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Search 3,721 documents across 34 fields — every claim tier-rated by evidence

3,721 Documents 34 Sections 43,625 Citations 34,852 Keywords Indexed 4 Evidence Tiers

3,633 are the core, quality-scored corpus (34 lettered sections — see How We Work); the remaining 88 are cross-corpus synthesis documents (68 InterDocs, 12 Connections, 8 Theories) also indexed here.

41 results for "Atlantic Meridional Overturning Circulation" — page 1 of 3

ZF_1_01 Verified Oceanography

ZF_1_01 — Physical Oceanography: Thermohaline Circulation, Currents, and ENSO

Physical oceanography studies the motion, properties, and dynamics of the global ocean — a system containing 97% of Earth's water, covering 71% of the surface, and storing over 90% of the excess heat from anthropogenic c

thermohaline circulation AMOC ENSO El Niño La Niña ocean currents
ZF_1_09 Verified Oceanography

ZF_1_09 — Thermohaline Circulation and Ocean Conveyor

The thermohaline circulation (THC) — often called the "global ocean conveyor belt" — is the large-scale, density-driven system of deep ocean currents that redistributes heat, salt, carbon, and nutrients throughout the wo

thermohaline circulation ocean conveyor belt AMOC Atlantic meridional overturning deep water formation abyssal circulation
ZF_1_19 Verified Oceanography

ZF_1_19 — AMOC Collapse Risk

The Atlantic Meridional Overturning Circulation (AMOC) — a system of ocean currents carrying warm surface water northward through the Atlantic and returning cold, dense water at depth — is one of Earth's most critical cl

AMOC Atlantic Meridional Overturning Circulation thermohaline Gulf Stream climate tipping point Rahmstorf
E_2_09 Verified Cataclysms & Chronology

E_2_09 — Heinrich Events and Bond Cycles: Millennial-Scale Climate Oscillations

Heinrich events are episodes of massive iceberg discharge from the Laurentide Ice Sheet through Hudson Strait into the North Atlantic, depositing distinctive layers of ice-rafted debris (IRD) across the ocean floor. Firs

Heinrich events Bond cycles ice-rafted debris Dansgaard-Oeschger thermohaline circulation AMOC
O_1_13 Verified Earth Anomalies

O_1_13 — South Atlantic Anomaly: Geomagnetic Weakness and Radiation Belt Gap

The South Atlantic Anomaly (SAA) is the largest known weakness in Earth's magnetic field, centered over South America and the South Atlantic Ocean (roughly between Brazil and southern Africa), where the inner Van Allen r

South Atlantic Anomaly SAA geomagnetic Van Allen belt radiation magnetosphere
F_1_19 Speculative Lost Connections

F_1_19 — Irish Monks in America: The Brendan Voyage and Pre-Columbian North Atlantic Contacts

The hypothesis that Irish monks reached Iceland, the Faroe Islands, and possibly North America before the Norse has a foundation in medieval literary, place-name, and archaeological evidence, though the most ambitious cl

Saint Brendan Navigatio Irish monks pre-Columbian contact North Atlantic Iceland
F_3_17 Credible Lost Connections

F_3_17 — Megalithic Diffusion Debate: Atlantic Façade Connections

The megalithic diffusion debate is one of archaeology's longest-running controversies: did the remarkable concentrations of megalithic monuments (dolmens, passage tombs, standing stones, stone circles, alignments, and ch

megalith diffusion Atlantic façade standing stone dolmen passage tomb
ZF_3_11 Verified Oceanography

ZF_3_11 — The Sargasso Sea, Bermuda Triangle, and Western Atlantic Anomalies

The Sargasso Sea is the only "sea" in the world defined not by coastlines but by ocean currents — a roughly elliptical region (~3.1 million km²) in the western North Atlantic, bounded by the Gulf Stream (west), North Atl

Sargasso Sea Bermuda Triangle Sargassum North Atlantic gyre methane hydrate compass variation
F_1_03 Verified Lost Connections

F_1_03 — Phoenician and Carthaginian Atlantic Exploration

The Phoenicians and their Carthaginian successors were the ancient world's supreme mariners, operating an extensive maritime network across the Mediterranean and beyond from roughly 1500 BCE to 146 BCE. Ancient literary

Phoenician Carthaginian Hanno Himilco Atlantic circumnavigation
E_2_22 Verified Cataclysms & Chronology

E_2_22 — Dansgaard-Oeschger Events: Rapid Climate Oscillations of the Last Ice Age

Dansgaard-Oeschger (D-O) events are rapid climate oscillations that occurred during the last glacial period (~120,000–11,700 years BP), characterized by abrupt warmings of 8–16°C over Greenland within decades (as few as

Dansgaard-Oeschger events D-O events abrupt climate change ice core Greenland stadial
O_3_10 Verified Earth Anomalies

O_3_10 — Sargasso Sea and Ocean Gyres

Ocean gyres are large-scale, semi-permanent circular current systems driven by the interaction of wind stress, the Coriolis effect, and continental boundaries — there are five major subtropical gyres (North Atlantic, Sou

Sargasso Sea ocean gyre subtropical gyre Sargassum Great Pacific Garbage Patch thermohaline circulation
D_2_16 Credible Sites & Artifacts

D_2_16 — Tartessos & Iberian Peninsula Civilizations

Tartessos was a semi-legendary Bronze Age and Iron Age civilization centered in the lower Guadalquivir River valley of southwestern Iberia (modern Andalusia and southern Portugal), flourishing approximately 1100–550 BCE.

Tartessos Tartessian Iberia Phoenician Carambolo treasure Atlantic Bronze Age
F_1_25 Speculative Lost Connections

F_1_25 — Roman-Era Artifacts in the Americas

The claim that Roman-era artifacts have been found in the Americas — suggesting trans-Atlantic contact between the Roman world and pre-Columbian civilizations — is a recurring theme in diffusionist and alternative archae

Roman pre-Columbian Tecaxic-Calixtlahuaca amphorae coins terracotta
F_1_24 Speculative Lost Connections

F_1_24 — Phoenician Contact with the Americas

The hypothesis that Phoenician or Carthaginian sailors reached the Americas before Columbus is one of the most persistent and emotionally charged claims in the field of pre-Columbian transatlantic contact — a proposition

Phoenician Carthaginian pre-Columbian transatlantic Paraíba inscription Bat Creek
ZF_2_06 Verified Oceanography

ZF_2_06 — Mangrove and Estuary Ecosystems

Mangroves and estuaries are transitional ecosystems where terrestrial and marine environments meet, creating some of the most biologically productive and ecologically critical habitats on Earth. Estuaries — semi-enclosed

mangrove estuary salt marsh brackish water coastal wetland nursery habitat
ZF_2_21 Verified Oceanography

ZF_2_21 — Sargassum Bloom Crisis

The Great Atlantic Sargassum Belt (GASB) — an unprecedented, continent-spanning mass of floating Sargassum macroalgae stretching from West Africa to the Gulf of Mexico — has emerged since 2011 as one of the most dramatic

Sargassum great Atlantic Sargassum belt macroalgae bloom Caribbean nutrient loading
ZF_5_12 Verified Oceanography

ZF_5_12 — Paleocene-Eocene Thermal Maximum: Ancient Anoxic Ocean Crisis

The Paleocene-Eocene Thermal Maximum (PETM), occurring approximately 55.8 million years ago (latest Paleocene), was one of the most dramatic and rapid climate change events in the Cenozoic, offering the closest geologica

PETM Paleocene-Eocene Thermal Maximum hyperthermal carbon isotope excursion CIE ocean acidification
ZF_4_18 Verified Oceanography

ZF_4_18 — Deep Ocean Microplastics

Deep ocean microplastics — synthetic polymer particles smaller than 5 mm that have infiltrated the deepest marine environments on Earth — represent one of the most alarming and poorly understood dimensions of global plas

microplastics nanoplastics deep sea ocean floor Mariana Trench sediment
ZF_1_12 Verified Oceanography

ZF_1_12 — El Niño and ENSO: Pacific Oscillation and Global Climate Impact

The El Niño–Southern Oscillation (ENSO) is the most powerful year-to-year climate fluctuation on Earth — a coupled ocean-atmosphere phenomenon centered in the tropical Pacific that affects weather patterns, agriculture,

El Niño La Niña ENSO Pacific oscillation Walker circulation Bjerknes feedback
ZF_1_06 Verified Oceanography

ZF_1_06 — Arctic and Antarctic Ocean Systems

The Arctic and Antarctic ocean systems — the planet's polar marine environments — play disproportionately critical roles in global ocean circulation, climate regulation, and marine biodiversity. The Arctic Ocean (~14.06

polar ocean Arctic Ocean Southern Ocean sea ice ice sheet thermohaline circulation