Subduction/obduction rate in the North Pacific diagnosed by an eddy-resolving model
Ventilation in the North Pacifi c is examined using data from the eddy-resolving 1/12° global HYbrid Coordinate Ocean Model（HYCOM） and Quik SCAT wind stress data. For the period January 2004 to December 2006 and area 20°–40°N, the total annual subduction rate is estimated at 79 Sv, and the obduction...
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| Published in | Chinese journal of oceanology and limnology Vol. 34; no. 4; pp. 835 - 846 |
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| Main Author | |
| Format | Journal Article |
| Language | English |
| Published |
Heidelberg
Science Press
01.07.2016
Springer Nature B.V |
| Subjects | |
| Online Access | Get full text |
| ISSN | 0254-4059 2096-5508 1993-5005 2523-3521 |
| DOI | 10.1007/s00343-016-5036-y |
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| Abstract | Ventilation in the North Pacifi c is examined using data from the eddy-resolving 1/12° global HYbrid Coordinate Ocean Model（HYCOM） and Quik SCAT wind stress data. For the period January 2004 to December 2006 and area 20°–40°N, the total annual subduction rate is estimated at 79 Sv, and the obduction rate 41 Sv. Resolving the small-scale and high-frequency components of the eddy fi eld can increase the subduction rate by 42 Sv, and obduction by 31 Sv. Lateral induction is the dominant contributor to enhancement of subduction/obduction, and temporal change of mixed layer depth has a secondary role. Further analysis indicates that the high-frequency components of the eddy fi eld, especially those with timescale shorter than 10 days, are the most critical factor enhancing subduction/obduction. |
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| AbstractList | Ventilation in the North Pacific is examined using data from the eddy-resolving 1/12° global HYbrid Coordinate Ocean Model (HYCOM) and QuikSCAT wind stress data. For the period January 2004 to December 2006 and area 20°–40°N, the total annual subduction rate is estimated at 79 Sv, and the obduction rate 41 Sv. Resolving the small-scale and high-frequency components of the eddy field can increase the subduction rate by 42 Sv, and obduction by 31 Sv. Lateral induction is the dominant contributor to enhancement of subduction/obduction, and temporal change of mixed layer depth has a secondary role. Further analysis indicates that the high-frequency components of the eddy field, especially those with timescale shorter than 10 days, are the most critical factor enhancing subduction/obduction. Ventilation in the North Pacific is examined using data from the eddy-resolving 1/12 degree global HYbrid Coordinate Ocean Model (HYCOM) and QuikSCAT wind stress data. For the period January 2004 to December 2006 and area 20 degree -40 degree N, the total annual subduction rate is estimated at 79 Sv, and the obduction rate 41 Sv. Resolving the small-scale and high-frequency components of the eddy field can increase the subduction rate by 42 Sv, and obduction by 31 Sv. Lateral induction is the dominant contributor to enhancement of subduction/obduction, and temporal change of mixed layer depth has a secondary role. Further analysis indicates that the high-frequency components of the eddy field, especially those with timescale shorter than 10 days, are the most critical factor enhancing subduction/obduction. Ventilation in the North Pacifi c is examined using data from the eddy-resolving 1/12° global HYbrid Coordinate Ocean Model（HYCOM） and Quik SCAT wind stress data. For the period January 2004 to December 2006 and area 20°–40°N, the total annual subduction rate is estimated at 79 Sv, and the obduction rate 41 Sv. Resolving the small-scale and high-frequency components of the eddy fi eld can increase the subduction rate by 42 Sv, and obduction by 31 Sv. Lateral induction is the dominant contributor to enhancement of subduction/obduction, and temporal change of mixed layer depth has a secondary role. Further analysis indicates that the high-frequency components of the eddy fi eld, especially those with timescale shorter than 10 days, are the most critical factor enhancing subduction/obduction. |
| Author | 刘玲玲 黄瑞新 王凡 |
| AuthorAffiliation | Key Laboratory of Ocean Circulation and Waves, Institute of Oceanology, Chinese Academy of Sciences, Qingdao 266071, China Department of Physical Oceanography, Woods Hole Oceanographic Institution, Woods Hole, MA 02543, USA |
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| CitedBy_id | crossref_primary_10_1007_s00343_021_1097_7 crossref_primary_10_1007_s11802_020_4203_0 crossref_primary_10_1007_s10872_020_00559_1 crossref_primary_10_1016_j_dsr_2020_103227 |
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| Notes | 37-1150 subduction;obduction;eddy-resolved;high frequency;North Pacific Ventilation in the North Pacifi c is examined using data from the eddy-resolving 1/12° global HYbrid Coordinate Ocean Model（HYCOM） and Quik SCAT wind stress data. For the period January 2004 to December 2006 and area 20°–40°N, the total annual subduction rate is estimated at 79 Sv, and the obduction rate 41 Sv. Resolving the small-scale and high-frequency components of the eddy fi eld can increase the subduction rate by 42 Sv, and obduction by 31 Sv. Lateral induction is the dominant contributor to enhancement of subduction/obduction, and temporal change of mixed layer depth has a secondary role. Further analysis indicates that the high-frequency components of the eddy fi eld, especially those with timescale shorter than 10 days, are the most critical factor enhancing subduction/obduction. ObjectType-Article-1 SourceType-Scholarly Journals-1 ObjectType-Feature-2 content type line 14 content type line 23 |
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| Snippet | Ventilation in the North Pacifi c is examined using data from the eddy-resolving 1/12° global HYbrid Coordinate Ocean Model（HYCOM） and Quik SCAT wind stress... Ventilation in the North Pacific is examined using data from the eddy-resolving 1/12° global HYbrid Coordinate Ocean Model (HYCOM) and QuikSCAT wind stress... Ventilation in the North Pacific is examined using data from the eddy-resolving 1/12 degree global HYbrid Coordinate Ocean Model (HYCOM) and QuikSCAT wind... |
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| SubjectTerms | Components Earth and Environmental Science Earth Sciences environmental models Frequency General circulation models Marine Mixed layer Mixed layer depth Obduction Ocean circulation Ocean currents Ocean models Oceanography Physics Subduction temporal variation Ventilation Vortices wind Wind stress 俯冲 北太平洋 数据检查 模型诊断 海洋模式 涡流场 混合坐标 混合层深度 |
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| Title | Subduction/obduction rate in the North Pacific diagnosed by an eddy-resolving model |
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