Global cooling after the eruption of Mount Pinatubo: a test of climate feedback by water vapor.
about
Photophoretic levitation of engineered aerosols for geoengineeringEcosystem impacts of geoengineering: a review for developing a science planContributions of past and present human generations to committed warming caused by carbon dioxide.Global warming alters sound transmission: differential impact on the prey detection ability of echolocating bats.Greenhouse gases, radiative forcing, global warming potential and waste management--an introduction.Uncertainties associated with quantifying climate change impacts on human health: a case study for diarrheaMid-latitude interhemispheric hydrologic seesaw over the past 550,000 years.Identification of human-induced changes in atmospheric moisture content.Observational evidence for volcanic impact on sea level and the global water cycle.Feedbacks, climate sensitivity and the limits of linear models.Temperature reconstruction and volcanic eruption signal from tree-ring width and maximum latewood density over the past 304 years in the southeastern Tibetan Plateau.Chemical signals of past climate and environment from polar ice cores and firn air.Tropical explosive volcanic eruptions can trigger El Niño by cooling tropical AfricaEnhanced ice sheet melting driven by volcanic eruptions during the last deglaciationDirect human influence of irrigation on atmospheric water vapour and climateThe hydrological impact of geoengineering in the Geoengineering Model Intercomparison Project (GeoMIP)The equilibrium sensitivity of the Earth's temperature to radiation changesBeyond equilibrium climate sensitivityIntroduction: Mount Pinatubo as a test of climate feedback mechanismsAn observationally based constraint on the water-vapor feedbackClimate Engineering and Abatement: A ‘flat’ Relationship Under UncertaintyCounteracting the climate effects of volcanic eruptions using short-lived greenhouse gasesStratospheric aerosol particles and solar-radiation managementStratospheric Aerosols from Major Volcanic Eruptions: A Composition-Climate Model Study of the Aerosol Cloud Dispersal and e-folding TimeStratospheric ozone response to sulfate geoengineering: Results from the Geoengineering Model Intercomparison Project (GeoMIP)Intercomparison of atmospheric water vapour measurements at a Canadian High Arctic siteSensitivity of volcanic aerosol dispersion to meteorological conditions: A Pinatubo case studyBi-decadal variability excited in the coupled ocean–atmosphere system by strong tropical volcanic eruptionsTwentieth-century temperature and precipitation trends in ensemble climate simulations including natural and anthropogenic forcingRadiative and Chemical Response to Interactive Stratospheric Sulfate Aerosols in Fully Coupled CESM1(WACCM)Studying geoengineering with natural and anthropogenic analogsImpacts of a Pinatubo-size volcanic eruption on ENSOImplications of the glacial CO2“iron hypothesis” for Quaternary climate changeSmall global-mean cooling due to volcanic radiative forcingCombining satellite data and models to estimate cloud radiative effect at the surface and in the atmosphereExploitation of Geostationary Earth Radiation Budget data using simulations from a numerical weather prediction model: Methodology and data validationObserved multivariable signals of late 20th and early 21st century volcanic activityClimatic impact of volcanic emissionsSensitivity of the regional climate in the Middle East and North Africa to volcanic perturbations20th century changes in surface solar irradiance in simulations and observations
P2860
Q24601828-97FE6B38-298A-4813-A073-A99BD0E784A7Q28727329-47CFF6E1-B490-40E5-ABAA-AA7701AADDE6Q28769541-82AAFB89-BAE6-4A1F-8419-EB9ED5CB1AC9Q30419268-9335B6D1-3E71-448E-AFB3-D3E1765E547DQ33502532-268C84B4-41A2-4B4F-809F-5A6AA598FC26Q33712545-31FE38CE-9850-4523-B576-4496A8330904Q34413346-978CEC8E-13A2-4ED0-92A5-FCAF3CADDD43Q36002433-F44CBB2D-FE04-48D1-A2E3-1AEB58BCCDF0Q36288829-0AFAC996-331E-4CCB-8721-B8EA2B045D66Q38599675-3E524804-DBA4-4DA4-86F9-0D6937E32571Q38690115-E6D968D7-8694-4B96-991F-7483537F6D37Q39119547-4C5B6583-6803-438E-B98B-696FE64F3BD1Q41924370-E42883DC-BE29-474E-8FC0-0E110381717BQ42639762-72A349E0-03BF-441D-AA78-B2172E407E52Q56037716-BA098184-B0AF-4483-9604-0FB729551F10Q56523879-37CC2DD2-6317-45B2-9D2D-FDFE01B1B0DCQ56620062-CD507E17-D336-466A-97F2-EE6D2B436B03Q56620065-492920D4-83D1-4060-AA56-D13EECDD659BQ56680822-7097F335-454F-4FC0-A75E-A01F6DDC96CCQ56837431-531F304E-D8DF-431D-8B5F-53770EC27418Q56867657-A9161728-779B-4A80-A9FB-D315901CAC11Q57402959-D4096C76-008C-4E06-BBEF-FFC051E8F73DQ57534050-1551042C-32CB-4F4C-9815-EE7C669BAF59Q57536785-0D34A58F-BFAB-47B9-9C55-6308FEB99E53Q57536800-11744EF7-4BB8-40C7-BED5-F12E06A65FB5Q57884720-A82A8588-0E16-4274-B776-E83D24923153Q57915001-A03E1DD6-5B00-4A11-AD25-FA3D296FAC06Q58060469-736E38FB-97A4-480E-B86D-C04E472EF1A9Q58068846-2EEA8B01-D5FE-4266-A778-412C65FA64EDQ58070024-62006FFD-6E15-4155-AB78-6FFF21CE525BQ58070110-97238B6B-530E-4FCE-B45D-63C2253A4758Q58073040-63970D2B-EA70-46E7-A7C7-4E2556F9D3FDQ58074744-325F9DD1-455B-4EB9-AE43-C685E34FE978Q58076094-4BDBF68A-2DEE-482F-BFFC-76C1B8FA7EB8Q58098936-454588B1-C6F1-4643-8BFB-C32D24BDC1D2Q58099018-BC137792-69DF-4AD6-9327-126DA59F2355Q58258647-4F368A82-C907-46CE-8C67-16BC6D464BD6Q58262566-3EC281CC-4805-4BB5-B746-E4C8E4549DFDQ58382432-F8377D32-EBE3-4166-BCA6-5BDF60F740E5Q58384560-F44C5DA4-F78B-4271-9678-8550188C2DC4
P2860
Global cooling after the eruption of Mount Pinatubo: a test of climate feedback by water vapor.
description
2002 nî lūn-bûn
@nan
2002年の論文
@ja
2002年論文
@yue
2002年論文
@zh-hant
2002年論文
@zh-hk
2002年論文
@zh-mo
2002年論文
@zh-tw
2002年论文
@wuu
2002年论文
@zh
2002年论文
@zh-cn
name
Global cooling after the erupt ...... imate feedback by water vapor.
@en
Global cooling after the erupt ...... imate feedback by water vapor.
@nl
type
label
Global cooling after the erupt ...... imate feedback by water vapor.
@en
Global cooling after the erupt ...... imate feedback by water vapor.
@nl
prefLabel
Global cooling after the erupt ...... imate feedback by water vapor.
@en
Global cooling after the erupt ...... imate feedback by water vapor.
@nl
P50
P1433
P1476
Global cooling after the erupt ...... imate feedback by water vapor.
@en
P2093
Richard T Wetherald
P304
P356
10.1126/SCIENCE.296.5568.727
P407
P577
2002-04-01T00:00:00Z