KnowraVolcanic winterLinked fromLinked fromThe 32 pages that link to Volcanic winter, each with the reason it gives.All 32Broader topic 3Related 17Narrower topic 6Compared with 6Permian–Triassic extinction eventCompared with: Short-lived volcanic cooling may have accompanied, but cannot alone explain, prolonged warming.Volcanic gasRelated: Sulfur gases from large eruptions can form the aerosols that drive cooling.Volcanic eruptionRelated: Large eruptions can inject sulfur compounds high enough to cool the climate temporarily.Ice coreRelated: Sulfate layers in ice cores can identify eruptions and help assess their climatic effects.AlbedoRelated: Stratospheric aerosols raise Earth's reflectivity, illustrating how atmospheric particles alter planetary albedo.Milankovitch cyclesCompared with: Volcanic cooling is abrupt and short-lived compared with orbital cycles spanning thousands of years.VolcanismBroader topic: Large explosive eruptions can inject sulfur compounds high into the atmosphere.Little Ice AgeRelated: Repeated eruptions could reinforce cooling by reducing incoming sunlight.Flood basaltRelated: Sulfur-rich emissions can cool the surface during or shortly after eruptive pulses.GradualismBroader topic: Large eruptions show that sudden disruptions can interrupt slower geological trends.Climate variabilityRelated: Large eruptions can impose short-lived variability distinct from internally generated cycles.CatastrophismRelated: It shows how a sudden geological event can rapidly alter climate.Nuclear winterCompared with: Both involve sunlight reduction, but volcanic aerosols and nuclear-fire soot differ in origin and properties.Volcanic Explosivity IndexRelated: Large explosive eruptions can produce the aerosols behind this consequence, though VEI alone cannot predict it.Mount VesuviusRelated: The AD 79 eruption affected the region, but evidence does not establish a global volcanic winter.Large igneous provinceRelated: Sulfur-rich eruptions from a province can cool climate over short timescales.Siberian TrapsCompared with: Short-lived cooling from eruptions may have alternated with the longer warming that dominated the crisis.Mount PinatuboNarrower topic: Pinatubo's sulfur-rich plume caused measurable global cooling after the eruption.Explosive eruptionRelated: Sulfur dioxide from a large explosive eruption can form sunlight-reflecting aerosols.KrakatoaNarrower topic: Krakatoa’s stratospheric aerosols produced measurable global cooling after the eruption.Mount TamboraNarrower topic: Tambora is a major historical example of eruption-driven cooling on a global scale.Year Without a SummerNarrower topic: The cold summer was a regional expression of this global cooling mechanism.1991 eruption of Mount PinatuboNarrower topic: The aerosol veil from Pinatubo caused measurable global cooling after the eruption.Fissure eruptionRelated: Sulfur dioxide from some prolonged fissure eruptions can form aerosols with regional or global effects.Volcanic outgassingBroader topic: Sulfur gases from major eruptions can form the cooling aerosols involved.Klyuchevskaya SopkaCompared with: Unlike Klyuchevskaya’s typical local hazards, volcanic winter requires exceptionally large eruptions with far-reaching effects.1883 eruption of KrakatoaRelated: Krakatoa’s aerosols contributed to measurable short-term cooling after the eruption.Global coolingRelated: Volcanic aerosols provide a short-lived natural mechanism for cooling, unlike persistent pollution emissions.SupervolcanoRelated: Sulfur-rich emissions from an exceptionally large eruption could cool climate temporarily.HeklaRelated: Hekla’s explosive eruptions contributed ash and gases to the atmosphere, linking local folklore to wider environmental effects.Mount Tambora eruptionNarrower topic: This broader phenomenon links Tambora’s atmospheric effects to the cooling that followed.Solar activity and climateCompared with: Volcanic cooling can coincide with solar minima but arises from a separate atmospheric forcing.
KnowraVolcanic winterLinked fromLinked fromThe 32 pages that link to Volcanic winter, each with the reason it gives.All 32Broader topic 3Related 17Narrower topic 6Compared with 6Permian–Triassic extinction eventCompared with: Short-lived volcanic cooling may have accompanied, but cannot alone explain, prolonged warming.Volcanic gasRelated: Sulfur gases from large eruptions can form the aerosols that drive cooling.Volcanic eruptionRelated: Large eruptions can inject sulfur compounds high enough to cool the climate temporarily.Ice coreRelated: Sulfate layers in ice cores can identify eruptions and help assess their climatic effects.AlbedoRelated: Stratospheric aerosols raise Earth's reflectivity, illustrating how atmospheric particles alter planetary albedo.Milankovitch cyclesCompared with: Volcanic cooling is abrupt and short-lived compared with orbital cycles spanning thousands of years.VolcanismBroader topic: Large explosive eruptions can inject sulfur compounds high into the atmosphere.Little Ice AgeRelated: Repeated eruptions could reinforce cooling by reducing incoming sunlight.Flood basaltRelated: Sulfur-rich emissions can cool the surface during or shortly after eruptive pulses.GradualismBroader topic: Large eruptions show that sudden disruptions can interrupt slower geological trends.Climate variabilityRelated: Large eruptions can impose short-lived variability distinct from internally generated cycles.CatastrophismRelated: It shows how a sudden geological event can rapidly alter climate.Nuclear winterCompared with: Both involve sunlight reduction, but volcanic aerosols and nuclear-fire soot differ in origin and properties.Volcanic Explosivity IndexRelated: Large explosive eruptions can produce the aerosols behind this consequence, though VEI alone cannot predict it.Mount VesuviusRelated: The AD 79 eruption affected the region, but evidence does not establish a global volcanic winter.Large igneous provinceRelated: Sulfur-rich eruptions from a province can cool climate over short timescales.Siberian TrapsCompared with: Short-lived cooling from eruptions may have alternated with the longer warming that dominated the crisis.Mount PinatuboNarrower topic: Pinatubo's sulfur-rich plume caused measurable global cooling after the eruption.Explosive eruptionRelated: Sulfur dioxide from a large explosive eruption can form sunlight-reflecting aerosols.KrakatoaNarrower topic: Krakatoa’s stratospheric aerosols produced measurable global cooling after the eruption.Mount TamboraNarrower topic: Tambora is a major historical example of eruption-driven cooling on a global scale.Year Without a SummerNarrower topic: The cold summer was a regional expression of this global cooling mechanism.1991 eruption of Mount PinatuboNarrower topic: The aerosol veil from Pinatubo caused measurable global cooling after the eruption.Fissure eruptionRelated: Sulfur dioxide from some prolonged fissure eruptions can form aerosols with regional or global effects.Volcanic outgassingBroader topic: Sulfur gases from major eruptions can form the cooling aerosols involved.Klyuchevskaya SopkaCompared with: Unlike Klyuchevskaya’s typical local hazards, volcanic winter requires exceptionally large eruptions with far-reaching effects.1883 eruption of KrakatoaRelated: Krakatoa’s aerosols contributed to measurable short-term cooling after the eruption.Global coolingRelated: Volcanic aerosols provide a short-lived natural mechanism for cooling, unlike persistent pollution emissions.SupervolcanoRelated: Sulfur-rich emissions from an exceptionally large eruption could cool climate temporarily.HeklaRelated: Hekla’s explosive eruptions contributed ash and gases to the atmosphere, linking local folklore to wider environmental effects.Mount Tambora eruptionNarrower topic: This broader phenomenon links Tambora’s atmospheric effects to the cooling that followed.Solar activity and climateCompared with: Volcanic cooling can coincide with solar minima but arises from a separate atmospheric forcing.