The weakness of the tremor, the temperature of the coladas and jameos, and the general stability of all the parameters, have been some of the issues that have been discussed at today's meeting of the Steering Committee of the Special Plan for Civil Protection and Emergency Attention for Volcanic Risk of the Canary Islands (PEVOLCA), coordinated by the Minister of Public Administrations, Justice and Security, Julio Pérez.
The technical director of PEVOLCA, Miguel Ángel Morcuende, recalled that during today and tomorrow, on the occasion of Christmas Day, there will be no accompaniments. This will be repeated on
December 31 and
January 1, 2022. Likewise, he insisted that, when the evacuated areas can be accessed, it must always be done in a accompanied manner, the homes must be permanently ventilated and wait, minimum 15 minutes to enter it, focusing on not entering underground areas such as semi-buried warehouses or garages. In addition, he explained that there are still areas of very hot casting at shallow depths that oscillate around 180 degrees in temperature.
María José Blanco, spokesperson for the Scientific Committee, pointed out that the observables, both direct on the surface and from surveillance systems, continue to show signs of exhaustion of the eruptive process. If this trend continues for the next 24 hours, the PEVOLCA Plan would end the eruptive process. However, the end of the eruption does not imply the end of some dangers associated with the volcanic phenomenon, nor the end of the magmatic reactivation in Cumbre Vieja.
Seismicity continues at very low levels at all depths and tremor continues at the background noise level. Despite this, earthquakes that can be felt are not ruled out.
Regarding deformation, the episode that began last
December 19 at the Jedey station (LP03) persists and requires follow-up, although no variations are observed in the rest of the data and observables. Regarding the visible emission of volcanic gases, it is punctual and sporadic, concentrating in the area of the eruptive centers and in the jameos of the volcanic tubes. In addition, small collapses in the crater walls of the main and secondary cone and existing fissures continue to occur.
During yesterday the air quality due to sulfur dioxide (SO2) was at good levels in all seasons, while the emission rate has been low and very low. This is not related to magma ascent, but to a process of solidification of the superficial magma existing in the conduits of the eruptive center.
The diffuse emission of carbon dioxide (CO2) continues to reflect an emission higher than the average value of the background levels and, in fact, yesterday this diffuse emission was 8.5 times the average of the background levels. In some specific areas of Cumbre Vieja, these diffuse CO2 emanations can represent a danger to people as long as high values of diffuse CO2 flux are registered in areas that are not very well ventilated and / or at heights below one meter from the ground as a consequence. of the possible accumulation of CO2 and decrease of oxygen in the air. At the Los Llanos de Aridane station, a slight magmatic-hydrothermal fraction continues to be recorded in the CO2 in the soil atmosphere, while at the Fuencaliente station it is practically nil.
Regarding the concentration of particles less than 10 microns (PM10), air quality levels are maintained in all stations, although yesterday there was a slight increase in them from noon, not exceeding the daily limit value in none of them. However, during this morning the levels remain between good and reasonably good in all the stations of the network.
Regarding the meteorological conditions, the west component wind is expected to turn to the north component during the next morning, weak with a predominance of breezes. Daytime cloudiness is expected today and, as of the next morning, the arrival of a weakened Atlantic front is expected, which will probably produce weak to locally moderate rainfall on the northern slope of La Palma. In this sense, the operation of the airport in the next few hours will be subject only to purely meteorological conditions due to the absence of volcanic ash in the troposphere.
Those housed in hotels stand at 560, three people more than yesterday. Of the total, 385 are staying in Fuencaliente, 105 in Breña Baja and 70 in Los Llanos de Aridane, managed by the Red Cross and municipal services. In addition, 43 dependent people continue to be cared for in insular health centers.
Daily opinion of the Scientific Committee
The observables, both direct on the surface and from surveillance systems, corroborate the signs of exhaustion of the eruptive process. The end of the eruption does not have to imply the end of some dangers associated with the volcanic phenomenon, nor the end of the magmatic reactivation in Cumbre Vieja.
The local deformation episode that began on 12/19 persists, which requires its monitoring, without observing variations in the rest of the data and observables. To be able to say that the eruptive process that began on
September 19 is complete, the recorded and observable data must maintain the signs of depletion of the system for one more day.
The visible emission of volcanic gases is punctual and sporadic, concentrating in the area of the eruptive centers and in the jameos of the volcanic tubes.
Continuous small collapses occur in the walls of the main and secondary cone craters in favor of existing faults and fissures.
Wind from component O that will turn to component N during the next morning, light with a predominance of breezes. Today daytime cloudiness is expected. As of the next morning, the arrival of a weakened Atlantic front will probably produce weak to locally moderate rainfall on the N slope of La Palma. The operation of the airport is subject to purely meteorological conditions, due to the absence of volcanic ash in the troposphere. The trend for the next few days is stable and dry
Weather around the eruption.
The flows reach temperatures of up to 180 degrees despite the fact that the volcano is depleted
The deformation episode that began last
December 19 at the Jedey station (LP03) persists and requires follow-up
The tremor is at the level of the background noise. Seismicity, which is of low magnitude, is at very low levels at all depths. Despite the current level of seismicity, the occurrence of felt earthquakes is not ruled out.
Regarding deformations, without a trend in all stations of the network, except for a local deformation in the Jedey station (LP03) that began on the 19th, it continues after having partially reversed.
As a consequence of the weakness and intermittency of the volcanic gas plume, the SO2 emission ranges will be expressed in units of kilograms per second (kg / s) from this report (*). The emission of sulfur dioxide (SO2) into the atmosphere by the current eruptive process in Cumbre Vieja (visible emanations of volcanic gases), registered through the use of remote optical sensors type miniDOAS in a land mobile position, was LOW yesterday ( 12/22). The LOW and VERY LOW emission rates are not related to magma rise, but rather to a process of solidification of the superficial magma existing in the conduits of the eruptive center.
In the case of non-visible volcanic gas emanations, the diffuse emission of carbon dioxide (CO2), associated with the 220 km2 of the Cumbre Vieja volcanic system, continues to reflect an emission higher than the average value of the background levels (B ) and during yesterday (12/22) this diffuse emission was 8.5 times the average of the background levels (8.5 x B). This diffuse emission is estimated after evaluating and integrating hundreds of diffuse CO2 flow measurements that are carried out at observation points distributed throughout the volcanic building of Cumbre Vieja. In some specific areas of Cumbre Vieja, these diffuse CO2 emanations can represent a danger to people as long as high values of diffuse CO2 flux are registered in areas that are not very well ventilated and / or at heights below one meter from the ground as a consequence. of the possible accumulation of CO2 and decrease of oxygen (O2) in the air. At the Los Llanos de Aridane station (LP10) a slight magmatic-hydrothermal fraction continues to be recorded in the CO2 of the soil atmosphere, while this is practically nil at the Fuencaliente station (LP08). All these geochemical observations are consistent with the current eruptive process. At the Los Llanos de Aridane station (LP10) a slight magmatic-hydrothermal fraction continues to be recorded in the CO2 of the soil atmosphere, while this is practically nil at the Fuencaliente station (LP08). All these geochemical observations are consistent with the current eruptive process. At the Los Llanos de Aridane station (LP10) a slight magmatic-hydrothermal fraction continues to be recorded in the CO2 of the soil atmosphere, while this is practically nil at the Fuencaliente station (LP08). All these geochemical observations are consistent with the current eruptive process.
During yesterday the air quality due to sulfur dioxide (SO2), a pollutant associated with the eruptive process, continued at good levels in all seasons. No exceedances of the hourly or daily limit values have been recorded in any station. In the early morning and tomorrow of today good levels of air quality are maintained in all stations.
With regard to particles smaller than 10 microns (PM10), yesterday, air quality levels have been maintained in all stations, with a slight increase in them from noon, not exceeding the limit value daily (set at 50 µg / m3) in none of them. During the morning of today the levels are maintained, between good and reasonably good in all the stations of the network. Consult the website of the Government of the Canary Islands for Air Quality:
https://www.canarias7.es/canarias/la-pal...ados&vli=_