Cambios
En el instante 5 de septiembre de 2024, 15:10:59 UTC,
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Modificado el valor del campo
dataset_end_date
a2016-01-11
en 2016 JANUARY TUPIZA OX -
Modificado el valor del campo
dataset_start_date
a2016-01-11
en 2016 JANUARY TUPIZA OX -
Añadido recurso TZJ2J_2016011230804_OX.png a 2016 JANUARY TUPIZA OX
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Añadido recurso TZJ2J_2016011231305_OX.png a 2016 JANUARY TUPIZA OX
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Añadido recurso TZJ2J_2016011230306_OX.png a 2016 JANUARY TUPIZA OX
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Añadido recurso TZJ2J_2016011225804_OX.png a 2016 JANUARY TUPIZA OX
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Añadido recurso TZJ2J_2016011232805_OX.png a 2016 JANUARY TUPIZA OX
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Añadido recurso TZJ2J_2016011233304_OX.png a 2016 JANUARY TUPIZA OX
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Añadido recurso TZJ2J_2016011234805_OX.png a 2016 JANUARY TUPIZA OX
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Añadido recurso TZJ2J_2016011231804_OX.png a 2016 JANUARY TUPIZA OX
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Añadido recurso TZJ2J_2016011235804_OX.png a 2016 JANUARY TUPIZA OX
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Añadido recurso TZJ2J_2016011235304_OX.png a 2016 JANUARY TUPIZA OX
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Añadido recurso TZJ2J_2016011233805_OX.png a 2016 JANUARY TUPIZA OX
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Añadido recurso TZJ2J_2016011232304_OX.png a 2016 JANUARY TUPIZA OX
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Añadido recurso TZJ2J_2016011234304_OX.png a 2016 JANUARY TUPIZA OX
| f | 1 | { | f | 1 | { |
| 2 | "creator_user_id": "770631d3-fc59-4c0b-a34e-8ec37ebe30ec", | 2 | "creator_user_id": "770631d3-fc59-4c0b-a34e-8ec37ebe30ec", | ||
| 3 | "data_type": "OX", | 3 | "data_type": "OX", | ||
| n | 4 | "dataset_end_date": "2200-01-01", | n | 4 | "dataset_end_date": "2016-01-11", |
| 5 | "dataset_start_date": "1900-01-01", | 5 | "dataset_start_date": "2016-01-11", | ||
| 6 | "groups": [], | 6 | "groups": [], | ||
| 7 | "id": "df224c79-8d57-457f-b8d9-99e6fe538a77", | 7 | "id": "df224c79-8d57-457f-b8d9-99e6fe538a77", | ||
| 8 | "isopen": false, | 8 | "isopen": false, | ||
| 9 | "license_title": null, | 9 | "license_title": null, | ||
| 10 | "metadata_created": "2024-09-05T15:10:58.544264", | 10 | "metadata_created": "2024-09-05T15:10:58.544264", | ||
| n | 11 | "metadata_modified": "2024-09-05T15:10:58.544285", | n | 11 | "metadata_modified": "2024-09-05T15:10:59.548915", |
| 12 | "name": "2016_january_ox_tupi", | 12 | "name": "2016_january_ox_tupi", | ||
| 13 | "notes": "Data of Ionosonde OX", | 13 | "notes": "Data of Ionosonde OX", | ||
| n | 14 | "num_resources": 0, | n | 14 | "num_resources": 13, |
| 15 | "num_tags": 0, | 15 | "num_tags": 0, | ||
| 16 | "organization": { | 16 | "organization": { | ||
| 17 | "approval_status": "approved", | 17 | "approval_status": "approved", | ||
| 18 | "created": "2024-06-07T21:05:19.808275", | 18 | "created": "2024-06-07T21:05:19.808275", | ||
| 19 | "description": "The ionosondes provide virtual height information | 19 | "description": "The ionosondes provide virtual height information | ||
| 20 | and density profile estimates from the bottomside ionosphere (also by | 20 | and density profile estimates from the bottomside ionosphere (also by | ||
| 21 | bistatic soundings) with a cadence as small as 1 min, and follow the | 21 | bistatic soundings) with a cadence as small as 1 min, and follow the | ||
| 22 | twilight and nighttime E-region to sounding frequencies of less than | 22 | twilight and nighttime E-region to sounding frequencies of less than | ||
| 23 | 0.5 MHz when implemented with suitable antennas. They also provide | 23 | 0.5 MHz when implemented with suitable antennas. They also provide | ||
| 24 | information about drifts, ionospheric tilts, and the \u201crms\u201d | 24 | information about drifts, ionospheric tilts, and the \u201crms\u201d | ||
| 25 | amplitude and spectral index of density fluctuations by a phase | 25 | amplitude and spectral index of density fluctuations by a phase | ||
| 26 | structure function method. Five ionosondes with co-located flux-gate | 26 | structure function method. Five ionosondes with co-located flux-gate | ||
| 27 | magnetometers will be placed equidistantly and nearly aligned with the | 27 | magnetometers will be placed equidistantly and nearly aligned with the | ||
| 28 | magnetic flux tube intersecting the magnetic equator at 70\u00b0 W. In | 28 | magnetic flux tube intersecting the magnetic equator at 70\u00b0 W. In | ||
| 29 | our plan, one ionosonde will be installed at Tabatinga, Brazil located | 29 | our plan, one ionosonde will be installed at Tabatinga, Brazil located | ||
| 30 | near Leticia, Colombia and another near Antofagasta, Chile, to observe | 30 | near Leticia, Colombia and another near Antofagasta, Chile, to observe | ||
| 31 | the E- and F-region densities. Field lines intersecting 100 km | 31 | the E- and F-region densities. Field lines intersecting 100 km | ||
| 32 | altitude over these two stations map to the equator at 250 and 260 km | 32 | altitude over these two stations map to the equator at 250 and 260 km | ||
| 33 | respectively. A third ionosonde will be placed very close to the | 33 | respectively. A third ionosonde will be placed very close to the | ||
| 34 | magnetic equator in Puerto Maldonado. Two more ionosonde will be | 34 | magnetic equator in Puerto Maldonado. Two more ionosonde will be | ||
| 35 | located at 19-20\u00b0 away from the magnetic equator, near the crest | 35 | located at 19-20\u00b0 away from the magnetic equator, near the crest | ||
| 36 | caused by the equatorial \u2018fountain\u2019. Data from all 5 | 36 | caused by the equatorial \u2018fountain\u2019. Data from all 5 | ||
| 37 | ionosonde, magnetic fields from the co-located magnetometers, TEC | 37 | ionosonde, magnetic fields from the co-located magnetometers, TEC | ||
| 38 | values from the nearby GPS receivers, and the Kalman filter-based | 38 | values from the nearby GPS receivers, and the Kalman filter-based | ||
| 39 | assimilation will provide several geophysical parameters (winds, | 39 | assimilation will provide several geophysical parameters (winds, | ||
| 40 | electric fields and densities) from the E and F regions, and will also | 40 | electric fields and densities) from the E and F regions, and will also | ||
| 41 | fill in the regions between the sites. This will be the first time | 41 | fill in the regions between the sites. This will be the first time | ||
| 42 | that a numerical model of the equatorial ionosphere can be fully | 42 | that a numerical model of the equatorial ionosphere can be fully | ||
| 43 | constrained by data collected on both sides of the magnetic equator | 43 | constrained by data collected on both sides of the magnetic equator | ||
| 44 | and for a range of altitudes that includes the E region", | 44 | and for a range of altitudes that includes the E region", | ||
| 45 | "id": "6d5f18bf-4b25-4e58-bfcc-8b011418f417", | 45 | "id": "6d5f18bf-4b25-4e58-bfcc-8b011418f417", | ||
| 46 | "image_url": | 46 | "image_url": | ||
| 47 | "2024-06-11-201428.563392Screenshot-from-2024-06-11-15-14-08.png", | 47 | "2024-06-11-201428.563392Screenshot-from-2024-06-11-15-14-08.png", | ||
| 48 | "is_organization": true, | 48 | "is_organization": true, | ||
| 49 | "name": "ionosonde", | 49 | "name": "ionosonde", | ||
| 50 | "state": "active", | 50 | "state": "active", | ||
| 51 | "title": "IONOSONDE", | 51 | "title": "IONOSONDE", | ||
| 52 | "type": "project" | 52 | "type": "project" | ||
| 53 | }, | 53 | }, | ||
| 54 | "owner_org": "6d5f18bf-4b25-4e58-bfcc-8b011418f417", | 54 | "owner_org": "6d5f18bf-4b25-4e58-bfcc-8b011418f417", | ||
| 55 | "private": false, | 55 | "private": false, | ||
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| 57 | "relationships_as_subject": [], | 57 | "relationships_as_subject": [], | ||
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