Regionalization of the Atmospheric Dust Cycle on the Periphery of the East Antarctic Ice Sheet Since the Last Glacial Maximum

Autor: Baccolo G.[1, 2, Delmonte B.[2], Albani S.[4], Baroni C.[5, Cibin G.[7], Frezzotti M.[8], Hampai D.[9], Marcelli A.[9, 10] Revel M.[11], Salvatore M.C.[5, 6] Stenni B.[12], Maggi V.[2

Publikováno v: Geochemistry, Geophysics, Geosystems
Geochemistry, Geophysics, Geosystems, AGU and the Geochemical Society, 2018, 19 (9), pp.3540-3554. ⟨10.1029/2018GC007658⟩
Geochemistry, geophysics, geosystems 19 (2018): 3540–3554. doi:10.1029/2018GC007658
info:cnr-pdr/source/autori:Baccolo G.[1,2,3], Delmonte B.[2], Albani S.[4], Baroni C.[5,6], Cibin G.[7], Frezzotti M.[8], Hampai D.[9], Marcelli A.[9,10] Revel M.[11], Salvatore M.C.[5,6] Stenni B.[12], Maggi V.[2,3]/titolo:Regionalization of the Atmospheric Dust Cycle on the Periphery of the East Antarctic Ice Sheet Since the Last Glacial Maximum/doi:10.1029%2F2018GC007658/rivista:Geochemistry, geophysics, geosystems/anno:2018/pagina_da:3540/pagina_a:3554/intervallo_pagine:3540–3554/volume:19
Geochemistry, Geophysics, Geosystems, 2018, 19 (9), pp.3540-3554. ⟨10.1029/2018GC007658⟩

Ice cores from inner East Antarctica provided some of the longest and most detailed climatic reconstructions and allowed understanding the relationships between atmospheric mineral dust and climate. In this work we present synchrotron radiation X-ray

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::42141cfbcf39064a4b70779860f0a3b6
https://hal.archives-ouvertes.fr/hal-02196120