RESEARCH BASE
Search 3,717 documents across 34 fields — every claim tier-rated by evidence
192 results for "ocean acidification" — page 2 of 10
ZF_4_11 — Sea Ice Dynamics and Polar Oceanography
Sea ice — frozen seawater that forms a thin crust (typically 1–4 m thick) over polar and subpolar oceans — is one of Earth's most dynamic and climate-sensitive features, playing a disproportionate role in global climate
ZF_4_13 — Ocean Noise Pollution: Anthropogenic Sound and Marine Life
Ocean noise pollution — the introduction of excessive or harmful human-generated sound into the marine environment — has emerged as one of the most pervasive and least visible threats to marine ecosystems. Sound travels
ZF_4_02 — Ocean Pollution and Plastic Debris
Ocean pollution encompasses the introduction of harmful substances and materials into the marine environment, degrading water quality, damaging ecosystems, and threatening human health. The major categories are: plastic
ZF_4_06 — Ocean Remote Sensing and Satellite Oceanography
Satellite oceanography — the use of Earth-orbiting sensors to observe ocean properties from space — has transformed ocean science since the 1970s from a data-sparse field reliant on sparse ship transects to a globally co
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
ZF_4_10 — Coral as Climate Archive — Paleoceanographic Proxies
Coral paleoclimatology uses the geochemical and physical properties of coral skeletons as high-resolution archives of past ocean conditions — providing some of the most detailed tropical climate records available for the
ZF_4_16 — Microplastics in the Ocean: Sources, Pathways, and Ecological Impact
Microplastics — plastic particles smaller than 5 mm in diameter — have become one of the most pervasive and persistent pollutants in the global ocean. First systematically described as a marine pollutant by Richard Thomp
ZF_4_15 — Ocean Sediments: Deep-Sea Cores, Proxy Records, and Paleoclimate
Ocean sediments are the Earth's most comprehensive climate archive — a continuous record of planetary conditions extending back over 200 million years, slowly accumulated grain by grain on the deep seafloor at rates of m
ZF_4_04 — Ocean Acoustics and Sound Channels
Ocean acoustics — the study of sound propagation in the sea — is fundamental to marine science, military applications, and understanding marine life. Sound travels approximately 4.5× faster in seawater (~1,500 m/s) than
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
ZF_1_20 — Ocean Stratification
Ocean stratification — the formation of stable density layers in the water column due to gradients in temperature, salinity, and pressure — is one of the most fundamental physical characteristics of the global ocean and
ZF_1_14 — Ocean-Atmosphere Coupling: Heat Exchange, Evaporation, and Weather
The ocean-atmosphere interface — the boundary between Earth's two great fluid envelopes — is the planet's most important energy exchange surface. The ocean absorbs approximately 93% of the excess heat trapped by anthropo
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
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
ZF_1_04 — Ocean-Climate Coupling: Paleoceanography
The ocean is Earth's primary climate regulator — absorbing ~93% of the excess heat trapped by greenhouse gases and ~30% of anthropogenic CO₂, storing 50 times more carbon than the atmosphere, and driving glacial-intergla
ZF_1_07 — Submarine Geology and Ocean Trenches
The submarine geology of the ocean floor encompasses a vast range of geological features — from abyssal plains (the flattest surfaces on Earth, at 3,000–6,000 m depth, covered by fine sediment) to mid-ocean ridges (the l
ZF_1_16 — Paleoceanography and Foraminifera: Reconstructing Ancient Oceans from Microfossil Archives
Paleoceanography — the study of the history of the oceans and their role in Earth's climate system through geological time — relies fundamentally on the geochemical analysis of foraminifera (single-celled protists with c
J_4_12 — Polynesian Navigation Canoes: Oceanic Vessel Engineering
The Polynesian double-hulled sailing canoe — waka hourua (Māori), wa'a kaulua (Hawaiian), vaka (general Polynesian) — was the vessel that made possible the most extraordinary feat of maritime exploration in human history
Q_3_15 — Icy Moons: Europa, Titan, Enceladus, and Subsurface Oceans
Among the most transformative discoveries of planetary science in the past three decades is the realization that several moons of the outer solar system — Europa (Jupiter), Enceladus (Saturn), Titan (Saturn), and Ganymed
ZB_3_23 — Coral Reef Ecosystem Dynamics
Coral reefs are among Earth's most biodiverse and economically valuable ecosystems, occupying less than 0.1% of the ocean floor yet supporting approximately 25% of all marine species (~830,000 species). Built over millen
BROWSE BY SECTION — 3717 documents across 34 fields