All Stories

  1. Last century warming over the Canadian Atlantic shelves linked to weak Atlantic Meridional Overturning Circulation
  2. Last century warming over the Canadian Atlantic shelves linked to weak Atlantic Meridional Overturning Circulation
  3. Weak overturning circulation and high Southern Ocean nutrient utilization maximized glacial ocean carbon
  4. Combined Effects of Atmospheric and Seafloor Iron Fluxes to the Glacial Ocean
  5. Carbon storage in the mid-depth Atlantic during millennial-scale climate events
  6. Core-top calibration of benthic carbon isotopes
  7. A cloud feedback emulator (CFE, version 1.0) for an intermediate complexity model
  8. Fate of the Atlantic Meridional Overturning Circulation: Strong decline under continued warming and Greenland melting
  9. Evidence for a biological pump driver of atmospheric CO2 rise during Heinrich Stadial 1
  10. The University of Victoria Cloud Feedback Emulator (UVic-CFE): cloud radiative feedbacks in an intermediate complexity model
  11. Stonger glacial ocean biological pump
  12. AMOC-emulator M-AMOC1.0 for uncertainty assessment of future projections
  13. Explicit Planktic Calcifiers in the University of Victoria Earth System Climate Model, Version 2.9
  14. Tides increased ice age ocean overturning circulation
  15. Southwest Atlantic water mass evolution during the last deglaciation
  16. Early deglacial Atlantic overturning decline and its role in atmospheric CO2 rise inferred from carbon isotopes (δ13C)
  17. Carbon isotopes support Atlantic meridional overturning circulation decline as a trigger for early deglacial CO2 rise
  18. Explicit planktic calcifiers in the University of Victoria Earth System Climate Model
  19. An improved parameterization of tidal mixing for ocean models
  20. Isotopic constraints on the pre-industrial oceanic nitrogen budget
  21. Biology and air–sea gas exchange controls on the distribution of carbon isotope ratios (δ13C) in the ocean
  22. An improved parameterization of tidal mixing for ocean models
  23. The acceleration of oceanic denitrification during deglacial warming
  24. Biology and air–sea gas exchange controls on the distribution of carbon isotope ratios (δ13C) in the ocean
  25. Isotopic constraints on the pre-industrial oceanic nitrogen budget
  26. A review of nitrogen isotopic alteration in marine sediments
  27. Response to Comment on "Climate Sensitivity Estimated from Temperature Reconstructions of the Last Glacial Maximum"
  28. Abrupt change in atmospheric CO2during the last ice age
  29. Calcium carbonate production response to future ocean warming and acidification
  30. Assessing the effects of ocean diffusivity and climate sensitivity on the rate of global climate change
  31. Global warming preceded by increasing carbon dioxide concentrations during the last deglaciation
  32. Changes in equatorial Pacific thermocline depth in response to Panamanian seaway closure: Insights from a multi-model study
  33. Climate Sensitivity Estimated from Temperature Reconstructions of the Last Glacial Maximum
  34. Nonlinearity of Carbon Cycle Feedbacks
  35. Ice-shelf collapse from subsurface warming as a trigger for Heinrich events
  36. Effects of Mountains and Ice Sheets on Global Ocean Circulation *
  37. Evaluation of a present-day climate simulation with a new coupled atmosphere-ocean model GENMOM
  38. What is the skill of ocean tracers in reducing uncertainties about ocean diapycnal mixing and projections of the Atlantic Meridional Overturning Circulation?
  39. Nitrogen isotope simulations show the importance of atmospheric iron deposition for nitrogen fixation across the Pacific Ocean
  40. Simulating the global distribution of nitrogen isotopes in the ocean
  41. Using tracer observations to reduce the uncertainty of ocean diapycnal mixing and climate-carbon cycle projections
  42. Correction to “Future changes in climate, ocean circulation, ecosystems, and biogeochemical cycling simulated for a business-as-usual CO2emission scenario until year 4000 AD”
  43. Glacial greenhouse-gas fluctuations controlled by ocean circulation changes
  44. Simulated 21st century's increase in oceanic suboxia by CO2-enhanced biotic carbon export
  45. Future changes in climate, ocean circulation, ecosystems, and biogeochemical cycling simulated for a business-as-usual CO2emission scenario until year 4000 AD
  46. Large fluctuations of dissolved oxygen in the Indian and Pacific oceans during Dansgaard-Oeschger oscillations caused by variations of North Atlantic Deep Water subduction
  47. Evaluation of Different Methods to Assess Model Projections of the Future Evolution of the Atlantic Meridional Overturning Circulation
  48. Preface
  49. Impact of the ocean's Overturning circulation on atmospheric CO2
  50. Simulating the impact of the Panamanian seaway closure on ocean circulation, marine productivity and nutrient cycling
  51. A global model of the marine ecosystem for long-term simulations: Sensitivity to ocean mixing, buoyancy forcing, particle sinking, and dissolved organic matter cycling
  52. Decline of the marine ecosystem caused by a reduction in the Atlantic overturning circulation
  53. The effect of Denmark Strait overflow on the Atlantic Meridional Overturning Circulation
  54. Model projections of the North Atlantic thermohaline circulation for the 21st century assessed by observations
  55. The Atlantic–Pacific Seesaw
  56. Modelling carbon cycle feedbacks during abrupt climate change
  57. Response to the comments by Peter Huybers
  58. Southern Ocean sea ice and radiocarbon ages of glacial bottom waters
  59. Atlantic deep circulation controlled by freshening in the Southern Ocean
  60. Ventilation of the North Atlantic Ocean during the Last Glacial Maximum: A comparison between simulated and observed radiocarbon ages
  61. Coupling of the hemispheres in observations and simulations of glacial climate change
  62. On the Role of Wind-Driven Sea Ice Motion on Ocean Ventilation
  63. Simulations of Heinrich Events in a coupled ocean-atmosphere-sea ice model
  64. Sensitivity of the thermohaline circulation to tropical and high latitude freshwater forcing during the last glacial-interglacial cycle
  65. Forcing of the deep ocean circulation in simulations of the Last Glacial Maximum
  66. Instability of Glacial Climate in a Model of the Ocean- Atmosphere-Cryosphere System
  67. A Seasonally Forced Ocean–Atmosphere Model for Paleoclimate Studies
  68. Enhanced Atlantic freshwater export during El Niño
  69. The Stability of the Thermohaline Circulation in Global Warming Experiments