Changes in Black Carbon Deposition to Antarctica from Two Ice Core Records, A.D. 1850-2000

Continuous flow analysis was based on a steady sample flow and in-line detection of BC and other chemical substances as described in McConnell et al. (2007). In the cold room, previously cut one meter ice core sticks of 3x3cm, are melted continuously on a heated melter head specifically designed to...

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Main Authors: Smith, Andrew M., Taylor, Kendrick, Curran, Mark A. J., Edward, Ross, Penner, Joyce E., Pasteris, Daniel R., VanOmmen, Tas D., Bisiaux, Marion M., McConnell, Joseph R., Neumann, Thomas A.
Format: Other/Unknown Material
Language:unknown
Published: 2012
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Online Access:http://hdl.handle.net/2060/20120010622
id ftnasantrs:oai:casi.ntrs.nasa.gov:20120010622
record_format openpolar
spelling ftnasantrs:oai:casi.ntrs.nasa.gov:20120010622 2023-05-15T14:05:05+02:00 Changes in Black Carbon Deposition to Antarctica from Two Ice Core Records, A.D. 1850-2000 Smith, Andrew M. Taylor, Kendrick Curran, Mark A. J. Edward, Ross Penner, Joyce E. Pasteris, Daniel R. VanOmmen, Tas D. Bisiaux, Marion M. McConnell, Joseph R. Neumann, Thomas A. Unclassified, Unlimited, Publicly available May 09, 2012 application/pdf http://hdl.handle.net/2060/20120010622 unknown Document ID: 20120010622 http://hdl.handle.net/2060/20120010622 Copyright, Distribution as joint owner in the copyright CASI Geophysics GSFC.JA.00429.2012 2012 ftnasantrs 2019-07-21T06:21:02Z Continuous flow analysis was based on a steady sample flow and in-line detection of BC and other chemical substances as described in McConnell et al. (2007). In the cold room, previously cut one meter ice core sticks of 3x3cm, are melted continuously on a heated melter head specifically designed to eliminate contamination from the atmosphere or by the external parts of the ice. The melted ice from the most inner part of the ice stick is continuously pumped by a peristaltic pump and carried to a clean lab by Teflon lines. The recorded signal is continuous, integrating a sample volume of about 0.05 mL, for which the temporal resolution depends on the speed of melting, ice density and snow accumulation rate at the ice core drilling site. For annual accumulation derived from the WAIS and Law Dome ice cores, we assumed ~3.1 cm water equivalent uncertainty in each year's accumulation from short scale spatial variability (glaciological noise) which was determined from several measurements of annual accumulation in multiple parallel ice cores notably from the WAIS Divide ice core site (Banta et al., 2008) and from South Pole site (McConnell et al., 1997; McConnell et al., 2000). Refractory black carbon (rBC) concentrations were determined using the same method as in (Bisiaux et al., 2011) and adapted to continuous flow measurements as described by (McConnell et al., 2007). The technique uses a single particle intracavity laser induced incandescence photometer (SP2, Droplet Measurement Technologies, Boulder, Colorado) coupled to an ultrasonic nebulizer/desolvation (CETAC UT5000) Flow Injection Analysis (FIA). All analyses, sample preparation etc, were performed in a class 100 cleanroom using anti contamination "clean techniques". The samples were not acidified. Other/Unknown Material Antarc* Antarctica ice core South pole South pole NASA Technical Reports Server (NTRS) South Pole Law Dome ENVELOPE(112.833,112.833,-66.733,-66.733)
institution Open Polar
collection NASA Technical Reports Server (NTRS)
op_collection_id ftnasantrs
language unknown
topic Geophysics
spellingShingle Geophysics
Smith, Andrew M.
Taylor, Kendrick
Curran, Mark A. J.
Edward, Ross
Penner, Joyce E.
Pasteris, Daniel R.
VanOmmen, Tas D.
Bisiaux, Marion M.
McConnell, Joseph R.
Neumann, Thomas A.
Changes in Black Carbon Deposition to Antarctica from Two Ice Core Records, A.D. 1850-2000
topic_facet Geophysics
description Continuous flow analysis was based on a steady sample flow and in-line detection of BC and other chemical substances as described in McConnell et al. (2007). In the cold room, previously cut one meter ice core sticks of 3x3cm, are melted continuously on a heated melter head specifically designed to eliminate contamination from the atmosphere or by the external parts of the ice. The melted ice from the most inner part of the ice stick is continuously pumped by a peristaltic pump and carried to a clean lab by Teflon lines. The recorded signal is continuous, integrating a sample volume of about 0.05 mL, for which the temporal resolution depends on the speed of melting, ice density and snow accumulation rate at the ice core drilling site. For annual accumulation derived from the WAIS and Law Dome ice cores, we assumed ~3.1 cm water equivalent uncertainty in each year's accumulation from short scale spatial variability (glaciological noise) which was determined from several measurements of annual accumulation in multiple parallel ice cores notably from the WAIS Divide ice core site (Banta et al., 2008) and from South Pole site (McConnell et al., 1997; McConnell et al., 2000). Refractory black carbon (rBC) concentrations were determined using the same method as in (Bisiaux et al., 2011) and adapted to continuous flow measurements as described by (McConnell et al., 2007). The technique uses a single particle intracavity laser induced incandescence photometer (SP2, Droplet Measurement Technologies, Boulder, Colorado) coupled to an ultrasonic nebulizer/desolvation (CETAC UT5000) Flow Injection Analysis (FIA). All analyses, sample preparation etc, were performed in a class 100 cleanroom using anti contamination "clean techniques". The samples were not acidified.
format Other/Unknown Material
author Smith, Andrew M.
Taylor, Kendrick
Curran, Mark A. J.
Edward, Ross
Penner, Joyce E.
Pasteris, Daniel R.
VanOmmen, Tas D.
Bisiaux, Marion M.
McConnell, Joseph R.
Neumann, Thomas A.
author_facet Smith, Andrew M.
Taylor, Kendrick
Curran, Mark A. J.
Edward, Ross
Penner, Joyce E.
Pasteris, Daniel R.
VanOmmen, Tas D.
Bisiaux, Marion M.
McConnell, Joseph R.
Neumann, Thomas A.
author_sort Smith, Andrew M.
title Changes in Black Carbon Deposition to Antarctica from Two Ice Core Records, A.D. 1850-2000
title_short Changes in Black Carbon Deposition to Antarctica from Two Ice Core Records, A.D. 1850-2000
title_full Changes in Black Carbon Deposition to Antarctica from Two Ice Core Records, A.D. 1850-2000
title_fullStr Changes in Black Carbon Deposition to Antarctica from Two Ice Core Records, A.D. 1850-2000
title_full_unstemmed Changes in Black Carbon Deposition to Antarctica from Two Ice Core Records, A.D. 1850-2000
title_sort changes in black carbon deposition to antarctica from two ice core records, a.d. 1850-2000
publishDate 2012
url http://hdl.handle.net/2060/20120010622
op_coverage Unclassified, Unlimited, Publicly available
long_lat ENVELOPE(112.833,112.833,-66.733,-66.733)
geographic South Pole
Law Dome
geographic_facet South Pole
Law Dome
genre Antarc*
Antarctica
ice core
South pole
South pole
genre_facet Antarc*
Antarctica
ice core
South pole
South pole
op_source CASI
op_relation Document ID: 20120010622
http://hdl.handle.net/2060/20120010622
op_rights Copyright, Distribution as joint owner in the copyright
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