IOCAS-IR  > 海洋环流与波动重点实验室
M-2 Internal Tide Energetics and Behaviors in the Subpolar North Pacific
You, Jia1,2,3,4; Xu, Zhenhua1,2,3,4,5; Li, Oun6; Zhang, Peiwen1,2,3,4; Yin, Baoshu1,2,3,4,5; Hou, Yijun1,2,3,4,5
2023-05-01
发表期刊JOURNAL OF PHYSICAL OCEANOGRAPHY
ISSN0022-3670
卷号53期号:5页码:1269-1290
通讯作者Xu, Zhenhua([email protected])
摘要Energetic internal tides in the Pacific Ocean generated from multiple sources are the subject of many stud-ies, although the subpolar North Pacific (SNP) is known as a high-latitude hotspot that remains less explored. The present study is the first detailed investigation on M2 internal tide energetics and dynamics in the SNP by high-resolution numerical simulations. The M2 internal tides in the SNP mainly originate from the Aleutian Ridge (area-integrated 5.51 GW and av-eraged ;10-3 W m-2 of barotropic-to-baroclinic conversion rate), wherein the Amukta Pass is the most significant source. The Amukta Pass radiates northward 0.55 GW (averaged 2.3 kW m-1) to the Bering Sea and southward 1.40 GW (aver-aged 3.7 kW m-1) to the North Pacific. The subsequent south-north asymmetric radiation pattern is consistent with satel-lite altimeter detection. In the Bering basin, multiwave superposition in the near field between the Amukta Pass and adjacent sources generates two standing wave patterns. After approaching the Bering Sea slope, remote internal tides from Aleutian Ridge enhance local generation and dissipation. The dissipation field is relatively similar to the generation map, which is explained by the higher local dissipation efficiency q (>1/2) and the faster energy attenuation than in the midlati-tudes. The simulated dissipation rates compare favorably with the estimate from fine-scale parameterization, indicating the dominance of internal tidal mixing. The averaged dissipation rate in SNP is O(10-10) W kg-1, and the depth-integrated dis-sipation rates reach O(10-1) W m-2 near the Amukta Pass. It is important to understand the unique physics and dissipative process of high-latitude internal tides to fully characterize the redistribution of global tidal energy and associated mixing.
关键词Internal waves Ocean dynamics Tides North Paci fi c Ocean Ocean models
DOI10.1175/JPO-D-22-0032.1
收录类别SCI
语种英语
资助项目Strategic Pioneering Research Program of CAS; National Natural Science Foundation of China; National Key Research and Development Program of China[92058202]; National Key Research and Development Program of China[XDB42000000]; National Key Research and Development Program of China[92258301]; National Key Research and Development Program of China[42176244]; National Key Research and Development Program of China[42006031]; National Key Research and Development Program of China[XDA22050202]; High Performance Computing Center at the IOCAS
WOS研究方向Oceanography
WOS类目Oceanography
WOS记录号WOS:000990829900001
出版者AMER METEOROLOGICAL SOC
WOS关键词BAROCLINIC TIDES ; ENERGY FLUXES ; BERING-SEA ; OCEAN CIRCULATION ; MODEL ; DISSIPATION ; GENERATION ; RIDGE ; PROPAGATION ; CONVERSION
引用统计
被引频次:2[WOS]   [WOS记录]     [WOS相关记录]
文献类型期刊论文
条目标识符http://ir.qdio.ac.cn/handle/337002/183000
专题海洋环流与波动重点实验室
通讯作者Xu, Zhenhua
作者单位1.Chinese Acad Sci, Inst Oceanol, CAS Key Lab Ocean Circulat & Waves, Qingdao, Peoples R China
2.Pilot Natl Lab Marine Sci & Technol, Qingdao, Peoples R China
3.Chinese Acad Sci, Ctr Ocean Mega Sci, Qingdao, Peoples R China
4.Univ Chinese Acad Sci, Coll Earth & Planetary Sci, Beijing, Peoples R China
5.Chinese Acad Sci, Inst Oceanol, CAS Engn Lab Marine Ranching, Qingdao, Peoples R China
6.Polar Res Inst China, MNR Key Lab Polar Sci, Shanghai, Peoples R China
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You, Jia,Xu, Zhenhua,Li, Oun,et al. M-2 Internal Tide Energetics and Behaviors in the Subpolar North Pacific[J]. JOURNAL OF PHYSICAL OCEANOGRAPHY,2023,53(5):1269-1290.
APA You, Jia,Xu, Zhenhua,Li, Oun,Zhang, Peiwen,Yin, Baoshu,&Hou, Yijun.(2023).M-2 Internal Tide Energetics and Behaviors in the Subpolar North Pacific.JOURNAL OF PHYSICAL OCEANOGRAPHY,53(5),1269-1290.
MLA You, Jia,et al."M-2 Internal Tide Energetics and Behaviors in the Subpolar North Pacific".JOURNAL OF PHYSICAL OCEANOGRAPHY 53.5(2023):1269-1290.
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