How well is black carbon in the Arctic atmosphere captured by models?

International audience A correct representation of the spatial distribution of aerosols in atmospheric models is essential for realistic simulations of deposition and calculations of radiative forcing. It has been observed that transport of black carbon (BC) into the Arctic and scavenging is sometim...

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Main Authors: Eckhardt, Sabine, Berntsen, Terje, Cherian, Ribu, Daskalakis, Nikolaos, Heyes, Chris, Hodnebrog, Øivind, Kanakidou, Maria, Klimont, Zbigniew, Law, Kathy S., Lund, Marianne, Myhre, Gunnar, Myriokefalitakis, Stelios, Olivie, Dirk, Quaas, Johannes, Quennehen, Boris, Raut, Jean-Christophe, Samset, Bjørn, Schulz, Michael, Skeie, Ragnhild, Stohl, Andreas
Other Authors: Norwegian Institute for Air Research (NILU), Center for International Climate and Environmental Research Oslo (CICERO), University of Oslo (UiO), Leipzig University / Universität Leipzig, Environmental Chemical Processes Laboratory Heraklion (ECPL), Department of Chemistry Heraklion, University of Crete Heraklion (UOC)-University of Crete Heraklion (UOC), International Institute for Applied Systems Analysis Laxenburg (IIASA), TROPO - LATMOS, Laboratoire Atmosphères, Milieux, Observations Spatiales (LATMOS), Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS), Leipziger Institut für Meteorologie (LIM), Laboratoire de Météorologie Dynamique (UMR 8539) (LMD), Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-École polytechnique (X), Institut Polytechnique de Paris (IP Paris)-Institut Polytechnique de Paris (IP Paris)-École des Ponts ParisTech (ENPC)-Centre National de la Recherche Scientifique (CNRS)-Département des Géosciences - ENS Paris, École normale supérieure - Paris (ENS-PSL), Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)-École normale supérieure - Paris (ENS-PSL), Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)
Format: Conference Object
Language:English
Published: HAL CCSD 2014
Subjects:
Online Access:https://hal.science/hal-01119111
id ftecoleponts:oai:HAL:hal-01119111v1
record_format openpolar
institution Open Polar
collection École des Ponts ParisTech: HAL
op_collection_id ftecoleponts
language English
topic [PHYS.PHYS.PHYS-AO-PH]Physics [physics]/Physics [physics]/Atmospheric and Oceanic Physics [physics.ao-ph]
[SDE]Environmental Sciences
spellingShingle [PHYS.PHYS.PHYS-AO-PH]Physics [physics]/Physics [physics]/Atmospheric and Oceanic Physics [physics.ao-ph]
[SDE]Environmental Sciences
Eckhardt, Sabine
Berntsen, Terje
Cherian, Ribu
Daskalakis, Nikolaos
Heyes, Chris
Hodnebrog, Øivind
Kanakidou, Maria
Klimont, Zbigniew
Law, Kathy S.
Lund, Marianne
Myhre, Gunnar
Myriokefalitakis, Stelios
Olivie, Dirk
Quaas, Johannes
Quennehen, Boris
Raut, Jean-Christophe
Samset, Bjørn
Schulz, Michael
Skeie, Ragnhild
Stohl, Andreas
How well is black carbon in the Arctic atmosphere captured by models?
topic_facet [PHYS.PHYS.PHYS-AO-PH]Physics [physics]/Physics [physics]/Atmospheric and Oceanic Physics [physics.ao-ph]
[SDE]Environmental Sciences
description International audience A correct representation of the spatial distribution of aerosols in atmospheric models is essential for realistic simulations of deposition and calculations of radiative forcing. It has been observed that transport of black carbon (BC) into the Arctic and scavenging is sometimes not captured accurately enough in chemistry transport models (CTM) as well as global circulation models (GCM). In this study we determine the discrepancies between measured equivalent BC (EBC) and modeled BC for several Arctic measurement stations as well as for Arctic aircraft campaigns. For this, we use the output of a set of 5 models based on the same emission dataset (ECLIPSE emissions, see eclipse.nilu.no) and evaluate the simulated concentrations at the measurement locations and times. Emissions are separated for different sources such as biomass burning, domestic heating, gas flaring, industry and the transport sector. We focus on the years 2008 and 2009, where many campaigns took place in the framework of the International Polar Year. Arctic stations like Barrow, Alert, Station Nord in Greenland and Zeppelin show a very pronounced winter/spring maximum in BC. While monthly averaged measured EBC values are around 80 ng/m^3, the models severely underestimate this with some models simulating only a small percentage of the observed values. During summer measured concentrations are a magnitude lower, and still underestimated by almost an order of magnitude in some models. However, the best models are correct within a factor of 2 in winter/spring and give realistic concentrations in summer. In order to get information on the vertical profile we used measurements from aircraft campaigns like ARCTAS, ARCPAC and HIPPO. It is found that BC in latitudes below 60 degrees is better captured by the models than BC at higher latitudes, even though it is overestimated at high altitudes. A systematic analysis of the performance of different models is presented. With the dataset we use we capture remote, polluted and ...
author2 Norwegian Institute for Air Research (NILU)
Center for International Climate and Environmental Research Oslo (CICERO)
University of Oslo (UiO)
Leipzig University / Universität Leipzig
Environmental Chemical Processes Laboratory Heraklion (ECPL)
Department of Chemistry Heraklion
University of Crete Heraklion (UOC)-University of Crete Heraklion (UOC)
International Institute for Applied Systems Analysis Laxenburg (IIASA)
TROPO - LATMOS
Laboratoire Atmosphères, Milieux, Observations Spatiales (LATMOS)
Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)
Leipziger Institut für Meteorologie (LIM)
Laboratoire de Météorologie Dynamique (UMR 8539) (LMD)
Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-École polytechnique (X)
Institut Polytechnique de Paris (IP Paris)-Institut Polytechnique de Paris (IP Paris)-École des Ponts ParisTech (ENPC)-Centre National de la Recherche Scientifique (CNRS)-Département des Géosciences - ENS Paris
École normale supérieure - Paris (ENS-PSL)
Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)-École normale supérieure - Paris (ENS-PSL)
Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)
format Conference Object
author Eckhardt, Sabine
Berntsen, Terje
Cherian, Ribu
Daskalakis, Nikolaos
Heyes, Chris
Hodnebrog, Øivind
Kanakidou, Maria
Klimont, Zbigniew
Law, Kathy S.
Lund, Marianne
Myhre, Gunnar
Myriokefalitakis, Stelios
Olivie, Dirk
Quaas, Johannes
Quennehen, Boris
Raut, Jean-Christophe
Samset, Bjørn
Schulz, Michael
Skeie, Ragnhild
Stohl, Andreas
author_facet Eckhardt, Sabine
Berntsen, Terje
Cherian, Ribu
Daskalakis, Nikolaos
Heyes, Chris
Hodnebrog, Øivind
Kanakidou, Maria
Klimont, Zbigniew
Law, Kathy S.
Lund, Marianne
Myhre, Gunnar
Myriokefalitakis, Stelios
Olivie, Dirk
Quaas, Johannes
Quennehen, Boris
Raut, Jean-Christophe
Samset, Bjørn
Schulz, Michael
Skeie, Ragnhild
Stohl, Andreas
author_sort Eckhardt, Sabine
title How well is black carbon in the Arctic atmosphere captured by models?
title_short How well is black carbon in the Arctic atmosphere captured by models?
title_full How well is black carbon in the Arctic atmosphere captured by models?
title_fullStr How well is black carbon in the Arctic atmosphere captured by models?
title_full_unstemmed How well is black carbon in the Arctic atmosphere captured by models?
title_sort how well is black carbon in the arctic atmosphere captured by models?
publisher HAL CCSD
publishDate 2014
url https://hal.science/hal-01119111
op_coverage Vienna, Austria
long_lat ENVELOPE(-16.663,-16.663,81.599,81.599)
geographic Arctic
Greenland
Station Nord
geographic_facet Arctic
Greenland
Station Nord
genre Greenland
International Polar Year
genre_facet Greenland
International Polar Year
op_source EGU General Assembly 2014
https://hal.science/hal-01119111
EGU General Assembly 2014, Apr 2014, Vienna, Austria. pp.id.11440
op_relation BIBCODE: 2014EGUGA.1611440E
_version_ 1814273805221101568
spelling ftecoleponts:oai:HAL:hal-01119111v1 2024-10-29T17:44:29+00:00 How well is black carbon in the Arctic atmosphere captured by models? Eckhardt, Sabine Berntsen, Terje Cherian, Ribu Daskalakis, Nikolaos Heyes, Chris Hodnebrog, Øivind Kanakidou, Maria Klimont, Zbigniew Law, Kathy S. Lund, Marianne Myhre, Gunnar Myriokefalitakis, Stelios Olivie, Dirk Quaas, Johannes Quennehen, Boris Raut, Jean-Christophe Samset, Bjørn Schulz, Michael Skeie, Ragnhild Stohl, Andreas Norwegian Institute for Air Research (NILU) Center for International Climate and Environmental Research Oslo (CICERO) University of Oslo (UiO) Leipzig University / Universität Leipzig Environmental Chemical Processes Laboratory Heraklion (ECPL) Department of Chemistry Heraklion University of Crete Heraklion (UOC)-University of Crete Heraklion (UOC) International Institute for Applied Systems Analysis Laxenburg (IIASA) TROPO - LATMOS Laboratoire Atmosphères, Milieux, Observations Spatiales (LATMOS) Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS) Leipziger Institut für Meteorologie (LIM) Laboratoire de Météorologie Dynamique (UMR 8539) (LMD) Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-École polytechnique (X) Institut Polytechnique de Paris (IP Paris)-Institut Polytechnique de Paris (IP Paris)-École des Ponts ParisTech (ENPC)-Centre National de la Recherche Scientifique (CNRS)-Département des Géosciences - ENS Paris École normale supérieure - Paris (ENS-PSL) Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)-École normale supérieure - Paris (ENS-PSL) Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL) Vienna, Austria 2014-04-27 https://hal.science/hal-01119111 en eng HAL CCSD BIBCODE: 2014EGUGA.1611440E EGU General Assembly 2014 https://hal.science/hal-01119111 EGU General Assembly 2014, Apr 2014, Vienna, Austria. pp.id.11440 [PHYS.PHYS.PHYS-AO-PH]Physics [physics]/Physics [physics]/Atmospheric and Oceanic Physics [physics.ao-ph] [SDE]Environmental Sciences info:eu-repo/semantics/conferenceObject Conference papers 2014 ftecoleponts 2024-10-08T23:53:40Z International audience A correct representation of the spatial distribution of aerosols in atmospheric models is essential for realistic simulations of deposition and calculations of radiative forcing. It has been observed that transport of black carbon (BC) into the Arctic and scavenging is sometimes not captured accurately enough in chemistry transport models (CTM) as well as global circulation models (GCM). In this study we determine the discrepancies between measured equivalent BC (EBC) and modeled BC for several Arctic measurement stations as well as for Arctic aircraft campaigns. For this, we use the output of a set of 5 models based on the same emission dataset (ECLIPSE emissions, see eclipse.nilu.no) and evaluate the simulated concentrations at the measurement locations and times. Emissions are separated for different sources such as biomass burning, domestic heating, gas flaring, industry and the transport sector. We focus on the years 2008 and 2009, where many campaigns took place in the framework of the International Polar Year. Arctic stations like Barrow, Alert, Station Nord in Greenland and Zeppelin show a very pronounced winter/spring maximum in BC. While monthly averaged measured EBC values are around 80 ng/m^3, the models severely underestimate this with some models simulating only a small percentage of the observed values. During summer measured concentrations are a magnitude lower, and still underestimated by almost an order of magnitude in some models. However, the best models are correct within a factor of 2 in winter/spring and give realistic concentrations in summer. In order to get information on the vertical profile we used measurements from aircraft campaigns like ARCTAS, ARCPAC and HIPPO. It is found that BC in latitudes below 60 degrees is better captured by the models than BC at higher latitudes, even though it is overestimated at high altitudes. A systematic analysis of the performance of different models is presented. With the dataset we use we capture remote, polluted and ... Conference Object Greenland International Polar Year École des Ponts ParisTech: HAL Arctic Greenland Station Nord ENVELOPE(-16.663,-16.663,81.599,81.599)