Changes
On January 8, 2025 at 12:07:30 AM UTC,
ckancielo:
-
Changed value of field
dataset_end_date
to2025-01-08
in 2025 JANUARY TUCUMAN SAO -
Added resource TMJ20_2025008.SAO to 2025 JANUARY TUCUMAN SAO
| 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": "SAO", | 3 | "data_type": "SAO", | ||
| n | 4 | "dataset_end_date": "2025-01-07", | n | 4 | "dataset_end_date": "2025-01-08", |
| 5 | "dataset_start_date": "2025-01-01", | 5 | "dataset_start_date": "2025-01-01", | ||
| 6 | "groups": [], | 6 | "groups": [], | ||
| 7 | "id": "61b511bf-29b2-42fa-a085-ddf324595f8d", | 7 | "id": "61b511bf-29b2-42fa-a085-ddf324595f8d", | ||
| 8 | "isopen": false, | 8 | "isopen": false, | ||
| 9 | "license_title": null, | 9 | "license_title": null, | ||
| 10 | "maintainer": "Jose Carlos Rodriguez", | 10 | "maintainer": "Jose Carlos Rodriguez", | ||
| 11 | "maintainer_email": "Jrodriguezy@igp.edu.pe", | 11 | "maintainer_email": "Jrodriguezy@igp.edu.pe", | ||
| 12 | "metadata_created": "2025-01-06T15:47:08.925340", | 12 | "metadata_created": "2025-01-06T15:47:08.925340", | ||
| n | 13 | "metadata_modified": "2025-01-07T13:12:10.566538", | n | 13 | "metadata_modified": "2025-01-08T00:07:30.185843", |
| 14 | "name": "2025_01_sao_data_tucu", | 14 | "name": "2025_01_sao_data_tucu", | ||
| 15 | "notes": "Data of Ionosonde - SAO", | 15 | "notes": "Data of Ionosonde - SAO", | ||
| n | 16 | "num_resources": 7, | n | 16 | "num_resources": 8, |
| 17 | "num_tags": 0, | 17 | "num_tags": 0, | ||
| 18 | "organization": { | 18 | "organization": { | ||
| 19 | "approval_status": "approved", | 19 | "approval_status": "approved", | ||
| 20 | "created": "2024-06-07T21:05:19.808275", | 20 | "created": "2024-06-07T21:05:19.808275", | ||
| 21 | "description": "The ionosondes provide virtual height information | 21 | "description": "The ionosondes provide virtual height information | ||
| 22 | and density profile estimates from the bottomside ionosphere (also by | 22 | and density profile estimates from the bottomside ionosphere (also by | ||
| 23 | bistatic soundings) with a cadence as small as 1 min, and follow the | 23 | bistatic soundings) with a cadence as small as 1 min, and follow the | ||
| 24 | twilight and nighttime E-region to sounding frequencies of less than | 24 | twilight and nighttime E-region to sounding frequencies of less than | ||
| 25 | 0.5 MHz when implemented with suitable antennas. They also provide | 25 | 0.5 MHz when implemented with suitable antennas. They also provide | ||
| 26 | information about drifts, ionospheric tilts, and the \u201crms\u201d | 26 | information about drifts, ionospheric tilts, and the \u201crms\u201d | ||
| 27 | amplitude and spectral index of density fluctuations by a phase | 27 | amplitude and spectral index of density fluctuations by a phase | ||
| 28 | structure function method. Five ionosondes with co-located flux-gate | 28 | structure function method. Five ionosondes with co-located flux-gate | ||
| 29 | magnetometers will be placed equidistantly and nearly aligned with the | 29 | magnetometers will be placed equidistantly and nearly aligned with the | ||
| 30 | magnetic flux tube intersecting the magnetic equator at 70\u00b0 W. In | 30 | magnetic flux tube intersecting the magnetic equator at 70\u00b0 W. In | ||
| 31 | our plan, one ionosonde will be installed at Tabatinga, Brazil located | 31 | our plan, one ionosonde will be installed at Tabatinga, Brazil located | ||
| 32 | near Leticia, Colombia and another near Antofagasta, Chile, to observe | 32 | near Leticia, Colombia and another near Antofagasta, Chile, to observe | ||
| 33 | the E- and F-region densities. Field lines intersecting 100 km | 33 | the E- and F-region densities. Field lines intersecting 100 km | ||
| 34 | altitude over these two stations map to the equator at 250 and 260 km | 34 | altitude over these two stations map to the equator at 250 and 260 km | ||
| 35 | respectively. A third ionosonde will be placed very close to the | 35 | respectively. A third ionosonde will be placed very close to the | ||
| 36 | magnetic equator in Puerto Maldonado. Two more ionosonde will be | 36 | magnetic equator in Puerto Maldonado. Two more ionosonde will be | ||
| 37 | located at 19-20\u00b0 away from the magnetic equator, near the crest | 37 | located at 19-20\u00b0 away from the magnetic equator, near the crest | ||
| 38 | caused by the equatorial \u2018fountain\u2019. Data from all 5 | 38 | caused by the equatorial \u2018fountain\u2019. Data from all 5 | ||
| 39 | ionosonde, magnetic fields from the co-located magnetometers, TEC | 39 | ionosonde, magnetic fields from the co-located magnetometers, TEC | ||
| 40 | values from the nearby GPS receivers, and the Kalman filter-based | 40 | values from the nearby GPS receivers, and the Kalman filter-based | ||
| 41 | assimilation will provide several geophysical parameters (winds, | 41 | assimilation will provide several geophysical parameters (winds, | ||
| 42 | electric fields and densities) from the E and F regions, and will also | 42 | electric fields and densities) from the E and F regions, and will also | ||
| 43 | fill in the regions between the sites. This will be the first time | 43 | fill in the regions between the sites. This will be the first time | ||
| 44 | that a numerical model of the equatorial ionosphere can be fully | 44 | that a numerical model of the equatorial ionosphere can be fully | ||
| 45 | constrained by data collected on both sides of the magnetic equator | 45 | constrained by data collected on both sides of the magnetic equator | ||
| 46 | and for a range of altitudes that includes the E region", | 46 | and for a range of altitudes that includes the E region", | ||
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| 48 | "image_url": | 48 | "image_url": | ||
| 49 | "2024-06-11-201428.563392Screenshot-from-2024-06-11-15-14-08.png", | 49 | "2024-06-11-201428.563392Screenshot-from-2024-06-11-15-14-08.png", | ||
| 50 | "is_organization": true, | 50 | "is_organization": true, | ||
| 51 | "name": "ionosonde", | 51 | "name": "ionosonde", | ||
| 52 | "state": "active", | 52 | "state": "active", | ||
| 53 | "title": "IONOSONDE", | 53 | "title": "IONOSONDE", | ||
| 54 | "type": "project" | 54 | "type": "project" | ||
| 55 | }, | 55 | }, | ||
| 56 | "owner_org": "6d5f18bf-4b25-4e58-bfcc-8b011418f417", | 56 | "owner_org": "6d5f18bf-4b25-4e58-bfcc-8b011418f417", | ||
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| 244 | "cache_last_updated": null, | ||||
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| 246 | "created": "2025-01-08T00:07:30.254105", | ||||
| 247 | "datastore_active": false, | ||||
| 248 | "file_date": "2025-01-08", | ||||
| 249 | "format": "TXT", | ||||
| 250 | "hash": "", | ||||
| 251 | "id": "843d1252-fdd7-4e8d-b4ab-ff395c1a4f82", | ||||
| 252 | "last_modified": null, | ||||
| 253 | "metadata_modified": "2025-01-08T00:07:30.230984", | ||||
| 254 | "mimetype": null, | ||||
| 255 | "mimetype_inner": null, | ||||
| 256 | "name": "TMJ20_2025008.SAO", | ||||
| 257 | "others": [], | ||||
| 258 | "package_id": "61b511bf-29b2-42fa-a085-ddf324595f8d", | ||||
| 259 | "position": 7, | ||||
| 260 | "private": false, | ||||
| 261 | "resource_type": null, | ||||
| 262 | "size": null, | ||||
| 263 | "state": "active", | ||||
| 264 | "url": | ||||
| 265 | jicamarca/database-cielo/base/TMJ20/2025/01/08/SAO/TMJ20_2025008.SAO", | ||||
| 266 | "url_type": null, | ||||
| 267 | "voc_file_type": "SAO" | ||||
| 242 | } | 268 | } | ||
| 243 | ], | 269 | ], | ||
| 244 | "state": "active", | 270 | "state": "active", | ||
| 245 | "tags": [], | 271 | "tags": [], | ||
| 246 | "title": "2025 JANUARY TUCUMAN SAO", | 272 | "title": "2025 JANUARY TUCUMAN SAO", | ||
| 247 | "type": "dataset", | 273 | "type": "dataset", | ||
| 248 | "voc_instrument_type": "Ionosonde", | 274 | "voc_instrument_type": "Ionosonde", | ||
| 249 | "voc_station_name": "Tucuman" | 275 | "voc_station_name": "Tucuman" | ||
| 250 | } | 276 | } |