Continuous seismic observations across the Ross Ice Shelf reveal ubiquitous ambientresonances at frequencies >5 Hz.
[2] These firn-trapped surface wave signals arise through wind and snowbedform interactions coupled with very low velocity structures. Progressive and long-term spectral changesare associated with surface snow redistribution by wind and with a January 2016 regional melt event.
Original Source [3]
Technology Partners: MimirTech
Links:
[1] http://admin.indiaenvironmentportal.org.in/feature-article/near%E2%80%90surface-environmentally-forced-changes-ross-ice-shelf-observed-ambient-seismic
[2] http://www.indiaenvironmentportal.org.in/files/file/Ross_Iceshelf_Chaput_et_al-2018-Geophysical_Research_Letters.pdf
[3] https://agupubs.onlinelibrary.wiley.com/doi/epdf/10.1029/2018GL079665
[4] http://admin.indiaenvironmentportal.org.in/category/author/j-chaput
[5] http://admin.indiaenvironmentportal.org.in/category/author/r-c-aster
[6] http://admin.indiaenvironmentportal.org.in/category/author/d-mcgrath-et-al
[7] http://admin.indiaenvironmentportal.org.in/category/journal/geophysical-research-letters
[8] http://admin.indiaenvironmentportal.org.in/category/thesaurus/climate-change
[9] http://admin.indiaenvironmentportal.org.in/category/thesaurus/climate-science
[10] http://admin.indiaenvironmentportal.org.in/category/thesaurus/antarctica
[11] http://admin.indiaenvironmentportal.org.in/category/thesaurus/glaciers
[12] http://admin.indiaenvironmentportal.org.in/category/thesaurus/sea-level-rise
[13] http://admin.indiaenvironmentportal.org.in/category/thesaurus/global-warming
