Article
Environmental Sciences
Liyuan Fang, Kai Ma, Chuanyu Liu, Xiaowei Wang, Fan Wang
Summary: This study analyzes the 3D structure of the equatorial mode of tropical instability waves (TIWs) using high-resolution ocean reanalysis data and examines its temperature and shear distribution related to mixing mechanisms. The results show that temperature structure plays a crucial role in stratification pattern, while shear contributes less to instability and mixing. Specifically, in the northern (southern) part of the clockwise (anticlockwise) phase of the equatorial TIWs, a larger shear squared is observed, potentially leading to shear instability and mixing.
FRONTIERS IN MARINE SCIENCE
(2023)
Article
Geosciences, Multidisciplinary
L. Maillard, J. Boucharel, M. F. Stuecker, F. -F. Jin, L. Renault
Summary: This study investigates the effects of tropical instability waves (TIWs) on the seasonal cycle of the eastern Pacific Ocean. The results show that TIWs warm the equatorial waters and reduce the amplitude of the seasonal cycle in upper ocean temperatures. Additionally, TIWs stabilize the upper part of the Equatorial Undercurrent (EUC) and prevent unrealistic re-intensification.
GEOPHYSICAL RESEARCH LETTERS
(2022)
Article
Oceanography
D. B. Whitt, D. A. Cherian, R. M. Holmes, S. D. Bachman, R-C Lien, W. G. Large, J. N. Moum
Summary: The study analyzes mixing and deep-cycle turbulence in the Pacific cold tongue region, finding that subsurface turbulent fluxes vary with geographical location and season, and are correlated with surface heat fluxes. The results show that intense deep-cycle turbulence occurs frequently in the region of 0 degrees, 140 degrees W and 3 degrees N.
JOURNAL OF PHYSICAL OCEANOGRAPHY
(2022)
Article
Meteorology & Atmospheric Sciences
Xian Wu, Yuko M. Okumura, Pedro N. DiNezio, Stephen G. Yeager, Clara Deser
Summary: This study investigates the mean-state bias and associated forecast errors of the El Nino-Southern Oscillation (ENSO) using the Community Earth System Model, version 1. The forecasts show a strong bias in the equatorial Pacific cold tongue, which is caused by a combination of the model's climatological bias, initialization imbalance, and errors in initial ocean data. This bias affects the pattern, amplitude, and duration of ENSO in the forecasts by altering ocean-atmosphere feedbacks. The forecast errors subsequently degrade predictions of atmospheric teleconnections, land surface air temperature, and rainfall anomalies over the Northern Hemisphere.
JOURNAL OF CLIMATE
(2022)
Article
Oceanography
Yang Li, Quanliang Chen, Nan Xing, Zhigang Cheng, Yulei Qi, Fan Feng, Minggang Li
Summary: Our research reveals a significant trend in the weakening of the zonal sea surface temperature gradient in the equatorial Atlantic from 1900 to 2010. This trend is closely linked to the tropical Pacific cold tongue mode, showing a clear pattern of warming in the west and cooling in the east. The weakening trend is induced by ocean dynamical feedback in response to global warming, highlighting the potential impact of global warming on the equatorial Atlantic zonal SST gradient.
JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS
(2021)
Article
Geosciences, Multidisciplinary
R. Pinkel, S. Nguyen, J. A. Smith, A. J. Lucas, B. D. Reineman, A. F. Waterhouse
Summary: Strong vertical shears occur in the upper Equatorial Ocean due to the trade winds driving the South Equatorial Current westward above the Equatorial Undercurrent. The maintenance of speed-differential between the currents requires a large effective viscosity or vertical momentum transport. The analysis of data from the 2012 EquatorMix Experiment reveals the presence of energetic internal waves with a wavelength of approximately 600 m above the Undercurrent, which are excited by nocturnal sea surface convection and maintained by near-surface critical layer over-reflection. These waves contribute to the necessary momentum transport to balance the large-scale forcing of the equatorial current system.
GEOPHYSICAL RESEARCH LETTERS
(2023)
Article
Oceanography
Anna-Lena Deppenmeier, Frank O. Bryan, William S. Kessler, LuAnne Thompson
Summary: The cold tongue in the tropical Pacific Ocean plays a major role in the global climate system, affecting surface temperatures through processes such as water mass transformation and vertical mixing. During El Niño events, reduced vertical mixing weakens cooling, while during La Niña periods, enhanced vertical mixing leads to strong cooling processes.
JOURNAL OF PHYSICAL OCEANOGRAPHY
(2021)
Article
Oceanography
A. M. Santos-Ferreira, J. C. B. Da Silva, B. St-Denis, D. Bourgault, L. R. M. Maas
Summary: The equatorial cold tongue in the Pacific Ocean has been intensively studied in recent decades due to its important role in air-sea interactions and climate issues. This study presents satellite observations of internal solitary waves (ISWs) in the Pacific cold tongue, revealing their characteristics and connection with buoyant gravity currents. A numerical model confirms the continuous generation of resonantly generated nonlinear internal waves at the fronts of advancing gravity currents.
JOURNAL OF PHYSICAL OCEANOGRAPHY
(2023)
Article
Oceanography
Wei-Bang He, Yang Yang, X. San Liang
Summary: It is believed that both barotropic and baroclinic instabilities contribute to the variability of tropical instability waves (TIWs) in the equatorial Pacific Ocean. However, the coupling mechanisms between different meridional TIW modes and their vertical connections are still unclear. Through the use of multiscale window transform (MWT) and MWT-based theory, this study investigates the coupling mechanisms between the Yanai-mode and Rossby-mode TIWs. The results reveal that barotropic instability is the primary energy source for Yanai-mode TIWs in the subsurface layer, while baroclinic instability dominates the generation of eddy kinetic energy (EKE) for Rossby-mode TIWs. In the surface layer, nonlocal mechanisms, such as pressure work, modulate the two TIW modes and couple them in both meridional and vertical directions, leading to coherence between EKE in different vertical layers and regions. The seasonal variations of these mechanisms determine the seasonal cycles of TIWs in the equatorial Pacific Ocean.
DEEP-SEA RESEARCH PART I-OCEANOGRAPHIC RESEARCH PAPERS
(2023)
Article
Multidisciplinary Sciences
John C. H. Chiang, Alyssa R. Atwood, Daniel J. Vimont, Paul A. Nicknish, William H. G. Roberts, Clay R. Tabor, Anthony J. Broccoli
Summary: The annual cycle of sea surface temperature in the Pacific cold tongue is not only driven by Earth's axial tilt (tilt effect) but also by the variation in Earth-Sun distance caused by orbital eccentricity (distance effect). These two effects lead to a complex evolution of the net seasonality over time. This finding calls for a reassessment of our understanding of the annual cycle of the Pacific cold tongue.
Article
Meteorology & Atmospheric Sciences
Weixuan Xu, Jung-Eun Lee
Summary: The study suggests that current climate models overestimate precipitation and temperature over the southeast Pacific, with the Andes playing a key role in maintaining the climate in that region. Low-resolution climate models fail to accurately represent the effects of the Andes as a barrier in the southeast Pacific Ocean.
JOURNAL OF CLIMATE
(2021)
Article
Meteorology & Atmospheric Sciences
Ingo Richter, Malte F. Stuecker, Naoya Takahashi, Niklas Schneider
Summary: Variations of sea-surface temperature in the subtropical North Pacific, known as the North Pacific Meridional Mode, may not be accurately captured by the current statistical technique of maximum covariance analysis. This raises the need for refined tools to diagnose variability in this region.
NPJ CLIMATE AND ATMOSPHERIC SCIENCE
(2022)
Article
Environmental Sciences
Young Ho Ko, Geun-Ha Park, Dongseon Kim, Tae-Wook Kim
Summary: This study investigates the interannual variations in seawater CO2 partial pressure in the northwestern subtropical Pacific Ocean during the months of August to October with frequent tropical cyclone events. It found that the variations in pCO2 were related to vertical mixing likely caused by TC activity, leading the region to transition from a CO2 source to a CO2 sink during the TC season. In the southern part of the study area, smaller pCO2 variations were observed, possibly due to deeper mixed layer depth and a more homogenous CO2 profile in the tropical region.
FRONTIERS IN MARINE SCIENCE
(2021)
Article
Environmental Sciences
Duhan Shen, Jianing Wang, Zhiyu Liu, Fan Wang
Summary: Diapycnal mixing in the upper western equatorial Pacific (WEP) is important for tropical air-sea interactions and the global climate system. The WEP is unique in water masses from both hemispheres and multi-scale processes, creating a complex mixing regime that needs to be fully characterized by observations.
FRONTIERS IN MARINE SCIENCE
(2023)
Article
Oceanography
D. A. Cherian, D. B. Whitt, R. M. Holmes, R-C Lien, S. D. Bachman, W. G. Large
Summary: The study shows that deep-cycle turbulence occurs both on and off the equator in the cold tongue region, modulated by tropical instability waves. Further observational campaigns are needed to characterize the modulation of deep-cycle turbulence by TIWs both on and off the equator.
JOURNAL OF PHYSICAL OCEANOGRAPHY
(2021)
Article
Meteorology & Atmospheric Sciences
Matthew P. Couldrey, Jonathan M. Gregory, Xiao Dong, Oluwayemi Garuba, Helmuth Haak, Aixue Hu, William J. Hurlin, Jiangbo Jin, Johann Jungclaus, Armin Koehl, Hailong Liu, Sayantani Ojha, Oleg A. Saenko, Abhishek Savita, Tatsuo Suzuki, Zipeng Yu, Laure Zanna
Summary: The effect of anthropogenic climate change in the ocean is challenging to project due to the different responses of atmosphere-ocean general circulation models (AOGCMs). This study focuses on the changes in the Atlantic Meridional Overturning Circulation (AMOC), ocean heat content (Delta OHC), and the spatial pattern of ocean dynamic sea level (Delta zeta). The results show that the weakening of AMOC is mainly caused by the North Atlantic heat flux perturbation, and further weakened by a positive coupled heat flux feedback. The AMOC decline has significant impacts on the warming of the South Atlantic-Southern Ocean interface.
Article
Meteorology & Atmospheric Sciences
Lijing Cheng, John Abraham, Kevin E. Trenberth, John Fasullo, Tim Boyer, Michael E. Mann, Jiang Zhu, Fan Wang, Ricardo Locarnini, Yuanlong Li, Bin Zhang, Fujiang Yu, Liying Wan, Xingrong Chen, Licheng Feng, Xiangzhou Song, Yulong Liu, Franco Reseghetti, Simona Simoncelli, Viktor Gouretski, Gengxin Chen, Alexey Mishonov, Jim Reagan, Guancheng Li
Summary: Changes in ocean heat content, salinity, and stratification serve as critical indicators for Earth's energy and water cycles, which have been significantly impacted by human activities and greenhouse gas emissions. The year 2022 witnessed the highest ocean heat content on record, surpassing the previous maximum. The salinity-contrast index also reached a record high, indicating an intensification of the global hydrological cycle. Regional oceanic changes were driven by a strong La Nina event, and the global upper-ocean stratification continued to increase, ranking among the top seven in 2022.
ADVANCES IN ATMOSPHERIC SCIENCES
(2023)
Article
Geosciences, Multidisciplinary
Yan Du, Fan Wang, Tianyu Wang, Weiwei Liu, Linlin Liang, Ying Zhang, Yunfan Chen, Jiaxing Liu, Wei Wu, Kefu Yu, Jing Zhang
Summary: The Indo-Pacific Convergence Zone is a complex ocean dynamical system that links basin-scale circulations in the Pacific and Indian Oceans. It plays a crucial role in regulating atmospheric circulations and global climate events. Additionally, it has direct impacts on biodiversity and ecological processes.
EARTH-SCIENCE REVIEWS
(2023)
Article
Meteorology & Atmospheric Sciences
Chathurika Wickramage, Armin Koehl, Johann Jungclaus, Detlef Stammer
Summary: This study investigates the dependence of future regional sea level changes on ocean model resolution. The results indicate that each run reproduces previously identified large-scale dynamic sea level change patterns, but substantial sensitivity of the projected changes can be found on a regional to local scale with respect to model resolution. Sea level changes are enhanced in regions capturing mesoscale processes, such as the North Atlantic subtropical region, the Kuroshio region, and the Arctic Ocean. Smaller yet significant sea level changes are found in the Southern Ocean and the North Atlantic subpolar region. This study suggests that low-resolution sea level projections should be interpreted with care in regions with major differences revealed here.
JOURNAL OF CLIMATE
(2023)
Article
Meteorology & Atmospheric Sciences
Jing Duan, Yuanlong LI, Lijing Cheng, Pengfei Lin, Fan Wang
Summary: The heat content in the Indian Ocean has been increasing due to anthropogenic greenhouse warming. The storage location and method of anthropogenic heat in the Indian Ocean are not fully understood yet. Analysis of various datasets reveals a spatial pattern of ocean heat content trend, with enhanced warming in the subtropical southern Indian Ocean but weak to minimal warming in the tropical Indian Ocean. Surface wind changes play a crucial role in shaping this pattern.
JOURNAL OF CLIMATE
(2023)
Article
Oceanography
Xin Liu, Armin Koehl, Detlef Stammer
Summary: This study investigates regional freshwater content (FWC) changes in the Atlantic Ocean from 1961 to 2018 using the GECCO3 ocean synthesis. The study finds that both the surface freshwater flux and net freshwater transport across region boundaries contribute to FWC variability. Surface flux is more important on longer time scales, especially in the tropics, while horizontal transport fluctuations dominate FWC changes on shorter time scales in mid and high latitudes.
JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS
(2023)
Article
Oceanography
Hongyang Lin, Siyu Xu, Zhiyu Liu, Jianyu Hu, Fangtao Zhang, Zhiyong Cao
Summary: This study uses high-resolution, cross-frontal towed measurements to investigate temperature-salinity (T-S) compensation and its scale dependence in the Taiwan Strait. It is found that T-S compensation occurs within the interfacing zone, with temperature and salinity getting more (less) compensated at smaller scales in the S-dominated (T-dominated) frontal zone. The restratification-cooling mechanism, induced by submesoscale instabilities, explains the observed density compensating features on both flanks of the transition zone.
JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS
(2023)
Article
Environmental Sciences
Duhan Shen, Jianing Wang, Zhiyu Liu, Fan Wang
Summary: Diapycnal mixing in the upper western equatorial Pacific (WEP) is important for tropical air-sea interactions and the global climate system. The WEP is unique in water masses from both hemispheres and multi-scale processes, creating a complex mixing regime that needs to be fully characterized by observations.
FRONTIERS IN MARINE SCIENCE
(2023)
Article
Oceanography
Hang Zhang, Jianing Wang, Fan Wang, Zhixiang Zhang, Qiang Ma
Summary: The deep channel north of New Guinea is crucial for the upper deep branches of the Pacific meridional overturning circulation, which plays a significant role in the ocean's climate and biogeochemical systems. It carries mixed water with a potential temperature over 1.2 degrees-2.2 degrees C and exhibits seasonal variability.
JOURNAL OF PHYSICAL OCEANOGRAPHY
(2023)
Article
Oceanography
Qinbo Xu, Chun Zhou, Linlin Zhang, Fan Wang, Wei Zhao, Dunxin Hu
Summary: The deep western boundary current (DWBC) in the Northern Philippine Sea deep basin was studied using mooring data from January 2018 to May 2020. The DWBC flows southward with an average velocity of 1.18 cm/s at a depth of 3050 m. Significant intraseasonal and seasonal variations were observed, with the most prominent intraseasonal peak at approximately 120 days. The DWBC intensifies in summer/autumn and weakens in winter/spring, corresponding to the seasonal variation of ocean bottom pressure.
JOURNAL OF PHYSICAL OCEANOGRAPHY
(2023)
Article
Multidisciplinary Sciences
Fenzhen Su, Rong Fan, Fengqin Yan, Michael Meadows, Vincent Lyne, Po Hu, Xiangzhou Song, Tianyu Zhang, Zenghong Liu, Chenghu Zhou, Tao Pei, Xiaomei Yang, Yunyan Du, Zexun Wei, Fan Wang, Yiquan Qi, Fei Chai
Summary: Analysis of big Argo data reveals that only 3.8% of the mid-depth ocean circulation can be considered accurately modeled, compromising the representation of global ocean circulation near 1000-m depth. This has significant implications for climate change assessment, as the mid-depth ocean circulation is critically linked to global climate system changes. The study suggests improvements in forecasting, stochastic model representation, and observations of ocean currents to address these inaccuracies.
NATURE COMMUNICATIONS
(2023)
Article
Geosciences, Multidisciplinary
Gengbin Liu, Zhiwu Chen, Huaihao Lu, Zhiyu Liu, Qian Zhang, Qingyou He, Yinghui He, Jiexin Xu, Yankun Gong, Shuqun Cai
Summary: Ocean circulations require forward energy cascades from large to small scales, and mesoscale eddies are the dominant reservoir of kinetic energy in the oceans. However, the interaction between these eddies and near-inertial waves may contribute significantly to the forward energy cascade process. Previous studies underestimated the eddy-to-NIW energy transfer, but new calculations from global drifter observations suggest that it may be about 13% of the near-inertial wind work, providing a useful reference for future studies.
GEOPHYSICAL RESEARCH LETTERS
(2023)
Article
Oceanography
Kai Ge, Yuanlong Li, Yilong Lyu, Pengfei Lin, Lijing Cheng, Fan Wang
Summary: Sea surface salinity has shown a trend of increased salinity in salty regions and increased freshness in fresh regions in the past few decades. Changes in precipitation rate have been identified as the main driver for salinity trends in most tropical and subtropical regions. Wind-driven ocean dynamics and evaporation have secondary contributions. The relationship between sea surface salinity and freshwater fluxes varies by region, with many regions showing opposite trends in salinity and freshwater fluxes.
JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS
(2023)
Article
Oceanography
Zhongwei Yuan, Thomas J. Browning, Chuanjun Du, Hui Shen, Lei Wang, Yifan Ma, Zong-Pei Jiang, Zhiyu Liu, Kuanbo Zhou, Shuh-Ji Kao, Minhan Dai
Summary: This study investigates the spatial variability, temporal evolution, and impact of mesoscale eddies on upper ocean biogeochemistry in the subtropical Northwest Pacific. The results show that the upper layer of the eddy has lower phosphate concentrations within its core, which can be attributed to elevated N-2 fixation driven by enhanced subsurface iron supply. The presence of eddies affects the phytoplankton biomass in the lower euphotic zone but does not significantly impact the total phytoplankton biomass across the entire euphotic zone. With an anticipated increase in the frequency of cyclonic eddies in the subtropical North Pacific, their role in regulating nutrient biogeochemistry and productivity of the region may become more important.
JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS
(2023)
Review
Oceanography
Jie Ma, Zhanqing Zhang, Shijian Hu, Cesar Villanoy, Xinying Guo, Fan Wang, Dunxin Hu
Summary: The interannual variability of the Kuroshio and Luzon Undercurrent (LUC) east of the Luzon Island is examined using observations from a moorings during December 2010-October 2012 and three moorings during January 2018-May 2020 deployed at 18 degrees N. Measurements from acoustic Doppler current profiler (ADCP) equipped on the moorings indicate that the interannual variations of upper-layer Kuroshio and lower-layer LUC were in phase. The interannual variability is strong in the Kuroshio but weakens substantially in the LUC. A proxy of the Kuroshio and LUC based on sea level slope is developed and validated by comparing the ADCP and satellite altimeter measurements. The proxy during 1993-2020 shows that the interannual sea level slope across the Kuroshio is primarily associated with sea level fluctuations on its eastern flank. Diagnostic analysis and nu-merical sensitivity experiments using a simplified ocean model indicate that the wind forcing in the subtropical northwestern Pacific Ocean played an essential role in the interannual variability of Kuroshio and LUC's strength and water mass properties during the observation periods in 2011 and 2018-2020, although the tropical winds dominated the interannual variability of the two boundary currents during most time of the past three decades (1993-2020). The mooring observations show that the subsurface water mass in the LUC at the depth of about 650-800 m experienced a considerable freshening event from July 2019 until at least January 2020 due to abnormally strong subtropical wind forcing.
PROGRESS IN OCEANOGRAPHY
(2023)