Publications matching your search query
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Southern Hemisphere atmospheric history of carbon monoxide over the late Holocene reconstructed from multiple Antarctic ice archives Climate of the Past, 2023
(Ref: 16998)
Authors:
Category 1: Peer-reviewed literature
Carbon monoxide (CO) is a naturally occurring atmospheric trace gas, a regulated pollutant, and one of the main components determining the oxidative capacity of the atmosphere. Evaluating climate…
Ice core chemistry database: an Antarctic compilation of sodium and sulfate records spanning the past 2000 years Earth System Science Data, 2023
(Ref: 16890)
Authors:
Thomas E.R.Vladimirova D.O.Tetzner D.R.Emanuelsson B.D.Chellman N.Dixon D.A.Goosse H.Grieman M.M.King A.C.Sigl M.Udy D.G.Vance T.R.Winski D.A.Winton V.H.L.Bertler A.N.Hori A.Laluraj C.M.McConnell J.R.Motizuki Y.Takahashi K.Motoyama H.Nakai Y.Schwanck F.Simões J.C.Lindau F.G.L.Severi M.Traversi R.Wauthy S.Xiao C.Yang J.Mosely-Thompson E.Khodzher T.V.Golobokova L.P.Ekaykin A.A.
Category 1: Peer-reviewed literature
Changes in sea ice conditions and atmospheric circulation over the Southern Ocean play an important role in modulating Antarctic climate. However, observations of both sea ice and wind conditions are limited in Antarctica and the Southern Ocean, both temporally and spatially…
Improved estimates of preindustrial biomass burning reduce the magnitude of aerosol climate forcing in the Southern Hemisphere Science Advances, 2021
(Ref: 16416)
Authors:
Category 1: Peer-reviewed literature
No Coincident Nitrate Enhancement Events in Polar Ice Cores Following the Largest Known Solar Storms Journal of Geophysical Research: Atmospheres, 2017
(Ref: 15889)
Authors:
Category 1: Peer-reviewed literature
The ice-core record of volcanism: Status and future directions European Geosciences Union General Assembly 2016, Vienna, Austria, 17-22 April 2016, 2016
(Ref: 15800)
Authors:
Category 3: Verbal presentation
Radiative forcing resulting from stratospheric aerosols produced by major volcanic eruptions is a dominant driver of climate variability in the Earth's past.