Light-Absorbing Impurities in Snow: A Personal and Historical Account

The ability of light-absorbing impurities (LAI) to darken snow had been known for decades, even inspiring practical applications, but quantification of the radiative forcing awaited radiative-transfer modeling in 1980 and measurement of soot in Arctic snow in 1983-4. Climate-modeling interest in thi...

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Main Author: Stephen G. Warren
Format: Article
Language:English
Published: Frontiers Media S.A. 2019-01-01
Series:Frontiers in Earth Science
Subjects:
Online Access:https://www.frontiersin.org/article/10.3389/feart.2018.00250/full
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author Stephen G. Warren
author_facet Stephen G. Warren
author_sort Stephen G. Warren
collection DOAJ
description The ability of light-absorbing impurities (LAI) to darken snow had been known for decades, even inspiring practical applications, but quantification of the radiative forcing awaited radiative-transfer modeling in 1980 and measurement of soot in Arctic snow in 1983-4. Climate-modeling interest in this forcing began in 2004, spurring a modern explosion of research on several topics: methods to measure black carbon (BC) and other LAI, Arctic air pollution, measurement of BC mixing ratio in snow over large areas, and radiative transfer modeling of this forcing and its climatic and hydrological effects. The BC-content of snow in large remote regions of the northern hemisphere is on the order of 20 parts per billion, causing albedo reductions of ∼1–2%. This reduction is climatically significant but difficult to detect by remote sensing, so quantification requires fieldwork to collect and analyze snow samples. This review is a personal account of early research at the National Center for Atmospheric Research and the University of Washington, followed by a brief summary of recent work by the author and his colleagues.
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spelling doaj.art-ca0a18514efc49d5be69190a9696c7132022-12-22T01:48:23ZengFrontiers Media S.A.Frontiers in Earth Science2296-64632019-01-01610.3389/feart.2018.00250415700Light-Absorbing Impurities in Snow: A Personal and Historical AccountStephen G. WarrenThe ability of light-absorbing impurities (LAI) to darken snow had been known for decades, even inspiring practical applications, but quantification of the radiative forcing awaited radiative-transfer modeling in 1980 and measurement of soot in Arctic snow in 1983-4. Climate-modeling interest in this forcing began in 2004, spurring a modern explosion of research on several topics: methods to measure black carbon (BC) and other LAI, Arctic air pollution, measurement of BC mixing ratio in snow over large areas, and radiative transfer modeling of this forcing and its climatic and hydrological effects. The BC-content of snow in large remote regions of the northern hemisphere is on the order of 20 parts per billion, causing albedo reductions of ∼1–2%. This reduction is climatically significant but difficult to detect by remote sensing, so quantification requires fieldwork to collect and analyze snow samples. This review is a personal account of early research at the National Center for Atmospheric Research and the University of Washington, followed by a brief summary of recent work by the author and his colleagues.https://www.frontiersin.org/article/10.3389/feart.2018.00250/fullsnowlight-absorbing impurities in snowsnow albedoArcticradiative transfer
spellingShingle Stephen G. Warren
Light-Absorbing Impurities in Snow: A Personal and Historical Account
Frontiers in Earth Science
snow
light-absorbing impurities in snow
snow albedo
Arctic
radiative transfer
title Light-Absorbing Impurities in Snow: A Personal and Historical Account
title_full Light-Absorbing Impurities in Snow: A Personal and Historical Account
title_fullStr Light-Absorbing Impurities in Snow: A Personal and Historical Account
title_full_unstemmed Light-Absorbing Impurities in Snow: A Personal and Historical Account
title_short Light-Absorbing Impurities in Snow: A Personal and Historical Account
title_sort light absorbing impurities in snow a personal and historical account
topic snow
light-absorbing impurities in snow
snow albedo
Arctic
radiative transfer
url https://www.frontiersin.org/article/10.3389/feart.2018.00250/full
work_keys_str_mv AT stephengwarren lightabsorbingimpuritiesinsnowapersonalandhistoricalaccount