about
Why marine phytoplankton calcifyEl Niño and coral larval dispersal across the eastern Pacific marine barrierHistorical and idealized climate model experiments: an intercomparison of Earth system models of intermediate complexityThe geological record of ocean acidificationThe influence of the biological pump on ocean chemistry: implications for long-term trends in marine redox chemistry, the global carbon cycle, and marine animal ecosystemsCombustion of available fossil fuel resources sufficient to eliminate the Antarctic Ice SheetFuture habitat suitability for coral reef ecosystems under global warming and ocean acidificationWarm climates of the past--a lesson for the future?Surviving rapid climate change in the deep sea during the Paleogene hyperthermalsDust in the Earth system: the biogeochemical linking of land, air and sea.Tackling regional climate change by leaf albedo bio-geoengineering.Global iron connections between desert dust, ocean biogeochemistry, and climateA Palaeogene perspective on climate sensitivity and methane hydrate instability.Very large release of mostly volcanic carbon during the Palaeocene-Eocene Thermal Maximum.A probabilistic assessment of the rapidity of PETM onset.A Cenozoic record of the equatorial Pacific carbonate compensation depth.Onset of carbon isotope excursion at the Paleocene-Eocene thermal maximum took millennia, not 13 years.The societal challenge of ocean acidification.Geoengineering: taking control of our planet's climate?Changing atmospheric CO2 concentration was the primary driver of early Cenozoic climate.Potential methane reservoirs beneath Antarctica.Carbonate deposition, climate stability, and Neoproterozoic ice ages.Changes in benthic ecosystems and ocean circulation in the Southeast Atlantic across Eocene Thermal Maximum 2Climate model and proxy data constraints on ocean warming across the Paleocene–Eocene Thermal MaximumOcean acidification in the freezerPast constraints on the vulnerability of marine calcifiers to massive carbon dioxide releaseCO2-driven ocean circulation changes as an amplifier of Paleocene-Eocene thermal maximum hydrate destabilizationSelective environmental stress from sulphur emitted by continental flood basalt eruptionsAnthropogenic carbon release rate unprecedented during the past 66 million yearsSedimentary response to Paleocene-Eocene Thermal Maximum carbon release: A model-data comparisonAntarctic ice sheet fertilises the Southern OceanNutrients as the dominant control on the spread of anoxia and euxinia across the Cenomanian-Turonian oceanic anoxic event (OAE2): Model-data comparisonThe fate of the Greenland Ice Sheet in a geoengineered, high CO2worldEnhanced weathering strategies for stabilizing climate and averting ocean acidificationAssessing the controllability of Arctic sea ice extent by sulfate aerosol geoengineeringComparative carbon cycle dynamics of the present and last interglacialStrategies in times of crisis-insights into the benthic foraminiferal record of the Palaeocene-Eocene Thermal MaximumEmulation of long-term changes in global climate: application to the late Pliocene and futureLong-Term Climate Change Commitment and Reversibility: An EMIC IntercomparisonAn oceanic origin for the increase of atmospheric radiocarbon during the Younger Dryas
P50
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P50
description
onderzoeker
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researcher
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հետազոտող
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name
Andy Ridgwell
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Andy Ridgwell
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Andy Ridgwell
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Andy Ridgwell
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Andy Ridgwell
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Andy Ridgwell
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Andy Ridgwell
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Andy Ridgwell
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Andy Ridgwell
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Andy Ridgwell
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Andy Ridgwell
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Andy Ridgwell
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Andy Ridgwell
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Andy Ridgwell
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Andy Ridgwell
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P106
P1153
6602583456
P21
P31
P496
0000-0003-2333-0128