Artículo de revista
Global quieting of high-frequency seismic noise due to COVID-19 pandemic lockdown measures
Fecha
2020Registro en:
Science Volumen: 369 Número: 6509 Páginas: 1338-1343 Sep 2020
10.1126/science.abd2438
Autor
Lecocq, Thomas
Hicks, Stephen P.
Van Noten, Koen
van Wijk, Kasper
Koelemeijer, Paula
De Plaen, Raphael S. M.
Massin, Frederick
Hillers, Gregor
Anthony, Robert E.
Apoloner, Maria Theresia
Arroyo Solorzano, Mario
Assink, Jelle D.
Bueyuekakpinar, Pinar
Cannata, Andrea
Cannavo, Flavio
Carrasco, Sebastian
Caudron, Corentin
Chaves, Esteban J.
Cornwell, David G.
Craig, David
den Ouden, Olivier F. C.
Díaz, Jordi
Donner, Stefanie
Evangelidis, Christos P.
Evers, Laslo
Fauville, Benoit
Fernández, Gonzalo A.
Giannopoulos, Dimitrios
Gibbons, Steven J.
Girona, Tarsilo
Grecu, Bogdan
Grunberg, Marc
Hetenyi, Gyorgy
Horleston, Anna
Inza, Adolfo
Irving, Jessica C. E.
Jamalreyhani, Mohammadreza
Kafka, Alan
Koymans, Mathijs R.
Labedz, Celeste R.
Larose, Eric
Lindsey, Nathaniel J.
McKinnon, Mika
Megies, Tobias
Miller, Meghan S.
Minarik, William
Moresi, Louis
Marquez Ramírez, Victor H.
Mollhoff, Martin
Nesbitt, Ian M.
Niyogi, Shankho
Ojeda, Javier
Oth, Adrien
Proud, Simon
Pulli, Jay
Retailleau, Lise
Rintamaki, Annukka E.
Satriano, Claudio
Savage, Martha K.
Shani Kadmiel, Shahar
Sleeman, Reinoud
Sokos, Efthimios
Stammler, Klaus
Stott, Alexander E.
Subedi, Shiba
Sorensen, Mathilde B.
Taira, Taka'aki
Tapia, Mar
Turhan, Fatih
van der Pluijm, Ben
Vanstone, Mark
Vergne, Jerome
Vuorinen, Tommi A. T.
Warren, Tristram
Wassermann, Joachim
Xiao, Han
Institución
Resumen
Human activity causes vibrations that propagate into the ground as high-frequency seismic waves. Measures to mitigate the coronavirus disease 2019 (COVID-19) pandemic caused widespread changes in human activity, leading to a months-long reduction in seismic noise of up to 50%. The 2020 seismic noise quiet period is the longest and most prominent global anthropogenic seismic noise reduction on record. Although the reduction is strongest at surface seismometers in populated areas, this seismic quiescence extends for many kilometers radially and hundreds of meters in depth. This quiet period provides an opportunity to detect subtle signals from subsurface seismic sources that would have been concealed in noisier times and to benchmark sources of anthropogenic noise. A strong correlation between seismic noise and independent measurements of human mobility suggests that seismology provides an absolute, real-time estimate of human activities.