1750 to 2010 Refractory Black Carbon Deposition from a Global Ice-Core Array, Arctic, Antarctic, and alpine regions ...

Refractory black carbon (rBC) aerosols in air and precipitation result from incomplete combustion. Prior to 18th century industrialization, the primary emission sources were wildfires and agricultural fires. After industrialization, fossil fuel burning has become an important emission source as well...

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Bibliographic Details
Main Authors: McConnell, Joseph, Chellman, Nathan
Format: Dataset
Language:English
Published: Arctic Data Center 2024
Subjects:
Online Access:https://dx.doi.org/10.18739/a2kh0f13w
https://arcticdata.io/catalog/view/doi:10.18739/A2KH0F13W
id ftdatacite:10.18739/a2kh0f13w
record_format openpolar
spelling ftdatacite:10.18739/a2kh0f13w 2024-06-09T07:38:01+00:00 1750 to 2010 Refractory Black Carbon Deposition from a Global Ice-Core Array, Arctic, Antarctic, and alpine regions ... McConnell, Joseph Chellman, Nathan 2024 text/xml https://dx.doi.org/10.18739/a2kh0f13w https://arcticdata.io/catalog/view/doi:10.18739/A2KH0F13W en eng Arctic Data Center EARTH SCIENCE > PALEOCLIMATE > ICE CORE RECORDS > PARTICULATE MATTER EARTH SCIENCE > ATMOSPHERE > AEROSOLS > DUST/ASH/SMOKE EARTH SCIENCE > ATMOSPHERE > AEROSOLS > BLACK CARBON EARTH SCIENCE > CRYOSPHERE > SNOW/ICE > ALBEDO Dataset dataset 2024 ftdatacite https://doi.org/10.18739/a2kh0f13w 2024-05-13T10:53:51Z Refractory black carbon (rBC) aerosols in air and precipitation result from incomplete combustion. Prior to 18th century industrialization, the primary emission sources were wildfires and agricultural fires. After industrialization, fossil fuel burning has become an important emission source as well. Because these aerosols are import contributors to Earth’s radiative forcing both in the air and when deposited to bright surfaces such as fresh snow, quantifying past rBC emissions is critical to accurate Earth System Modeling. This data set contains 1750 to 2010 annual rBC depositional fluxes measured in a global array of 31, mostly polar ice cores. They were used (Zhang et al., Nature Communications, 2024) to reconstruct atmospheric rBC emissions using the atmospheric chemical transport GEOS-Chem. Details on the rBC measurement methods and chronology development are provided in the associated references for the individual ice core records. ... Dataset albedo Antarc* Antarctic Arctic black carbon ice core DataCite Metadata Store (German National Library of Science and Technology) Antarctic Arctic
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language English
topic EARTH SCIENCE > PALEOCLIMATE > ICE CORE RECORDS > PARTICULATE MATTER
EARTH SCIENCE > ATMOSPHERE > AEROSOLS > DUST/ASH/SMOKE
EARTH SCIENCE > ATMOSPHERE > AEROSOLS > BLACK CARBON
EARTH SCIENCE > CRYOSPHERE > SNOW/ICE > ALBEDO
spellingShingle EARTH SCIENCE > PALEOCLIMATE > ICE CORE RECORDS > PARTICULATE MATTER
EARTH SCIENCE > ATMOSPHERE > AEROSOLS > DUST/ASH/SMOKE
EARTH SCIENCE > ATMOSPHERE > AEROSOLS > BLACK CARBON
EARTH SCIENCE > CRYOSPHERE > SNOW/ICE > ALBEDO
McConnell, Joseph
Chellman, Nathan
1750 to 2010 Refractory Black Carbon Deposition from a Global Ice-Core Array, Arctic, Antarctic, and alpine regions ...
topic_facet EARTH SCIENCE > PALEOCLIMATE > ICE CORE RECORDS > PARTICULATE MATTER
EARTH SCIENCE > ATMOSPHERE > AEROSOLS > DUST/ASH/SMOKE
EARTH SCIENCE > ATMOSPHERE > AEROSOLS > BLACK CARBON
EARTH SCIENCE > CRYOSPHERE > SNOW/ICE > ALBEDO
description Refractory black carbon (rBC) aerosols in air and precipitation result from incomplete combustion. Prior to 18th century industrialization, the primary emission sources were wildfires and agricultural fires. After industrialization, fossil fuel burning has become an important emission source as well. Because these aerosols are import contributors to Earth’s radiative forcing both in the air and when deposited to bright surfaces such as fresh snow, quantifying past rBC emissions is critical to accurate Earth System Modeling. This data set contains 1750 to 2010 annual rBC depositional fluxes measured in a global array of 31, mostly polar ice cores. They were used (Zhang et al., Nature Communications, 2024) to reconstruct atmospheric rBC emissions using the atmospheric chemical transport GEOS-Chem. Details on the rBC measurement methods and chronology development are provided in the associated references for the individual ice core records. ...
format Dataset
author McConnell, Joseph
Chellman, Nathan
author_facet McConnell, Joseph
Chellman, Nathan
author_sort McConnell, Joseph
title 1750 to 2010 Refractory Black Carbon Deposition from a Global Ice-Core Array, Arctic, Antarctic, and alpine regions ...
title_short 1750 to 2010 Refractory Black Carbon Deposition from a Global Ice-Core Array, Arctic, Antarctic, and alpine regions ...
title_full 1750 to 2010 Refractory Black Carbon Deposition from a Global Ice-Core Array, Arctic, Antarctic, and alpine regions ...
title_fullStr 1750 to 2010 Refractory Black Carbon Deposition from a Global Ice-Core Array, Arctic, Antarctic, and alpine regions ...
title_full_unstemmed 1750 to 2010 Refractory Black Carbon Deposition from a Global Ice-Core Array, Arctic, Antarctic, and alpine regions ...
title_sort 1750 to 2010 refractory black carbon deposition from a global ice-core array, arctic, antarctic, and alpine regions ...
publisher Arctic Data Center
publishDate 2024
url https://dx.doi.org/10.18739/a2kh0f13w
https://arcticdata.io/catalog/view/doi:10.18739/A2KH0F13W
geographic Antarctic
Arctic
geographic_facet Antarctic
Arctic
genre albedo
Antarc*
Antarctic
Arctic
black carbon
ice core
genre_facet albedo
Antarc*
Antarctic
Arctic
black carbon
ice core
op_doi https://doi.org/10.18739/a2kh0f13w
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