Distribution of anthropogenic CO2 in the Pacific Ocean
[1] This work presents an estimate of anthropogenic CO2 in the Pacific Ocean based on measurements from the WOCE/JGOFS/OACES global CO2 survey. These estimates used a modified version of the DeltaC* technique. Modifications include a revised preformed alkalinity term, a correction for denitrificatio...
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Online Access: | https://oasis.postech.ac.kr/handle/2014.oak/29090 https://doi.org/10.1029/2001GB001639 |
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ftponangunivst:oai:oasis.postech.ac.kr:2014.oak/29090 2023-05-15T17:35:17+02:00 Distribution of anthropogenic CO2 in the Pacific Ocean Sabine, CL Feely, RA Key, RM Bullister, JL Millero, FJ Lee, K Peng, TH Tilbrook, B Ono, T Wong, CS 환경연구소 10056383 Lee, K 2002-10 https://oasis.postech.ac.kr/handle/2014.oak/29090 https://doi.org/10.1029/2001GB001639 English eng AMER GEOPHYSICAL UNION GLOBAL BIOGEOCHEMICAL CYCLES 16 4 1 17 SCI급, SCOPUS 등재논문 SCI Environmental Sciences Geosciences, Multidisciplinary Meteorology & Atmospheric Sciences Environmental Sciences & Ecology Geology 0886-6236 2002-OAK-0000016371 https://oasis.postech.ac.kr/handle/2014.oak/29090 doi:10.1029/2001GB001639 3292 GLOBAL BIOGEOCHEMICAL CYCLES, v.16, no.4, pp.1 - 17 000180874100030 Pacific Ocean anthropogenic CO2 carbon cycle total CO2 delta C* optimum multiparameter analysis DISSOLVED INORGANIC CARBON WESTERN NORTH PACIFIC INDIAN-OCEAN ATLANTIC-OCEAN SURFACE OCEAN BOTTOM WATER RED-SEA INCREASE DIOXIDE CIRCULATION Article ART 2002 ftponangunivst https://doi.org/10.1029/2001GB001639 2022-10-20T20:18:57Z [1] This work presents an estimate of anthropogenic CO2 in the Pacific Ocean based on measurements from the WOCE/JGOFS/OACES global CO2 survey. These estimates used a modified version of the DeltaC* technique. Modifications include a revised preformed alkalinity term, a correction for denitrification, and an evaluation of the disequilibrium terms using an optimum multiparameter analysis. The total anthropogenic CO2 inventory over an area from 120degreesE to 70degreesW and 70degreesS to 65degreesN (excluding the South China Sea, the Yellow Sea, the Japan/East Sea, and the Sea of Okhotsk) was 44.5 +/- 5 Pg C in 1994. Approximately 28 Pg C was located in the Southern Hemisphere and 16.5 Pg C was located north of the equator. The deepest penetration of anthropogenic CO2 is found at about 50 S. The shallowest penetration is found just north of the equator. Very shallow anthropogenic CO2 penetration is also generally observed in the high-latitude Southern Ocean. One exception to this is found in the far southwestern Pacific where there is evidence of anthropogenic CO2 in the northward moving bottom waters. In the North Pacific a strong zonal gradient is observed in the anthropogenic CO2 penetration depth with the deepest penetration in the western Pacific. The Pacific has the largest total inventory in all of the southern latitudes despite the fact that it generally has the lowest average inventory when normalized to a unit area. The lack of deep and bottom water formation in the North Pacific means that the North Pacific inventories are smaller than the North Atlantic. X 1 1 87 scie scopus Article in Journal/Newspaper North Atlantic Southern Ocean Pohang University of Science and Technology (POSTECH): Open Access System for Information Sharing (OASIS) Indian Okhotsk Pacific Southern Ocean Global Biogeochemical Cycles 16 4 30-1 30-17 |
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 |
Pacific Ocean anthropogenic CO2 carbon cycle total CO2 delta C* optimum multiparameter analysis DISSOLVED INORGANIC CARBON WESTERN NORTH PACIFIC INDIAN-OCEAN ATLANTIC-OCEAN SURFACE OCEAN BOTTOM WATER RED-SEA INCREASE DIOXIDE CIRCULATION |
spellingShingle |
Pacific Ocean anthropogenic CO2 carbon cycle total CO2 delta C* optimum multiparameter analysis DISSOLVED INORGANIC CARBON WESTERN NORTH PACIFIC INDIAN-OCEAN ATLANTIC-OCEAN SURFACE OCEAN BOTTOM WATER RED-SEA INCREASE DIOXIDE CIRCULATION Sabine, CL Feely, RA Key, RM Bullister, JL Millero, FJ Lee, K Peng, TH Tilbrook, B Ono, T Wong, CS Distribution of anthropogenic CO2 in the Pacific Ocean |
topic_facet |
Pacific Ocean anthropogenic CO2 carbon cycle total CO2 delta C* optimum multiparameter analysis DISSOLVED INORGANIC CARBON WESTERN NORTH PACIFIC INDIAN-OCEAN ATLANTIC-OCEAN SURFACE OCEAN BOTTOM WATER RED-SEA INCREASE DIOXIDE CIRCULATION |
description |
[1] This work presents an estimate of anthropogenic CO2 in the Pacific Ocean based on measurements from the WOCE/JGOFS/OACES global CO2 survey. These estimates used a modified version of the DeltaC* technique. Modifications include a revised preformed alkalinity term, a correction for denitrification, and an evaluation of the disequilibrium terms using an optimum multiparameter analysis. The total anthropogenic CO2 inventory over an area from 120degreesE to 70degreesW and 70degreesS to 65degreesN (excluding the South China Sea, the Yellow Sea, the Japan/East Sea, and the Sea of Okhotsk) was 44.5 +/- 5 Pg C in 1994. Approximately 28 Pg C was located in the Southern Hemisphere and 16.5 Pg C was located north of the equator. The deepest penetration of anthropogenic CO2 is found at about 50 S. The shallowest penetration is found just north of the equator. Very shallow anthropogenic CO2 penetration is also generally observed in the high-latitude Southern Ocean. One exception to this is found in the far southwestern Pacific where there is evidence of anthropogenic CO2 in the northward moving bottom waters. In the North Pacific a strong zonal gradient is observed in the anthropogenic CO2 penetration depth with the deepest penetration in the western Pacific. The Pacific has the largest total inventory in all of the southern latitudes despite the fact that it generally has the lowest average inventory when normalized to a unit area. The lack of deep and bottom water formation in the North Pacific means that the North Pacific inventories are smaller than the North Atlantic. X 1 1 87 scie scopus |
author2 |
환경연구소 10056383 Lee, K |
format |
Article in Journal/Newspaper |
author |
Sabine, CL Feely, RA Key, RM Bullister, JL Millero, FJ Lee, K Peng, TH Tilbrook, B Ono, T Wong, CS |
author_facet |
Sabine, CL Feely, RA Key, RM Bullister, JL Millero, FJ Lee, K Peng, TH Tilbrook, B Ono, T Wong, CS |
author_sort |
Sabine, CL |
title |
Distribution of anthropogenic CO2 in the Pacific Ocean |
title_short |
Distribution of anthropogenic CO2 in the Pacific Ocean |
title_full |
Distribution of anthropogenic CO2 in the Pacific Ocean |
title_fullStr |
Distribution of anthropogenic CO2 in the Pacific Ocean |
title_full_unstemmed |
Distribution of anthropogenic CO2 in the Pacific Ocean |
title_sort |
distribution of anthropogenic co2 in the pacific ocean |
publisher |
AMER GEOPHYSICAL UNION |
publishDate |
2002 |
url |
https://oasis.postech.ac.kr/handle/2014.oak/29090 https://doi.org/10.1029/2001GB001639 |
geographic |
Indian Okhotsk Pacific Southern Ocean |
geographic_facet |
Indian Okhotsk Pacific Southern Ocean |
genre |
North Atlantic Southern Ocean |
genre_facet |
North Atlantic Southern Ocean |
op_relation |
GLOBAL BIOGEOCHEMICAL CYCLES 16 4 1 17 SCI급, SCOPUS 등재논문 SCI Environmental Sciences Geosciences, Multidisciplinary Meteorology & Atmospheric Sciences Environmental Sciences & Ecology Geology 0886-6236 2002-OAK-0000016371 https://oasis.postech.ac.kr/handle/2014.oak/29090 doi:10.1029/2001GB001639 3292 GLOBAL BIOGEOCHEMICAL CYCLES, v.16, no.4, pp.1 - 17 000180874100030 |
op_doi |
https://doi.org/10.1029/2001GB001639 |
container_title |
Global Biogeochemical Cycles |
container_volume |
16 |
container_issue |
4 |
container_start_page |
30-1 |
op_container_end_page |
30-17 |
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1766134395033354240 |