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21 results for “Campi Flegrei”
Geodetic anomaly detection and analysis in the Campi Flegrei caldera (Italy) deformation pattern of the 2021-2023 escalating unrest phase
<p>Data used within the manuscript: "<strong><span>First evidence of a geodetic anomaly in the Campi Flegrei caldera (Italy) ground deformation pattern revealed by DInSAR and GNSS measurements during the 2021-2023 escalating unrest phase</span>"</strong></p> <p> </p> <p>Archive content:</p> <ul> <li><code>DTSLOS_CNRIREA_20150325_20231021_FB9K</code>: Line of Sight displacement time series retrieved by applying the P-SBAS algorithm to Sentinel-1 data set acquired from ascending orbits (Track 44) over Campi Flegrei caldera in the 20150325 - 20231021 interval. Data format is according to the <a href="https://gitlab.com/epos-tcs-satdata/doc/-/blob/main/TCS_SATD_Product_Description.md#los-displacement-time-series-dtslos" target="_blank" rel="noopener noreferrer">EPOS specification</a>.</li> <li><code>DTSLOS_CNRIREA_20150324_20231020_UJBI</code>: Line of Sight displacement time series retrieved by applying the P-SBAS algorithm to Sentinel-1 data set acquired from descending orbits (Track 22) over Campi Flegrei caldera in the 20150324 - 20231020 interval. Data format is according to the <a href="https://gitlab.com/epos-tcs-satdata/doc/-/blob/main/TCS_SATD_Product_Description.md#los-displacement-time-series-dtslos" target="_blank" rel="noopener noreferrer">EPOS specification</a>.</li> <li><code>Campi_Flegrei_GNSS_Weekly_Timeseries</code>: Weekly displacement time series of Campi Flegrei caldera GNSS network from 2016 to 2023.</li> </ul>
Ground tilt data at Campi Flegrei filtered in the fortnightly (Mf=13.66d) and [12h-90d] bands.
<p>Ground tilt (NS and EW components) at Campi Flegrei from April 1st 2015 to April 30th 2022 recorded at three borehole instruments (CMP, ECO and HDM) of the INGV network. </p> <p>1) Time series filtered in the fortnightly (Mf =13.66 days) tidal band [13 - 14.083 days]. Sampling rate=1min. </p> <p>2) Time series filtered in the [12 hours - 90 days] band. Sampling rate=1hour. </p>
Seismic noise recorded at Bagnolifutura area (Campi Flegrei) in 2012
<p>In 2012 two seismic surveys were carried out in the area of Bagnolifutura (Campi Flegrei, Naples), with the aim of characterizing the properties of the seismic noise. During the first survey, which was conducted from 2 to 4 April, seven broadband three-component seismometers were installed in two different array configurations. The second survey started on November 26 and ended on December 5. During this period, seismic noie was recorded by seven broadband and one short-period three-component sensors.</p>
Dailly Root Mean Square (RMS) of tiltmeter data recorded at Vesuvius and Campi Flegrei
<p>Dailly Root Mean Square (RMS) of tiltmeter data for:</p> <p>1) Vesuvius: time series from October 1<sup>st</sup> 2016 to March 31<sup>th</sup> 2021 recorded at four borehole instruments of the INGV network.</p> <p>2) Campi Flegrei: time series from April 1<sup>st</sup> 2015 to March 31<sup>st</sup> 2021 recorded at three borehole instruments of the INGV network.</p>
Campi Flegrei cGNSS Network - Rinex data quality control (2020)
<p>For each cGNSS station, the file contains a summary report with information about Rinex observation data. For each day, the summary line shows the following information:</p><ol><li>cGNSS station name (Name),</li><li>the start time of the window, the time format is year (Y), month (M), day (D), hour and minutes (Hour), day of year (DOY), modified Julian date (M J Date) and GNSS week (Week),</li><li>the end time of the window, the time format is year (Y), month (M), day (D), hour and minutes (Hour), day of year (DOY), modified Julian date (M J Date), and GNSS week (Week),</li><li>the start and end times of the window (time format is year month day hour min),</li><li>window time laps (Hrs),</li><li>observation interval (OI),</li><li>the number of possible observations (#expt) above the elevation mask,</li><li>the number of complete observations (#obs),</li><li>the ratio of complete to possible observations as a percent (DCP),</li><li>the RMS "multipath combinations" values MP1 and MP2, in meters, limited by the elevation mask (MP1, MP2) rounded to two decimal points,</li><li>cycle slips (CS),</li><li>the ratio of complete observations to cycle slips (obs/CS).</li></ol><p>A full description of cGNSS network is reported in:<br>- De Martino P, Dolce M, Brandi G, Scarpato G, Tammaro U (2021). The Ground Deformation History of the Neapolitan Volcanic Area (Campi Flegrei Caldera, Somma–Vesuvius Volcano, and Ischia Island) from 20 Years of Continuous GPS Observations (2000–2019). Remote Sensing. 13(14):2725. doi:10.3390/rs13142725.</p><p>Please cite this when using the dataset</p>
Campi Flegrei cGPS Daily Timeseries (2000-2019)
<p>Daily positions time series for the 21 Campi Flegrei cGPS stations from January 2000 to December 2019.</p> <p>A full description of cGPS network and time series analysis is reported in:<br> - De Martino P, Dolce M, Brandi G, Scarpato G, Tammaro U (2021). The Ground Deformation History of the Neapolitan Volcanic Area (Campi Flegrei Caldera, Somma–Vesuvius Volcano, and Ischia Island) from 20 Years of Continuous GPS Observations (2000–2019). Remote Sensing. 13(14):2725. doi:10.3390/rs13142725.</p> <p>Please cite this when using the dataset.</p>
Supporting Information for "Data analysis of the unsteadily accelerating GPS and seismic records at Campi Flegrei caldera from 2000 to 2021". Data Set S1. Extended dataset of all the analyses
<p>This compressed folder contains supporting information related to the Figures in the manuscript: "Data analysis of the unsteadily accelerating GPS and seismic records at Campi Flegrei caldera from 2000 to 2021".</p> <p>Files and folders labeled with G1…n are related to the GPS data, those labeled with H1…n are related to the seismic data.</p> <p>In particular: <br> Subfolder 1_DATA supports Figure 3 – the vertical and the horizontal moduli of ground displacement at all analyzed GPS stations; the logarithmic plots of all seismic events and of their energy. It also shows the complete plot leveling data from 1905 to 2010 (modified from del Gaudio et al., 2010). It also includes Figure 2 and Figure 6a-c.</p> <p>Subfolder 2_AnnualRate supports Figure 4 - the annual rate of the vertical and horizontal moduli of ground displacement at all analyzed GPS stations; the annual rate of all seismic events and of their energy. These detail the 2-year, the 6-month, and the 30-day average results. It also supports Figure 5 with similar data concerning 2018-2020.</p> <p>Subfolder 3_InverseRate supports Figure S3 - the inverse rate of the vertical and the horizontal moduli of ground displacement at all analyzed GPS stations; the inverse rate of all seismic events and of their energy. These detail the 2-year, 6-month, and 30-day average results, including detailed plots of 2018-2020.</p> <p>Subfolder 4_RateChange supports Figure S2 - the daily rate change of the vertical and horizontal moduli of ground displacement at all analyzed GPS stations; the daily rate change of all seismic events and of their energy. These detail the 2-year, the 6-month, and the 30-day average results, including detailed plots of 2018-2020.</p> <p>Subfolder 5_FourierCoef supports Figure 6 - the Fourier spectrum of the vertical and the horizontal moduli of ground displacement at all analyzed GPS stations. These detail the 2-year, 6-month, and 30-day average results obtained in 2000-2020, 2011-2020, 2018-2020. Also, additional plots that detail other combinations of time domain and part of the Fourier spectrum, thus testing the sensitivity of the main harmonics on the time domain selected.</p> <p>Subfolder 6_ FFM_WaitTime supports Figure 11 – waiting time examples based on vertical and horizontal moduli of ground displacement at all analyzed GPS stations; all seismic events, and their energy. These detail the 2-year, 6-month, and 30-day average rate results, and the 10-year, 5-year and 3-year regressions.</p> <p>Subfolder 7_FFM_FailTime also supports Figure 11 – all the results expressed in terms of the failure time t<sub>f</sub> instead of in terms of the waiting time [t<sub>f</sub>(t) - t].</p> <p>Subfolder 8_pFFM_Regression supports Figure 9 - the pFFM examples based on the vertical and the horizontal moduli of ground displacement at all analyzed GPS stations; all seismic events and of their energy. These detail the 2-year, 6-month, and 30-day average rate results, and the 10-year, 5-year and 3-year regression.</p> <p>Subfolder 9_pFFM_Probability supports Figure S4 - pFFM examples based on vertical and horizontal moduli of ground displacement at all analyzed GPS stations; all seismic events, and their energy. These detail the 2-year, 6-month, and 30-day average rates, and the 10-year, 5-year and 3-year regressions.</p> <p>Subfolder 10_BarplotProb supports Figure S5 - results expressed in terms of the mean failure time probability at 2, 5, 10, and 25 years.It also supports Figure S6 - examples based on 6-month, and 30-day average rate results.</p> <p>Subfolder 11_BarplotWaitTime supports Figure S6 - all the results expressed in terms of the waiting time (t<sub>f</sub> – t) barplot. It also includes Figure S5.</p>
Relocated event catalog for 2014-2024 seismicity at Campi Flegrei
Open the record for dataset details and reuse information.
Campi Flegrei cGPS network – RINEX data quality control (2000 – 2019)
<p>For each cGPS station, the file contains a summary report with information about Rinex observation data. For each day, the summary line shows the following information:</p> <ol> <li>cGPS station name (Name),</li> <li>the start time of the window, the time format is year (Y), month (M), day (D), hour and minutes (Hour), day of year (DOY), modified Julian date (M J Date) and GPS week (Week),</li> <li>the end time of the window, the time format is year (Y), month (M), day (D), hour and minutes (Hour), day of year (DOY), modified Julian date (M J Date), and GPS week (Week),</li> <li>the start and end times of the window (time format is year month day hour min),</li> <li>window time laps (Hrs),</li> <li>observation interval (OI),</li> <li>the number of possible observations (#expt) above the elevation mask,</li> <li>the number of complete observations (#obs),</li> <li>the ratio of complete to possible observations as a percent (DCP),</li> <li>the RMS “multipath combinations” values MP1 and MP2, in meters, limited by the elevation mask (MP1, MP22) rounded to two decimal points,</li> <li>cycle slips (CS),</li> <li>the ratio of complete observations to cycle slips (obs/CS).</li> </ol> <p>A full description of cGPS network is reported in:<br> - De Martino P, Dolce M, Brandi G, Scarpato G, Tammaro U (2021). The Ground Deformation History of the Neapolitan Volcanic Area (Campi Flegrei Caldera, Somma–Vesuvius Volcano, and Ischia Island) from 20 Years of Continuous GPS Observations (2000–2019). Remote Sensing. 13(14):2725. doi:10.3390/rs13142725.</p> <p>Please cite this when using the dataset</p>
Relocated event catalog for 2014-2023 seismicity at Campi Flegrei
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Seismic catalogue Campi Flegrei 1982-1984
<p>This is a temporary database, an updated database will be created within the INGV database </p>
Ground thermal image temperatures (Campi Flegrei and Vesuvius) and atmospheric temperature and pressure
<p>The dataset contains the ground thermal image temperatures measured by the thermal infrared camera network of Campi Flegrei and Vesuvius (Italy) and the temperature and pressure acquired by a local meteo station. The data refer to the period Jun 25, 2016-May 29, 2020.</p>
Hourly Root Mean Square (RMS) of hydrothermal seismic tremor recorded at Ischia and Campi Flegrei
<p>Hourly Root Mean Square (RMS) of the amplitude of hydrothermal seismic tremor for:</p> <p>1) Time series from 01 Jan to 29 Jun 2020 (180 days) recorded at IOCA station (INGV seismic network), Ischia. Data filtered in the [1-2 Hz] frequency band.</p> <p>2) Time series from 24 Mar to 8 Jun 2020 (75 days) recorded at T1367 station (INGV seismic network), Ischia. Data filtered in the [1-2 Hz] frequency band.</p> <p>3) Time series from 01 Jan to 19 Apr (109 days) recorded at CPIS station (INGV seismic network), Campi Flegrei. Data filtered in the [5-15 Hz] frequency band.</p> <p>4) Time series from 15 Feb to 30 Jun 2020 (136 days) recorded at ASBG station (INGV seismic network), Campi Flegrei. Data filtered in the [0.4-1 Hz] frequency band.</p>
Campi Flegrei cGPS Weekly Positions Time Series
<p>Weekly positions time series for the 21 Campi Flegrei cGPS stations from January 2000 to October 2023.</p><p>A full description of cGPS network and time series analysis is reported in:</p><ul><li>De Martino P, Dolce M, Brandi G, Scarpato G, Tammaro U (2021). The Ground Deformation History of the Neapolitan Volcanic Area (Campi Flegrei Caldera, Somma–Vesuvius Volcano, and Ischia Island) from 20 Years of Continuous GPS Observations (2000–2019). Remote Sensing. 13(14):2725. doi:10.3390/rs13142725.</li></ul><p>Please cite this when using the dataset</p>
NLL-SC processing parameters for the relocation of the 2014-2023 Campi Flegrei seismicity
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Geochemical Data reported in the Monthly Reports "Bollettino di Sorveglianza CAMPI FLEGREI" Period 2022-2023
<p>Chemical compositions of BG fumarole from Solfatara Campi Flegrei (Pozzuoli, Southern Italy) included in the monthly reports named "Bollettino di Sorveglianza CAMPI FLEGREI" (https://www.ov.ingv.it/index.php/monitoraggio-e-infrastrutture/bollettini-tutti/bollett-mensili-cf), in the period 2022-2023.</p> <p>Data are reported as ratios of gas species (e.g CO2/H2O) and in concentrations expressed in micromoles per mole for carbon monoxide.</p>
2005-2019 Campi Flegrei earthquake locations in GIS format
<p>2005-2019 Campi Flegrei earthquake location dataset in GIS format.</p> <p>This is the database used for the paper "GIS applications in volcano monitoring: the study of seismic swarms at the Campi Flegrei volcanic complex, Italy" by Bellucci Sessa, et al. 2021 (https://doi.org/10.5194/adgeo-52-131-2021)</p> <p> </p>
MEDUSA Campi Flegrei cGPS Weekly Timeseries (2016-2019)
<p>Weekly positions time series of the 4 cGPS stations on buoys ( MEDUSA marine research infrastructure) in Campi Flegrei caldera marine sector (Gulf of Pozzuoli) from January 2016 to December 2019.</p> <p>A full description of MEDUSA cGPS time series analysis is reported in:<br> - De Martino P, Guardato S, Donnarumma GP, Dolce M, Trombetti T, Chierici F, Macedonio G, Beranzoli L and Iannaccone G (2020). Four Years of Continuous Seafloor Displacement Measurements in the Campi Flegrei Caldera. Front. Earth Sci. 8:615178. doi: 10.3389/feart.2020.615178.<br> - De Martino P, Dolce M, Brandi G, Scarpato G, Tammaro U (2021). The Ground Deformation History of the Neapolitan Volcanic Area (Campi Flegrei Caldera, Somma–Vesuvius Volcano, and Ischia Island) from 20 Years of Continuous GPS Observations (2000–2019). Remote Sensing. 13(14):2725. doi:10.3390/rs13142725.</p> <p>Please cite these when using the dataset.</p>
Soil thermal gradient at Solfatara during 2020-2021 (Campi Flegrei, south Italy)
<p>The monitoring of energy fluxes associated with diffuse degassing may bean important tool in the surveillance of volcanic activity. In a purely conductive regime, the heat flux is a linear function of the soil thermal gradient with a slope proportional to the thermal conductivity of the medium.</p> <p>For that reason, soil temperatures were continuously measured during two years (2020 and 2021) within the crater of Solfatara using an automatic station. The station was equipped with a Gigalog mod.F data logger that acquires, at 1-hour time intervals, the soil temperature along a vertical profile at 0.1, 0.2, 0.3 and 0.4 m depth, </p> <p>The measurements, expressed in degrees centrigade, made with n.4 Resistance Temperature Detector "RTD" PT100 in platinum class B with a tolerance of ±0.3 °C at 0°C.</p> <p>The coordinates of the instrument are 33T 427461.48m E 4520150.14m N</p>
Soil thermal gradient at Solfatara during 2018-2019 (Campi Flegrei, south Italy)
<p>The monitoring of energy fluxes associated with diffuse degassing may bean important tool in the surveillance of volcanic activity. In a purely conductive regime, the heat flux is a linear function of the soil thermal gradient with a slope proportional to the thermal conductivity of the medium.</p> <p>For that reason, soil temperatures were continuously measured during two years (2018 and 2019) within the crater of Solfatara using an automatic station. The station was equipped with a Gigalog mod.F data logger that acquires, at 1-hour time intervals, the soil temperature along a vertical profile at 0.1, 0.2, 0.3 and 0.4 m depth, </p> <p>The measurements, expressed in degrees centrigade, made with n.4 Resistance Temperature Detector "RTD" PT100 in platinum class B with a tolerance of ±0.3 °C at 0°C.</p> <p>The coordinates of the instrument are 33T 427461.48m E 4520150.14m N</p>
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