IOCAS-IR  > 海洋环流与波动重点实验室
Mechanisms of tropical Pacific decadal variability
Capotondi, Antonietta1,2; McGregor, Shayne3,4; McPhaden, Michael J.5; Cravatte, Sophie6,7; Holbrook, Neil J.8,9; Imada, Yukiko10; Sanchez, Sara C.11; Sprintall, Janet12; Stuecker, Malte F.13,14; Ummenhofer, Caroline C.15,16; Zeller, Mathias17; Farneti, Riccardo18; Graffino, Giorgio19; Hu, Shijian20; Karnauskas, Kristopher B.1; Kosaka, Yu21; Kucharski, Fred18; Mayer, Michael22,23; Qiu, Bo13; Santoso, Agus16,24; Taschetto, Andrea S.16,24; Wang, Fan20; Zhang, Xuebin25; Holmes, Ryan M.26; Luo, Jing-Jia27; Maher, Nicola1,11,28,29; Martinez-Villalobos, Cristian30,31; Meehl, Gerald A.32; Naha, Rajashree3; Schneider, Niklas13,14; Stevenson, Samantha33; Sullivan, Arnold34; van Rensch, Peter3; Xu, Tongtong1,2
2023-10-18
Source PublicationNATURE REVIEWS EARTH & ENVIRONMENT
Pages16
Corresponding AuthorCapotondi, Antonietta(antonietta.capotondi@noaa.gov)
AbstractNaturally occurring tropical Pacific variations at timescales of 7-70 years - tropical Pacific decadal variability (TPDV) - describe basin-scale sea surface temperature (SST), sea-level pressure and heat content anomalies. Several mechanisms are proposed to explain TPDV, which can originate through oceanic processes, atmospheric processes or as an El Nino/Southern Oscillation (ENSO) residual. In this Review, we synthesize knowledge of these mechanisms, their characteristics and contribution to TPDV. Oceanic processes include off-equatorial Rossby waves, which mediate oceanic adjustment and contribute to variations in equatorial thermocline depth and SST; variations in the strength of the shallow upper-ocean overturning circulation, which exhibit a large anti-correlation with equatorial Pacific SST at interannual and decadal timescales; and the propagation of salinity-compensated temperature (spiciness) anomalies from the subtropics to the equatorial thermocline. Atmospheric processes include midlatitude internal variability leading to tropical and subtropical wind anomalies, which result in equatorial SST anomalies and feedbacks that enhance persistence; and atmospheric teleconnections from Atlantic and Indian Ocean SST variability, which induce winds conducive to decadal anomalies of the opposite sign in the Pacific. Although uncertain, the tropical adjustment through Rossby wave activity is likely a dominant mechanism. A deeper understanding of the origin and spectral characteristics of TPDV-related winds is a key priority.
DOI10.1038/s43017-023-00486-x
Indexed BySCI
Language英语
Funding ProjectCLIVAR ; Faculty of Science ; School of Earth Atmosphere and Environment at Monash University ; US CLIVAR ; NOAA Climate Program Office's Climate Variability and Predictability (CVP) ; Modeling, Analysis, Predictions and Projections (MAPP) programmes ; DOE ; Australian Government's National Environmental Science Program (NESP2) Climate Systems Hub ; IRD (French National Research Institute for Sustainable Development) ; NSF ; NOAA's Climate Program Office's MAPP programme ; NOAA's Global Ocean Monitoring and Observing Program ; Ministry of Education, Culture, Sports, Science and Technology, Japan ; Centre for Southern Hemisphere Oceans Research ; NASA Sea Level Change Science Program ; ARC Centre of Excellence for Climate Extremes ; NESP2 Climate Systems Hub ; Austrian Science Fund ; US Department of Energy ; US National Science Foundation (NSF) ; Proyecto ANID Fondecyt ; Australian Research Council ; James E. and Barbara V. Moltz Fellowship for Climate-Related Research[DE-SC0023228] ; Regional and Global Model Analysis component of the Earth and Environmental System Modelling Program of the US Department of Energy's Office of Biological and Environmental Research[FT160100162] ; Regional and Global Model Analysis component of the Earth and Environmental System Modelling Program of the US Department of Energy's Office of Biological and Environmental Research[DP200102329] ; National Center for Atmospheric Research ; joint JAMSTEC-IPRC Collaborative Research project JICore ; US Office of Naval Research through the Climate Resilience Collaborative at the University of Hawai'i at Mamacr;noa[AGS-2141728] ; US Office of Naval Research through the Climate Resilience Collaborative at the University of Hawai'i at Mamacr;noa[3200621] ; US Office of Naval Research through the Climate Resilience Collaborative at the University of Hawai'i at Mamacr;noa[DE-SC0022070] ; NOAA[AGS-2002083] ; U.S. Department of Energy (DOE)[DE-SC0023228]
WOS Research AreaEnvironmental Sciences & Ecology ; Geology
WOS SubjectEnvironmental Sciences ; Geosciences, Multidisciplinary
WOS IDWOS:001086343800002
PublisherSPRINGERNATURE
WOS KeywordSEA-SURFACE TEMPERATURE ; MERIDIONAL OVERTURNING CIRCULATION ; EL-NINO/SOUTHERN OSCILLATION ; NINO-SOUTHERN OSCILLATION ; OCEAN HEAT-CONTENT ; EQUATORIAL PACIFIC ; NORTH PACIFIC ; WIND STRESS ; CLIMATE VARIABILITY ; SUBTROPICAL CELLS
Citation statistics
Cited Times:8[WOS]   [WOS Record]     [Related Records in WOS]
Document Type期刊论文
Identifierhttp://ir.qdio.ac.cn/handle/337002/181611
Collection海洋环流与波动重点实验室
Corresponding AuthorCapotondi, Antonietta
Affiliation1.Univ Colorado, Cooperat Inst Res Environm Sci, Boulder, CO 80309 USA
2.NOAA, Phys Sci Lab, Boulder, CO 80305 USA
3.Monash Univ, Sch Earth Atmosphere & Environm, Clayton, Vic, Australia
4.Monash Univ, ARC Ctr Excellence Climate Extremes, Clayton, Vic, Australia
5.NOAA, Pacific Marine Environm Lab, Seattle, WA USA
6.Univ Toulouse, CNRS, LEGOS, CNES,IRD,UPS, Toulouse, France
7.IRD, Noumea, New Caledonia
8.Univ Tasmania, Inst Marine & Antarctic Studies, Hobart, Tas, Australia
9.Univ Tasmania, ARC Ctr Excellence Climate Extremes, Hobart, Tas, Australia
10.Univ Tokyo, Atmosphere & Ocean Res Inst, Chiba, Japan
11.Univ Colorado, Dept Atmospher & Ocean Sci, Boulder, CO USA
12.Univ Calif San Diego, Scripps Inst Oceanog, La Jolla, CA USA
13.Univ Hawaii Manoa, Sch Ocean & Earth Sci & Technol SOEST, Dept Oceanog, Honolulu, HI USA
14.Univ Hawaii Manoa, Int Pacific Res Ctr IPRC, Sch Ocean & Earth Sci & Technol SOEST, Honolulu, HI USA
15.Woods Hole Oceanog Inst, Dept Phys Oceanog, Woods Hole, MA USA
16.Univ New South Wales, ARC Ctr Excellence Climate Extremes, Sydney, NSW, Australia
17.GEOMAR Helmholtz Ctr Ocean Res, Kiel, Germany
18.Abdus Salam Int Ctr Theoret Phys, Trieste, Italy
19.Univ Reading, Natl Ctr Atmospher Sci, Dept Meteorol, Reading, England
20.Chinese Acad Sci, Inst Oceanol, CAS Key Lab Ocean Circulat & Waves, Qingdao, Peoples R China
21.Univ Tokyo, Res Ctr Adv Sci & Technol, Tokyo, Japan
22.European Ctr Medium Range Weather Forecasts, Res Dept, Reading, England
23.Univ Vienna, Dept Meteorol & Geophys, Vienna, Austria
24.Univ New South Wales, Climate Change Res Ctr, Sydney, NSW, Australia
25.CSIRO Environm, Climate Sci Ctr, Hobart, Tas, Australia
26.Univ Sydney, Sch Geosci, Sydney, NSW, Australia
27.Nanjing Univ Informat Sci & Technol, Inst Climate Applicat Res ICAR CIC FEMD, Nanjing, Peoples R China
28.Australian Natl Univ, Res Sch Earth Sci, Canberra, ACT, Australia
29.Australian Natl Univ, ARC Ctr Excellence Climate Extremes, Canberra, ACT, Australia
30.Univ Adolfo Ibanez, Fac Engn & Sci, Santiago, Chile
31.Data Observ Fdn, Santiago, Chile
32.Natl Ctr Atmospher Res, Boulder, CO USA
33.Univ Calif Santa Baranra, Bren Sch Environm Sci & Management, Santa Baranra, CA USA
34.CSIRO Oceans & Atmosphere, Aspendale, Vic, Australia
Recommended Citation
GB/T 7714
Capotondi, Antonietta,McGregor, Shayne,McPhaden, Michael J.,et al. Mechanisms of tropical Pacific decadal variability[J]. NATURE REVIEWS EARTH & ENVIRONMENT,2023:16.
APA Capotondi, Antonietta.,McGregor, Shayne.,McPhaden, Michael J..,Cravatte, Sophie.,Holbrook, Neil J..,...&Xu, Tongtong.(2023).Mechanisms of tropical Pacific decadal variability.NATURE REVIEWS EARTH & ENVIRONMENT,16.
MLA Capotondi, Antonietta,et al."Mechanisms of tropical Pacific decadal variability".NATURE REVIEWS EARTH & ENVIRONMENT (2023):16.
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