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8 results for "Milankovitch"

O_5_05 — Ice Ages and Milankovitch Cycles: Orbital Forcing of Climate

Ice ages — periods when massive continental ice sheets expand to cover large portions of Earth's surface — are among the most dramatic climate events in the planet's history. The Quaternary glaciation (beginning ~2.6 mil

ice age glacial interglacial Milankovitch orbital eccentricity

E_4_13 Verified Cataclysms & Chronology

E_4_13 — Milankovitch Cycles and Orbital Forcing

Milankovitch cycles are periodic variations in Earth's orbital geometry that modulate the distribution and intensity of solar radiation reaching Earth's surface, driving the glacial-interglacial cycles that have dominate

Milankovitch cycles orbital forcing eccentricity obliquity precession ice age

E_4_11 Cataclysms & Chronology

E_4_11 — The Holocene Climate Optimum and Mid-Holocene Transition

The Holocene Climate Optimum (also called the Holocene Thermal Maximum or Hypsithermal) designates a prolonged warm interval roughly spanning 9,000–5,000 years before present, during which Northern Hemisphere summer temp

Holocene Thermal Maximum Holocene Climate Optimum Green Sahara African Humid Period Milankovitch obliquity

ZH_5_04 Verified Archaeoastronomy

ZH_5_04 — Precession of the Equinoxes: Hipparchus, Axial Wobble, and the Great Year

The precession of the equinoxes — the slow, continuous westward shift of the equinoctial points (where the ecliptic crosses the celestial equator) along the ecliptic — is one of the most consequential astronomical phenom

precession equinoxes Hipparchus axial wobble Platonic year Great Year

ZF_1_04 Oceanography

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

paleoceanography ice age Milankovitch cycles foraminifera oxygen isotope ocean carbon pump

E_4_21 Verified Cataclysms & Chronology

E_4_21 — Oxygen Isotope Stages: Marine Isotope Record and Climate Cycles

The marine oxygen isotope record — constructed from measurements of the ratio of oxygen-18 to oxygen-16 (δ¹⁸O) in the calcium carbonate (CaCO₃) shells of foraminifera (single-celled marine organisms) preserved in deep-se

oxygen isotope δ18O marine isotope stage MIS benthic foraminifera planktonic

S_3_01 Future Technology

S_3_01 — Climate Change, Civilization, and Deep-Time Context

Earth's climate has always changed — but the current rate and mechanism are unprecedented in geological history. This document places the modern climate crisis within the deep-time context that the corpus demands: from t

climate change anthropocene PETM Green Sahara tipping points climate refugees

F_4_09 Lost Connections

F_4_09 — The Green Sahara — When the Desert Was Eden

For most of the last several thousand years, the Sahara has been the world's largest hot desert — 9.2 million km² of arid wasteland. Yet between approximately 11,000 and 5,000 years ago, during the period known as the Af

Green Sahara African Humid Period Saharan rock art Tassili n'Ajjer Lake Mega-Chad Nabta Playa

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