistently subject to more slips than frequency
L
1
both for quiet and disturbed conditions. The probability of TEC jumps is higher than for cycle slips in phase at frequencies
L
1
and
L
2
. The maximum of TEC jumps is observed during the recovery phase of the auroral substorm. Our findings are based on a data set obtained for a particular event. A generalization of the obtained numerical estimates to other events requires additional research and further analysis. The influence of an auroral substorm on the total electron content (TEC) jumps and cycle slips on Global Positioning System (GPS) at high-latitudes is studied. For the first time, optical data from the all-sky imager, as well as interplanetary magnetic field and magnetometer data are used to complete the analysis of the slips occurrence and to monitor the substorm evolution. Two types of slips are considered: (i) instrumental slips including losses in the measured phase of the GPS signal and (ii) sharp TEC variations (TEC jumps) It is demonstrated that the jumps in TEC determined from the GPS signals are mainly related to the auroral particle precipitation that normally occurs during geomagnetic substorms in the polar ionosphere. The GPS frequency [Formula: see text] is consistently subject to more slips than frequency [Formula: see text] both for quiet and disturbed conditions. The probability of TEC jumps is higher than for cycle slips in phase at frequencies [Formula: see text] and [Formula: see text]. The maximum of TEC jumps is observed during the recovery phase of the auroral substorm. Our findings are based on a data set obtained for a particular event. A generalization of the obtained numerical estimates to other events requires additional research and further analysis. The influence of an auroral substorm on the total electron content (TEC) jumps and cycle slips on Global Positioning System (GPS) at high-latitudes is studied. For the first time, optical data from the all-sky imager, as well as interplanetary magnetic field and magnetometer data are used to complete the analysis of the slips occurrence and to monitor the substorm evolution. Two types of slips are considered: (i) instrumental slips including losses in the measured phase of the GPS signal and (ii) sharp TEC variations (TEC jumps) It is demonstrated that the jumps in TEC determined from the GPS signals are mainly related to the auroral particle precipitation that normally occurs during geomagnetic substorms in the polar ionosphere. The GPS frequency $${L}_{2}$$ L 2 is consistently subject to more slips than frequency $${L}_{1}$$ L 1 both for quiet and disturbed conditions. The probability of TEC jumps is higher than for cycle slips in phase at frequencies $${L}_{1}$$ L 1 and $${L}_{2}$$ L 2 . The maximum of TEC jumps is observed during the recovery phase of the auroral substorm. Our findings are based on a data set obtained for a particular event. A generalization of the obtained numerical estimates to other events requires additional research and further analysis. The influence of an auroral substorm on the total electron content (TEC) jumps and cycle slips on Global Positioning System (GPS) at high-latitudes is studied. For the first time, optical data from the all-sky imager, as well as interplanetary magnetic field and magnetometer data are used to complete the analysis of the slips occurrence and to monitor the substorm evolution. Two types of slips are considered: (i) instrumental slips including losses in the measured phase of the GPS signal and (ii) sharp TEC variations (TEC jumps) It is demonstrated that the jumps in TEC determined from the GPS signals are mainly related to the auroral particle precipitation that normally occurs during geomagnetic substorms in the polar ionosphere. The GPS frequency L2 is consistently subject to more slips than frequency L1 both for quiet and disturbed conditions. The probability of TEC jumps is higher than for cycle slips in phase at frequencies L1 and L2. The maximum of TEC jumps is observed during the recovery phase of the auroral substorm. Our findings are based on a data set obtained for a particular event. A generalization of the obtained numerical estimates to other events requires additional research and further analysis. The influence of an auroral substorm on the total electron content (TEC) jumps and cycle slips on Global Positioning System (GPS) at high-latitudes is studied. For the first time, optical data from the all-sky imager, as well as interplanetary magnetic field and magnetometer data are used to complete the analysis of the slips occurrence and to monitor the substorm evolution. Two types of slips are considered: (i) instrumental slips including losses in the measured phase of the GPS signal and (ii) sharp TEC variations (TEC jumps) It is demonstrated that the jumps in TEC determined from the GPS signals are mainly related to the auroral particle precipitation that normally occurs during geomagnetic substorms in the polar ionosphere. The GPS frequency [Formula: see text] is consistently subject to more slips than frequency [Formula: see text] both for quiet and disturbed conditions. The probability of TEC jumps is higher than for cycle slips in phase at frequencies [Formula: see text] and [Formula: see text]. The maximum of TEC jumps is observed during the recovery phase of the auroral substorm. Our findings are based on a data set obtained for a particular event. A generalization of the obtained numerical estimates to other events requires additional research and further analysis.The influence of an auroral substorm on the total electron content (TEC) jumps and cycle slips on Global Positioning System (GPS) at high-latitudes is studied. For the first time, optical data from the all-sky imager, as well as interplanetary magnetic field and magnetometer data are used to complete the analysis of the slips occurrence and to monitor the substorm evolution. Two types of slips are considered: (i) instrumental slips including losses in the measured phase of the GPS signal and (ii) sharp TEC variations (TEC jumps) It is demonstrated that the jumps in TEC determined from the GPS signals are mainly related to the auroral particle precipitation that normally occurs during geomagnetic substorms in the polar ionosphere. The GPS frequency [Formula: see text] is consistently subject to more slips than frequency [Formula: see text] both for quiet and disturbed conditions. The probability of TEC jumps is higher than for cycle slips in phase at frequencies [Formula: see text] and [Formula: see text]. The maximum of TEC jumps is observed during the recovery phase of the auroral substorm. Our findings are based on a data set obtained for a particular event. A generalization of the obtained numerical estimates to other events requires additional research and further analysis. The influence of an auroral substorm on the total electron content (TEC) jumps and cycle slips on Global Positioning System (GPS) at high-latitudes is studied. For the first time, optical data from the all-sky imager, as well as interplanetary magnetic field and magnetometer data are used to complete the analysis of the slips occurrence and to monitor the substorm evolution. Two types of slips are considered: (i) instrumental slips including losses in the measured phase of the GPS signal and (ii) sharp TEC variations (TEC jumps) It is demonstrated that the jumps in TEC determined from the GPS signals are mainly related to the auroral particle precipitation that normally occurs during geomagnetic substorms in the polar ionosphere. The GPS frequency $${L}_{2}$$ L2 is consistently subject to more slips than frequency $${L}_{1}$$ L1 both for quiet and disturbed conditions. The probability of TEC jumps is higher than for cycle slips in phase at frequencies $${L}_{1}$$ L1 and $${L}_{2}$$ L2. The maximum of TEC jumps is observed during the recovery phase of the auroral substorm. Our findings are based on a data set obtained for a particular event. A generalization of the obtained numerical estimates to other events requires additional research and further analysis. |
| ArticleNumber | 6363 |
| Author | Zakharov, V. I. Miloch, W. J. Jin, Y. Chernyshov, A. A. |
| Author_xml | – sequence: 1 givenname: A. A. orcidid: 0000-0003-4692-9643 surname: Chernyshov fullname: Chernyshov, A. A. email: achernyshov@iki.rssi.ru organization: Space Research Institute of the Russian Academy of Science, West Department of Pushkov Institute of Terrestrial Magnetism, Ionosphere and Radio Wave Propagation, RAS – sequence: 2 givenname: W. J. surname: Miloch fullname: Miloch, W. J. organization: Department of Physics, University of Oslo – sequence: 3 givenname: Y. surname: Jin fullname: Jin, Y. organization: Department of Physics, University of Oslo – sequence: 4 givenname: V. I. orcidid: 0000-0002-2214-2195 surname: Zakharov fullname: Zakharov, V. I. organization: Faculty of Physics, Lomonosov Moscow State University |
| BackLink | https://www.ncbi.nlm.nih.gov/pubmed/32286480$$D View this record in MEDLINE/PubMed |
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| CitedBy_id | crossref_primary_10_1038_s41598_025_86960_6 crossref_primary_10_1029_2021RS007344 crossref_primary_10_1016_j_asr_2025_02_015 crossref_primary_10_31857_S0367676524030117 crossref_primary_10_1016_j_ecoser_2024_101660 crossref_primary_10_1007_s11038_024_09556_6 crossref_primary_10_12737_szf_93202307 crossref_primary_10_3390_rs15245685 crossref_primary_10_1029_2021SW002850 crossref_primary_10_1051_swsc_2022038 crossref_primary_10_1016_j_heliyon_2024_e30725 crossref_primary_10_1016_j_asr_2023_06_051 crossref_primary_10_1186_s40623_022_01642_1 crossref_primary_10_12737_stp_93202307 crossref_primary_10_1029_2023SW003475 crossref_primary_10_1007_s11600_021_00568_8 crossref_primary_10_1134_S1062873823705524 |
| Cites_doi | 10.1029/2002GL014770 10.1038/s41598-019-44829-5 10.1029/2007SW000349 10.1134/S0001433818090499 10.1002/2014SW001072 10.1134/S1063780X15030010 10.1029/2009JA014420 10.1029/RS020i003p00347 10.1016/S1364-6826(98)00131-X 10.5194/angeo-28-1307-2010 10.1051/swsc/2014019 10.1186/BF03352332 10.1051/swsc/2013049 10.1134/S0010952516010147 10.1016/j.jastp.2017.06.013 10.1029/2008JA013076 10.5772/54568 10.1007/978-3-7091-3297-5 10.1029/RS020i004p00923 10.1063/1.4916125 10.21046/2070-7401-2017-14-1-88-98 10.1002/2015JA021449 10.1029/97GL02273 10.3367/UFNe.0185.201506i.0649 10.4401/ag-3494 10.1109/PROC.1982.12313 10.1007/s10291-016-0581-6 10.1029/97JA01118 |
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Res.1997102A817219172311997JGR...10217219A10.1029/97JA01118 IlyasovAAChernyshovAAMogilevskyMMGolovchanskayaIVKozelovBVInhomogeneities of plasma density and electric field as sources of electrostatic turbulence in the auroral regionPhysics of Plasmas20152230329062015PhPl...22c2906I1:CAS:528:DC%2BC2MXlt1CgtLY%3D10.1063/1.4916125 KC Yeh (63422_CR15) 1982; 70 Y Jin (63422_CR33) 2014; 4 E Astafyeva (63422_CR14) 2014; 12 EJ Frernouw (63422_CR37) 1985; 20 L Bastos (63422_CR27) 1988; 13 P Prikryl (63422_CR28) 2010; 28 G Paschmann (63422_CR7) 2002; 103 S Basu (63422_CR21) 1985; 20 Y Jin (63422_CR25) 2015; 120 A Kosov (63422_CR12) 2018; 54 63422_CR23 63422_CR26 EL Afraimovich (63422_CR2) 2002; 45 J Aarons. 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| Snippet | The influence of an auroral substorm on the total electron content (TEC) jumps and cycle slips on Global Positioning System (GPS) at high-latitudes is studied.... |
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| SubjectTerms | 704/172/4081 704/525/868 Global positioning systems GPS Humanities and Social Sciences Ionosphere Latitude Magnetic fields multidisciplinary Science Science (multidisciplinary) |
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| Title | Relationship between TEC jumps and auroral substorm in the high-latitude ionosphere |
| URI | https://link.springer.com/article/10.1038/s41598-020-63422-9 https://www.ncbi.nlm.nih.gov/pubmed/32286480 https://www.proquest.com/docview/2389706219 https://www.proquest.com/docview/2389673725 http://hdl.handle.net/10852/83890 https://pubmed.ncbi.nlm.nih.gov/PMC7156765 https://www.nature.com/articles/s41598-020-63422-9.pdf |
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