Evidence of Regional and Global Climate Change in the Mineral Aerosol (Dust) Record from Ice Cores Through the Anthropocene and Pleistocene.
Dust in the atmosphere has a significant effect on earth’s climate by scattering or absorption of incoming solar radiation, acting as cloud condensation nuclei, or providing critical nutrients to oceans and terrestrial biospheres. Changes in the locations of dust source areas and pathways can provid...
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ftumdeepblue:oai:deepblue.lib.umich.edu:2027.42/120678 2024-01-07T09:39:54+01:00 Evidence of Regional and Global Climate Change in the Mineral Aerosol (Dust) Record from Ice Cores Through the Anthropocene and Pleistocene. Aarons, Sarah Miranda Aciego, Sarah M Blum, Joel D Bassis, Jeremy N Flanner, Mark G Cory, Rose 2016 application/pdf https://hdl.handle.net/2027.42/120678 en_US eng https://hdl.handle.net/2027.42/120678 Dust record in ice cores Dust as an indicator of climate change Reconstruction of atmospheric processes using physical and chemical measurements of dust in ice Influence of retreating ice sheet on local coastal Antarctic climate Anthropogenic input to a midlatitude North American glacier Dust provenance using radiogenic isotopes Geology and Earth Sciences Science Thesis 2016 ftumdeepblue 2023-12-10T17:48:39Z Dust in the atmosphere has a significant effect on earth’s climate by scattering or absorption of incoming solar radiation, acting as cloud condensation nuclei, or providing critical nutrients to oceans and terrestrial biospheres. Changes in the locations of dust source areas and pathways can provide insight into understanding the relationship between mineral dust, global climate, and biogeochemical cycles. To gain a better understanding of the impact of the dust cycle on global and regional climate, the dust records within ice-cores from three locations are utilized to reconstruct changes in atmospheric circulation and dust provenance using radiogenic isotope data, trace and rare earth element composition, anion concentration, dust concentration, and size distribution. In this dissertation thesis, we applied this methodology to investigate three case studies. Ice-core samples from the Upper Fremont Glacier (UFG) in Wyoming, Taylor Dome, an East Antarctic ice-dome, and Taylor Glacier, the outlet glacier for Taylor Dome, are investigated here. In the UFG, we found that samples reveal anthropogenic influences. Variability in dust sources and pathways indicates a transition from far to near-range transport due to land-use changes associated with agricultural activity and livestock grazing expansion during 1700 – 1975 A.D. Samples from Taylor Dome and Taylor Glacier, spanning the time period 1,800 – 55,000 years before present, indicate a shift from long-range transported dust to a more variable local input during the transition out of the last glacial period when global temperatures rose 4-7 degrees C. Dust sources and transport pathway changes reveal atmospheric circulation restructuring following the last climatic transition and subsequent retreat of the Ross Ice Shelf. PhD Geology University of Michigan, Horace H. Rackham School of Graduate Studies http://deepblue.lib.umich.edu/bitstream/2027.42/120678/1/smaarons_1.pdf Thesis Antarc* Antarctic ice core Ice Sheet Ice Shelf Ross Ice Shelf Taylor Glacier University of Michigan: Deep Blue Antarctic Ross Ice Shelf Taylor Dome ENVELOPE(157.667,157.667,-77.667,-77.667) Taylor Glacier ENVELOPE(162.167,162.167,-77.733,-77.733) |
institution |
Open Polar |
collection |
University of Michigan: Deep Blue |
op_collection_id |
ftumdeepblue |
language |
English |
topic |
Dust record in ice cores Dust as an indicator of climate change Reconstruction of atmospheric processes using physical and chemical measurements of dust in ice Influence of retreating ice sheet on local coastal Antarctic climate Anthropogenic input to a midlatitude North American glacier Dust provenance using radiogenic isotopes Geology and Earth Sciences Science |
spellingShingle |
Dust record in ice cores Dust as an indicator of climate change Reconstruction of atmospheric processes using physical and chemical measurements of dust in ice Influence of retreating ice sheet on local coastal Antarctic climate Anthropogenic input to a midlatitude North American glacier Dust provenance using radiogenic isotopes Geology and Earth Sciences Science Aarons, Sarah Miranda Evidence of Regional and Global Climate Change in the Mineral Aerosol (Dust) Record from Ice Cores Through the Anthropocene and Pleistocene. |
topic_facet |
Dust record in ice cores Dust as an indicator of climate change Reconstruction of atmospheric processes using physical and chemical measurements of dust in ice Influence of retreating ice sheet on local coastal Antarctic climate Anthropogenic input to a midlatitude North American glacier Dust provenance using radiogenic isotopes Geology and Earth Sciences Science |
description |
Dust in the atmosphere has a significant effect on earth’s climate by scattering or absorption of incoming solar radiation, acting as cloud condensation nuclei, or providing critical nutrients to oceans and terrestrial biospheres. Changes in the locations of dust source areas and pathways can provide insight into understanding the relationship between mineral dust, global climate, and biogeochemical cycles. To gain a better understanding of the impact of the dust cycle on global and regional climate, the dust records within ice-cores from three locations are utilized to reconstruct changes in atmospheric circulation and dust provenance using radiogenic isotope data, trace and rare earth element composition, anion concentration, dust concentration, and size distribution. In this dissertation thesis, we applied this methodology to investigate three case studies. Ice-core samples from the Upper Fremont Glacier (UFG) in Wyoming, Taylor Dome, an East Antarctic ice-dome, and Taylor Glacier, the outlet glacier for Taylor Dome, are investigated here. In the UFG, we found that samples reveal anthropogenic influences. Variability in dust sources and pathways indicates a transition from far to near-range transport due to land-use changes associated with agricultural activity and livestock grazing expansion during 1700 – 1975 A.D. Samples from Taylor Dome and Taylor Glacier, spanning the time period 1,800 – 55,000 years before present, indicate a shift from long-range transported dust to a more variable local input during the transition out of the last glacial period when global temperatures rose 4-7 degrees C. Dust sources and transport pathway changes reveal atmospheric circulation restructuring following the last climatic transition and subsequent retreat of the Ross Ice Shelf. PhD Geology University of Michigan, Horace H. Rackham School of Graduate Studies http://deepblue.lib.umich.edu/bitstream/2027.42/120678/1/smaarons_1.pdf |
author2 |
Aciego, Sarah M Blum, Joel D Bassis, Jeremy N Flanner, Mark G Cory, Rose |
format |
Thesis |
author |
Aarons, Sarah Miranda |
author_facet |
Aarons, Sarah Miranda |
author_sort |
Aarons, Sarah Miranda |
title |
Evidence of Regional and Global Climate Change in the Mineral Aerosol (Dust) Record from Ice Cores Through the Anthropocene and Pleistocene. |
title_short |
Evidence of Regional and Global Climate Change in the Mineral Aerosol (Dust) Record from Ice Cores Through the Anthropocene and Pleistocene. |
title_full |
Evidence of Regional and Global Climate Change in the Mineral Aerosol (Dust) Record from Ice Cores Through the Anthropocene and Pleistocene. |
title_fullStr |
Evidence of Regional and Global Climate Change in the Mineral Aerosol (Dust) Record from Ice Cores Through the Anthropocene and Pleistocene. |
title_full_unstemmed |
Evidence of Regional and Global Climate Change in the Mineral Aerosol (Dust) Record from Ice Cores Through the Anthropocene and Pleistocene. |
title_sort |
evidence of regional and global climate change in the mineral aerosol (dust) record from ice cores through the anthropocene and pleistocene. |
publishDate |
2016 |
url |
https://hdl.handle.net/2027.42/120678 |
long_lat |
ENVELOPE(157.667,157.667,-77.667,-77.667) ENVELOPE(162.167,162.167,-77.733,-77.733) |
geographic |
Antarctic Ross Ice Shelf Taylor Dome Taylor Glacier |
geographic_facet |
Antarctic Ross Ice Shelf Taylor Dome Taylor Glacier |
genre |
Antarc* Antarctic ice core Ice Sheet Ice Shelf Ross Ice Shelf Taylor Glacier |
genre_facet |
Antarc* Antarctic ice core Ice Sheet Ice Shelf Ross Ice Shelf Taylor Glacier |
op_relation |
https://hdl.handle.net/2027.42/120678 |
_version_ |
1787430204800499712 |