Atlantic Meridional Overturning Circulation (AMOC)
node · earth · Atlantic Ocean
The Atlantic limb of the density-driven circulation: warm, salty water moving north near the surface, losing heat to the atmosphere at high latitudes, sinking, and returning south at depth as North Atlantic Deep Water. It is the best-observed overturning cell on Earth because a single mooring array has watched it continuously at one latitude for over twenty years. Across April 2004 to January 2023 the RAPID array at 26.5°N gives a mean overturning maximum of 17.0 Sv with a standard deviation of 2.8 Sv, and a weakening trend of 1.0 [0.4–1.6] Sv per decade. That trend is small against the variability, which is why the argument about whether the AMOC is declining is an argument about signal and noise as much as about physics.
Read in · 1
Evidence · 2
Timeline
No dated observations are stored for this object. Atlas shows what was observed and when — it does not infer a history.
Connections · 1
- Thermohaline Circulationpart_of
Assembled narrative · 1
Assembled from 31 blocks · 2 evidence · 54 related
- Story
- The Atlantic limb of the density-driven circulation: warm, salty water moving north near the surface, losing heat to the atmosphere at high latitudes, sinking, and returning south at depth as North Atlantic Deep Water. It is the best-observed overturning cell on Earth because a single mooring array has watched it continuously at one latitude for over twenty years. Across April 2004 to January 2023 the RAPID array at 26.5°N gives a mean overturning maximum of 17.0 Sv with a standard deviation of 2.8 Sv, and a weakening trend of 1.0 [0.4–1.6] Sv per decade. That trend is small against the variability, which is why the argument about whether the AMOC is declining is an argument about signal and noise as much as about physics.
- Knowledge
- Thermohaline Circulation
- Atlantic Meridional Overturning Circulation (AMOC)
- Connections
- Gulf Stream
- Thermohaline Circulation
- Antarctic Circumpolar Current (ACC)
- North Atlantic Deep Water (NADW)
- RAPID-MOCHA-WBTS Array at 26.5°N
- Overturning in the Subpolar North Atlantic Program (OSNAP)
- Meridional Ocean Heat Transport
- The RAPID array begins continuous AMOC measurement at 26.5°N
- OSNAP moves the engine room out of the Labrador Sea
- IPCC AR6 assesses AMOC decline as very likely and collapse as unlikely this century
- A statistical early-warning analysis puts an AMOC collapse mid-century
- A physics-based early warning signal is proposed
- Twenty-two years of continuous AMOC observation
- Atlantic Meridional Overturning Circulation (AMOC)
- Coastal and Equatorial Upwelling
- Antarctic Bottom Water (AABW)
- Southern Ocean
- Argo Profiling Float Array
- Wallace Broecker
- The great ocean conveyor is drawn
- The Argo design array is completed
- IPCC AR6 assesses AMOC decline as very likely and collapse as unlikely this century
- Evidence
- The RAPID array at 26.5°N gives a mean AMOC of 17.0 Sv (s.d. 2.8 Sv) for April 2004 to January 2023 and a weakening of 1.0 [0.4–1.6] Sv per decade; the trend is not expected to exceed a signal-to-noise ratio of 2 until the 2040s. Read via search summary; the paper itself could not be fetched because the publisher domain is blocked to this run.
- The AMOC will very likely decline over the twenty-first century under all SSP scenarios, with medium confidence that the decline will not involve an abrupt collapse before 2100. The assessment language is quoted from secondary reporting of the chapter; the chapter itself was not fetched.
Observed changes · 0
No public Signals are attached to this object. Signals show what changed and when it was observed — never a direction or a rank.
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