All Stories

  1. Benguela Upwelling Filaments Are a Significant Pathway of New Nutrients to the South Atlantic Subtropical Gyre
  2. nextGEMS: entering the era of kilometer-scale Earth system modeling
  3. Seasonal productivity of the equatorialAtlantic shaped by distinct wind-drivenprocesses
  4. Variability of the Western Boundary Current System at 11°S
  5. BOWTIE: A ship-based field campaign to explore the inner life of the Atlantic ITCZ
  6. Impact of Submesoscale Dynamics and Turbulent Mixing on the Senegalo-Mauritanian Upwelling System
  7. Sensitivity of the tropical Atlantic to vertical mixing in two ocean models (ICON-O v2.6.6 and FESOM v2.5)
  8. Toward an integrated pantropical ocean observing system
  9. Seasonal productivity of the equatorial Atlantic shaped by distinct wind-driven processes
  10. Drivers and impact of the 2021 extreme warm event in the tropical Angolan upwelling system
  11. ATOMIX benchmark datasets for dissipation rate measurements using shear probes
  12. Using NIW Observations to Assess Mixed Layer Parameterizations: A Case Study in the Tropical Atlantic
  13. Best practices recommendations for estimating dissipation rates from shear probes
  14. Coastal trapped waves and tidal mixing control primary production in the tropical Angolan upwelling system
  15. Turbulent diapycnal fluxes as a pilot Essential Ocean Variable
  16. Nitrogen fixation rates in the Guinea Dome and the equatorial upwelling regions in the Atlantic Ocean
  17. Wind Dependencies of Deep Cycle Turbulence in the Equatorial Cold Tongues
  18. Physical processes and biological productivity in the upwelling regions of the tropical Atlantic
  19. Energetics of eddy–mean flow interactions in the deep western boundary current off the northeastern coast of Brazil
  20. Seasonal cycle of sea surface temperature in the tropical Angolan Upwelling System
  21. Physical processes in the upwelling regions of the tropical Atlantic
  22. Seasonal cycle of sea surface temperature in the tropical Angolan upwelling system
  23. Tropical Instability Waves and Wind‐Forced Cross‐Equatorial Flow in the Central Atlantic Ocean
  24. Sediment Release in the Benguela Upwelling System Dominates Trace Metal Input to the Shelf and Eastern South Atlantic Ocean
  25. Deep Cycle Turbulence in Atlantic and Pacific Cold Tongues
  26. Seasonal mixed layer heat budget in coastal waters off Angola
  27. Deep cycle turbulence in Atlantic and Pacific cold tongues
  28. Organic Matter Supply and Utilization in Oxygen Minimum Zones
  29. Atlantic Equatorial Undercurrent intensification counteracts warming-induced deoxygenation
  30. Climate-Biogeochemistry Interactions in the Tropical Ocean: Data collection and legacy
  31. Supplementary material to "Climate-Biogeochemistry Interactions in the Tropical Ocean: Data collection and legacy"
  32. Three‐Dimensional Numerical Simulations of Internal Tides in the Angolan Upwelling Region
  33. Influence of intraseasonal eastern boundary circulation variability on hydrography and biogeochemistry off Peru
  34. Three Dimensional Numerical Simulations of Internal Tides in the Angolan Upwelling Region
  35. Effects of <sup>238</sup>U variability and physical transport on water column <sup>234</sup>Th downward fluxes in the coastal upwelling system off Peru
  36. Salinity Biases and the Variability of the Atlantic Meridional Overturning Circulation in GFDL-CM3
  37. Surface cooling caused by rare but intense near-inertial wave induced mixing in the tropical Atlantic
  38. Three Dimensional Numerical Simulations of Internal Tides at the Continental Slope and Shelf off Angola
  39. Decadal variability of circulation and oxygen in the equatorial Atlantic
  40. Internal Wave Generation in Tropical Upwelling Regions: the Angolan and Peruvian Shelves
  41. Observational evidence of diapycnal upwelling in a bottom enhanced mixing environment
  42. Effects of <sup>238</sup>U variability and physical transport on water column <sup>234</sup>Th downward fluxes in the coastal upwelling system off Peru
  43. Supplementary material to "Effects of <sup>238</sup>U variability and physical transport on water column <sup>234</sup>Th downward fluxes in the coastal upwelling system off Peru"
  44. Vertical Turbulent Cooling of the Mixed Layer in the Atlantic ITCZ and Trade Wind Regions
  45. Controls on redox-sensitive trace metals in the Mauritanian oxygen minimum zone
  46. Global Perspectives on Observing Ocean Boundary Current Systems
  47. Influence of intraseasonal eastern boundary circulation variability on hydrography and biogeochemistry off Peru
  48. Gas exchange estimates in the Peruvian upwelling regime biased by multi-day near-surface stratification
  49. Diapycnal dissolved organic matter supply into the upper Peruvian oxycline
  50. The Tropical Atlantic Observing System
  51. PIRATA: A Sustained Observing System for Tropical Atlantic Climate Research and Forecasting
  52. Remote and local drivers of oxygen and nitrate variability in the shallow oxygen minimum zone off Mauritania in June 2014
  53. A Dynamic Flight Model for Slocum Gliders and Implications for Turbulence Microstructure Measurements
  54. Causes and evolution of the southeastern tropical Atlantic warm event in early 2016
  55. Controls on redox-sensitive trace metals in the Mauritanian oxygen minimum zone
  56. Supplementary material to "Controls on redox-sensitive trace metals in the Mauritanian oxygen minimum zone"
  57. Seasonal Variability of the Mauritania Current and Hydrography at 18°N
  58. Gas exchange estimates in the Peruvian upwelling regime biased by multi-day near-surface stratification
  59. H2S events in the Peruvian oxygen minimum zone facilitate enhanced dissolved Fe concentrations
  60. Eastern Boundary Circulation and Hydrography Off Angola: Building Angolan Oceanographic Capacities
  61. Diapycnal dissolved organic matter supply into the upper Peruvian oxycline
  62. Remote and local drivers of oxygen and nitrate variability in the shallow oxygen minimum zone off Mauritania in June 2014
  63. Evidence for the Maintenance of Slowly Varying Equatorial Currents by Intraseasonal Variability
  64. Role of Equatorial Basin-Mode Resonance for the Seasonal Variability of the Angola Current at 11°S
  65. The Angola Current: Flow and hydrographic characteristics as observed at 11°S
  66. Nitrous oxide during the onset of the Atlantic cold tongue
  67. Depletion of oxygen, nitrate and nitrite in the Peruvian oxygen minimum zone cause an imbalance of benthic nitrogen fluxes
  68. Thermal small steps staircase and layer migration in the Atlantis II Deep, Red Sea
  69. Peruvian sediments as recorders of an evolving hiatus for the last 22 thousand years
  70. Thermocline mixing and vertical oxygen fluxes in the stratified central North Sea
  71. The formation of a subsurface anticyclonic eddy in the P eru‐ C hile U ndercurrent and its impact on the near‐coastal salinity, oxygen, and nutrient distributions
  72. Coastal upwelling off Peru and Mauritania inferred from helium isotope disequilibrium
  73. Interannual to decadal changes in the western boundary circulation in the Atlantic at 11°S
  74. The squat lobster Pleuroncodes monodon tolerates anoxic “dead zone” conditions off Peru
  75. Nitrate and Nitrite Variability at the Seafloor of an Oxygen Minimum Zone Revealed by a Novel Microfluidic In-Situ Chemical Sensor
  76. Nitrogen Fuelling of the Pelagic Food Web of the Tropical Atlantic
  77. Turbulence and finestructure in a deep ocean channel with sill overflow on the mid-Atlantic ridge
  78. Organic carbon production, mineralisation and preservation on the Peruvian margin
  79. On the role of circulation and mixing in the ventilation of oxygen minimum zones with a focus on the eastern tropical North Atlantic
  80. Mixed layer heat and salinity budgets during the onset of the 2011 Atlantic cold tongue
  81. Diapycnal heat flux and mixed layer heat budget within the Atlantic Cold Tongue
  82. Diapycnal oxygen supply to the tropical North Atlantic oxygen minimum zone
  83. Seasonal and regional variability of upper ocean diapycnal heat flux in the Atlantic cold tongue
  84. Factors influencing the distribution of epibenthic megafauna across the Peruvian oxygen minimum zone
  85. Diapycnal diffusivity at the upper boundary of the tropical North Atlantic oxygen minimum zone
  86. Sea-to-air and diapycnal nitrous oxide fluxes in the eastern tropical North Atlantic Ocean
  87. Interannual atmospheric variability forced by the deep equatorial Atlantic Ocean
  88. Tidal-induced mixing and diapycnal nutrient fluxes in the Mauritanian upwelling region
  89. A one-dimensional modeling study of the diurnal cycle in the equatorial Atlantic at the PIRATA buoys during the EGEE-3 campaign
  90. Upwelling and associated heat flux in the equatorial Atlantic inferred from helium isotope disequilibrium
  91. Equatorial upper-ocean dynamics and their interaction with the West African monsoon
  92. Oxygen tongues and zonal currents in the equatorial Atlantic
  93. Stacked jets in the deep equatorial Atlantic Ocean
  94. Deep Labrador Current and its variability in 1996–2005
  95. Variability of the Deep Western Boundary Current east of the Grand Banks
  96. The Shallow and Deep Western Boundary Circulation of the South Atlantic at 5°–11°S
  97. Upper ocean circulation in the western tropical Atlantic in boreal fall 2000
  98. Break-up of the Atlantic deep western boundary current into eddies at 8° S
  99. Boundary Circulation at the Exit of the Labrador Sea
  100. Circulation and Deep-Water Export at the Western Exit of the Subpolar North Atlantic
  101. Intraseasonal variability in the southwestern Arabian Sea and its relation to the seasonal circulation
  102. Surveying the Upper Ocean with the Ocean Surveyor: A New Phased Array Doppler Current Profiler
  103. The zonal currents and transports at 35°W in the tropical Atlantic
  104. Erratum to: The shallow overturning circulation of the Indian Ocean
  105. Equatorial Deep Jets and Abyssal Mixing in the Indian Ocean
  106. The shallow overturning circulation of the Indian Ocean
  107. Abyssal circulation in the Somali Basin
  108. Annual Rossby waves in the Arabian Sea from TOPEX/POSEIDON altimeter and in situ data