Insolation-driven 100,000-year glacial cycles and hysteresis of ice-sheet volume - Wikidata - wikimedia - TriplyDB

Insolation-driven 100,000-year glacial cycles and hysteresis of ice-sheet volume

Insolation-driven 100,000-year glacial cycles and hysteresis of ice-sheet volume

http://www.wikidata.org/entity/Q29540552

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Lineage range estimation method reveals fine-scale endemism linked to Pleistocene stability in Australian rainforest herpetofauna Exposure age and ice-sheet model constraints on Pliocene East Antarctic ice sheet dynamics.The Asian monsoon over the past 640,000 years and ice age terminations.State dependence of climatic instability over the past 720,000 years from Antarctic ice cores and climate modeling.Evolution of the early Antarctic ice ages.Nonlinear climatic sensitivity to greenhouse gases over past 4 glacial/interglacial cycles Critical insolation-CO2 relation for diagnosing past and future glacial inception.Carbon choices determine US cities committed to futures below sea level.MIS-11 duration key to disappearance of the Greenland ice sheet.Climate science: Solution proposed for ice-age mystery.Overestimate of committed warming.Snyder replies.Causes of ice age intensification across the Mid-Pleistocene Transition.Enhancing (crop) plant photosynthesis by introducing novel genetic diversity.A simple rule to determine which insolation cycles lead to interglacials.Sea-level variability over five glacial cycles.Asynchrony between Antarctic temperature and CO2 associated with obliquity over the past 720,000 years.Abrupt Climate Change in an Oscillating World.Ice Sheet Model Intercomparison Project (ISMIP6) contribution to CMIP6.Consequences of twenty-first-century policy for multi-millennial climate and sea-level change Interglacials of the last 800,000 years Laurentide ice-sheet instability during the last deglaciation Forcing of late Pleistocene ice volume by spatially variable summer energy The middle Pleistocene transition as a generic bifurcation on a slow manifold A review of progress towards understanding the transient global mean surface temperature response to radiative perturbation A lower limit to atmospheric CO2 concentrations over the past 800,000 years Geographic Variability of Sea-Level Change Eccentricity pacing of eastern equatorial Pacific carbonate dissolution cycles during the Miocene Climatic Optimum

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P2860

Insolation-driven 100,000-year glacial cycles and hysteresis of ice-sheet volume

http://www.wikidata.org/entity/Q29540552

description

2013 nî lūn-bûn

@nan

2013 թուականի Օգոստոսին հրատարակուած գիտական յօդուած

@hyw

2013 թվականի օգոստոսին հրատարակված գիտական հոդված

@hy

2013年の論文

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2013年論文

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2013年論文

@zh-hant

2013年論文

@zh-hk

2013年論文

@zh-mo

2013年論文

@zh-tw

2013年论文

@wuu

name

Insolation-driven 100,000-year glacial cycles and hysteresis of ice-sheet volume

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Insolation-driven 100,000-year glacial cycles and hysteresis of ice-sheet volume

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type

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Insolation-driven 100,000-year glacial cycles and hysteresis of ice-sheet volume

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Insolation-driven 100,000-year glacial cycles and hysteresis of ice-sheet volume

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Insolation-driven 100,000-year glacial cycles and hysteresis of ice-sheet volume

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Insolation-driven 100,000-year glacial cycles and hysteresis of ice-sheet volume

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P1476

Insolation-driven 100,000-year glacial cycles and hysteresis of ice-sheet volume

@en

P2093

Heinz Blatter

http://www.w3.org/2001/XMLSchema#string

Jun’ichi Okuno

http://www.w3.org/2001/XMLSchema#string

Kunio Takahashi

http://www.w3.org/2001/XMLSchema#string

Maureen E. Raymo

http://www.w3.org/2001/XMLSchema#string

P2860

The 100,000-year ice-Age cycle identified and found to lag temperature, carbon dioxide, and orbital eccentricity

Northern Hemisphere forcing of climatic cycles in Antarctica over the past 360,000 years

Variations in the Earth's Orbit: Pacemaker of the Ice Ages

The Last Glacial Maximum

Deglacial rapid sea level rises caused by ice-sheet saddle collapses.

Modelling West Antarctic ice sheet growth and collapse through the past five million years.

Northern Hemisphere forcing of Southern Hemisphere climate during the last deglaciation.

Combined obliquity and precession pacing of late Pleistocene deglaciations.

Climate and atmospheric history of the past 420,000 years from the Vostok ice core, Antarctica

The timing of Pleistocene glaciations from a simple multiple-state climate model

P2888

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190-193

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scholarly article

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10.1038/NATURE12374

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7461

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500

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Ayako Abe-Ouchi

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2013-08-07T00:00:00Z

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1026861987

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23925242

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