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...
Published in: | Journal of Climate |
---|---|
Main Authors: | , , , , , |
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 |