Importance of Human-Induced Nitrogen Flux Increases for Simulated Arctic Warming

Human activities such as fossil fuel combustion, land-use change, nitrogen (N) fertilizer use, emission of livestock, and waste excretion accelerate the transformation of reactive N and its impact on the marine environment. This study elucidates that anthropogenic N fluxes (ANFs) from atmospheric an...

Full description

Bibliographic Details
Published in:Journal of Climate
Main Authors: Lim, Hyung-Gyu, Park, Jong-Yeon, Dunne, John P., Stock, Charles A., Kang, Sung-Ho, Kug, Jong-Seong
Format: Article in Journal/Newspaper
Language:English
Published: AMER METEOROLOGICAL SOC 2021
Subjects:
Online Access:https://oasis.postech.ac.kr/handle/2014.oak/106844
https://doi.org/10.1175/JCLI-D-20-0180.1
id ftponangunivst:oai:oasis.postech.ac.kr:2014.oak/106844
record_format openpolar
spelling ftponangunivst:oai:oasis.postech.ac.kr:2014.oak/106844 2023-05-15T14:38:16+02:00 Importance of Human-Induced Nitrogen Flux Increases for Simulated Arctic Warming Lim, Hyung-Gyu Park, Jong-Yeon Dunne, John P. Stock, Charles A. Kang, Sung-Ho Kug, Jong-Seong Kug, Jong-Seong 2021-05 https://oasis.postech.ac.kr/handle/2014.oak/106844 https://doi.org/10.1175/JCLI-D-20-0180.1 English eng AMER METEOROLOGICAL SOC JOURNAL OF CLIMATE Meteorology & Atmospheric Sciences 0894-8755 https://oasis.postech.ac.kr/handle/2014.oak/106844 doi:10.1175/JCLI-D-20-0180.1 45563 JOURNAL OF CLIMATE, v.34, no.10, pp.3799 - 3819 000644153200005 2-s2.0-85105315329 SEA-ICE LOSS FUTURE CLIMATE-CHANGE BASE-LINE PART I ANTHROPOGENIC NITROGEN DYNAMICAL CORE OCEAN CARBON MODEL PHYTOPLANKTON Arctic Climate change Ocean models Article ART 2021 ftponangunivst https://doi.org/10.1175/JCLI-D-20-0180.1 2022-10-20T21:02:41Z Human activities such as fossil fuel combustion, land-use change, nitrogen (N) fertilizer use, emission of livestock, and waste excretion accelerate the transformation of reactive N and its impact on the marine environment. This study elucidates that anthropogenic N fluxes (ANFs) from atmospheric and river deposition exacerbate Arctic warming and sea ice loss via physical-biological feedback. The impact of physical-biological feedback is quantified through a suite of experiments using a coupled climate-ocean-biogeochemical model (GFDL-CM2.1-TOPAZ) by prescribing the preindustrial and contemporary amounts of riverine and atmospheric N fluxes into the Arctic Ocean. The experiment forced by ANFs represents the increase in ocean N inventory and chlorophyll concentrations in present and projected future Arctic Ocean relative to the experiment forced by preindustrial N flux inputs. The enhanced chlorophyll concentrations by ANFs reinforce shortwave attenuation in the upper ocean, generating additional warming in the Arctic Ocean. The strongest responses are simulated in the Eurasian shelf seas (Kara, Barents, and Laptev Seas; 65 degrees-90 degrees N, 20 degrees-160 degrees E) due to increased N fluxes, where the annual mean surface temperature increase by 12% and the annual mean sea ice concentration decrease by 17% relative to the future projection, forced by preindustrial N inputs. 1 1 N scie scopus Article in Journal/Newspaper Arctic Arctic Ocean Climate change laptev Phytoplankton Sea ice Pohang University of Science and Technology (POSTECH): Open Access System for Information Sharing (OASIS) Arctic Arctic Ocean Journal of Climate 34 10 3799 3819
institution Open Polar
collection Pohang University of Science and Technology (POSTECH): Open Access System for Information Sharing (OASIS)
op_collection_id ftponangunivst
language English
topic SEA-ICE LOSS
FUTURE CLIMATE-CHANGE
BASE-LINE
PART I
ANTHROPOGENIC NITROGEN
DYNAMICAL CORE
OCEAN
CARBON
MODEL
PHYTOPLANKTON
Arctic
Climate change
Ocean models
spellingShingle SEA-ICE LOSS
FUTURE CLIMATE-CHANGE
BASE-LINE
PART I
ANTHROPOGENIC NITROGEN
DYNAMICAL CORE
OCEAN
CARBON
MODEL
PHYTOPLANKTON
Arctic
Climate change
Ocean models
Lim, Hyung-Gyu
Park, Jong-Yeon
Dunne, John P.
Stock, Charles A.
Kang, Sung-Ho
Kug, Jong-Seong
Importance of Human-Induced Nitrogen Flux Increases for Simulated Arctic Warming
topic_facet SEA-ICE LOSS
FUTURE CLIMATE-CHANGE
BASE-LINE
PART I
ANTHROPOGENIC NITROGEN
DYNAMICAL CORE
OCEAN
CARBON
MODEL
PHYTOPLANKTON
Arctic
Climate change
Ocean models
description Human activities such as fossil fuel combustion, land-use change, nitrogen (N) fertilizer use, emission of livestock, and waste excretion accelerate the transformation of reactive N and its impact on the marine environment. This study elucidates that anthropogenic N fluxes (ANFs) from atmospheric and river deposition exacerbate Arctic warming and sea ice loss via physical-biological feedback. The impact of physical-biological feedback is quantified through a suite of experiments using a coupled climate-ocean-biogeochemical model (GFDL-CM2.1-TOPAZ) by prescribing the preindustrial and contemporary amounts of riverine and atmospheric N fluxes into the Arctic Ocean. The experiment forced by ANFs represents the increase in ocean N inventory and chlorophyll concentrations in present and projected future Arctic Ocean relative to the experiment forced by preindustrial N flux inputs. The enhanced chlorophyll concentrations by ANFs reinforce shortwave attenuation in the upper ocean, generating additional warming in the Arctic Ocean. The strongest responses are simulated in the Eurasian shelf seas (Kara, Barents, and Laptev Seas; 65 degrees-90 degrees N, 20 degrees-160 degrees E) due to increased N fluxes, where the annual mean surface temperature increase by 12% and the annual mean sea ice concentration decrease by 17% relative to the future projection, forced by preindustrial N inputs. 1 1 N scie scopus
author2 Kug, Jong-Seong
format Article in Journal/Newspaper
author Lim, Hyung-Gyu
Park, Jong-Yeon
Dunne, John P.
Stock, Charles A.
Kang, Sung-Ho
Kug, Jong-Seong
author_facet Lim, Hyung-Gyu
Park, Jong-Yeon
Dunne, John P.
Stock, Charles A.
Kang, Sung-Ho
Kug, Jong-Seong
author_sort Lim, Hyung-Gyu
title Importance of Human-Induced Nitrogen Flux Increases for Simulated Arctic Warming
title_short Importance of Human-Induced Nitrogen Flux Increases for Simulated Arctic Warming
title_full Importance of Human-Induced Nitrogen Flux Increases for Simulated Arctic Warming
title_fullStr Importance of Human-Induced Nitrogen Flux Increases for Simulated Arctic Warming
title_full_unstemmed Importance of Human-Induced Nitrogen Flux Increases for Simulated Arctic Warming
title_sort importance of human-induced nitrogen flux increases for simulated arctic warming
publisher AMER METEOROLOGICAL SOC
publishDate 2021
url https://oasis.postech.ac.kr/handle/2014.oak/106844
https://doi.org/10.1175/JCLI-D-20-0180.1
geographic Arctic
Arctic Ocean
geographic_facet Arctic
Arctic Ocean
genre Arctic
Arctic Ocean
Climate change
laptev
Phytoplankton
Sea ice
genre_facet Arctic
Arctic Ocean
Climate change
laptev
Phytoplankton
Sea ice
op_relation JOURNAL OF CLIMATE
Meteorology & Atmospheric Sciences
0894-8755
https://oasis.postech.ac.kr/handle/2014.oak/106844
doi:10.1175/JCLI-D-20-0180.1
45563
JOURNAL OF CLIMATE, v.34, no.10, pp.3799 - 3819
000644153200005
2-s2.0-85105315329
op_doi https://doi.org/10.1175/JCLI-D-20-0180.1
container_title Journal of Climate
container_volume 34
container_issue 10
container_start_page 3799
op_container_end_page 3819
_version_ 1766310382704525312