Arctic Oscillation response to the 1991 Mount Pinatubo eruption: Effects of volcanic aerosols and ozone depletion
about
Are there statistical links between the direction of European weather systems and ENSO, the solar cycle or stratospheric aerosols?Bidecadal North Atlantic ocean circulation variability controlled by timing of volcanic eruptions.A model-tested North Atlantic Oscillation reconstruction for the past millennium.Global monsoon precipitation responses to large volcanic eruptions.Pacific North American circulation pattern links external forcing and North American hydroclimatic change over the past millenniumThe hydrological impact of geoengineering in the Geoengineering Model Intercomparison Project (GeoMIP)Introduction: Mount Pinatubo as a test of climate feedback mechanismsRole of the Atlantic Multidecadal Variability in modulating the climate response to a Pinatubo-like volcanic eruptionNew-generation NASA Aura Ozone Monitoring Instrument (OMI) volcanic SO<sub>2</sub> dataset: algorithm description, initial results, and continuation with the Suomi-NPP Ozone Mapping and Profiler Suite (OMPS)Stratospheric heating by potential geoengineering aerosolsBi-decadal variability excited in the coupled ocean–atmosphere system by strong tropical volcanic eruptionsStratospheric Dynamical Response and Ozone Feedbacks in the Presence of SO2 InjectionsEuropean climate response to tropical volcanic eruptions over the last half millenniumImpacts of a Pinatubo-size volcanic eruption on ENSOTambora 1815 as a test case for high impact volcanic eruptions: Earth system effectsNorthern hemispheric winter warming pattern after tropical volcanic eruptions: Sensitivity to the ozone climatologyNorthern Hemisphere winter warming and summer monsoon reduction after volcanic eruptions over the last millenniumWinter warming and summer monsoon reduction after volcanic eruptions in Coupled Model Intercomparison Project 5 (CMIP5) simulationsOcean response to volcanic eruptions in Coupled Model Intercomparison Project 5 simulationsCoupled Model Intercomparison Project 5 (CMIP5) simulations of climate following volcanic eruptionsClimate effects of high-latitude volcanic eruptions: Role of the time of yearSouthern Hemisphere atmospheric circulation effects of the 1991 Mount Pinatubo eruptionClimatic impact of volcanic emissionsThe response of winter Pacific North American pattern to strong volcanic eruptionsCO2seasonality indicates origins of post-Pinatubo sinkRegional Effects of the Mount Pinatubo Eruption on the Middle East and the Red SeaSensitivity of the regional climate in the Middle East and North Africa to volcanic perturbationsMeteorological responses to Mt. Baekdu volcanic eruption over east asia in an offline global climate-chemistry model: A pilot studyImpact of volcanic stratospheric aerosols on diurnal temperature range in Europe over the past 200 years: Observations versus model simulationsPossible Influence of Volcanic Activity on the Decadal Potential Predictability of the Natural Variability in Near-Term Climate PredictionsThe impact of natural versus anthropogenic aerosols on atmospheric circulation in the Community Atmosphere ModelRole of natural external forcing factors in modulating the Indian summer monsoon rainfall, the winter North Atlantic Oscillation and their relationship on inter-decadal timescale
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Arctic Oscillation response to the 1991 Mount Pinatubo eruption: Effects of volcanic aerosols and ozone depletion
description
article
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im Januar 2002 veröffentlichter wissenschaftlicher Artikel
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wetenschappelijk artikel
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наукова стаття, опублікована у 2002
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name
Arctic Oscillation response to ...... c aerosols and ozone depletion
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Arctic Oscillation response to ...... c aerosols and ozone depletion
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type
label
Arctic Oscillation response to ...... c aerosols and ozone depletion
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Arctic Oscillation response to ...... c aerosols and ozone depletion
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prefLabel
Arctic Oscillation response to ...... c aerosols and ozone depletion
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Arctic Oscillation response to ...... c aerosols and ozone depletion
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P356
P1476
Arctic Oscillation response to ...... c aerosols and ozone depletion
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P356
10.1029/2002JD002090
P407
P577
2002-01-01T00:00:00Z