sameAs
Solar forcing synchronizes decadal North Atlantic climate variability.Amplifying the Pacific climate system response to a small 11-year solar cycle forcing.Decadal variability of tropical tropopause temperature and its relationship to the Pacific Decadal OscillationRegional atmospheric circulation shifts induced by a grand solar minimumEleven-year solar cycle variations in the atmosphere: observations, mechanisms and modelsSOLAR INFLUENCES ON CLIMATEThe Detection and Attribution Model Intercomparison Project (DAMIP v1.0) contribution to CMIP6Solar forcing for CMIP6 (v3.2)What is the solar influence on climate? Overview of activities during CAWSES-IIThe representation of solar cycle signals in stratospheric ozone – Part 1: A comparison of recently updated satellite observationsThe tropical tropopause inversion layer: variability and modulation by equatorial wavesHow does downward planetary wave coupling affect polar stratospheric ozone in the Arctic winter stratosphere?Wave modulation of the extratropical tropopause inversion layerThe importance of interactive chemistry for stratosphere–troposphere–couplingThe representation of solar cycle signals in stratospheric ozone – Part 2: Analysis of global modelsRadiative effects of ozone waves on the Northern Hemisphere polar vortex and its modulation by the QBORadiative effects of ozone waves on the Northern Hemisphere polar vortex and its modulation by the QBOThe representation of solar cycle signals in stratospheric ozone. Part II: Analysis of global modelsWave Modulation of the Extratropical Tropopause Inversion LayerHow Does Downward Planetary Wave Coupling Affect Polar Stratospheric Ozone in the Arctic Winter Stratosphere?Validation of COSMIC water vapor data in the upper troposphere and lower stratosphere using MLS, MERRA and ERA-InterimSolar Forcing for CMIP6 (v3.1)The representation of solar cycle signals in stratospheric ozone – Part 1: A comparison of satellite observationsHow can we understand the global distribution of the solar cycle signal on the Earth's surface?Impact of the Antarctic Ozone Hole on the Vertical Coupling of the Stratosphere–Mesosphere–Lower Thermosphere SystemInfluence of the Quasi-Biennial Oscillation and Sea Surface Temperature Variability on Downward Wave Coupling in the Northern HemispherePoleward transport variability in the Northern Hemisphere during final stratospheric warmings simulated by CESM(WACCM)Solar signals in CMIP-5 simulations: effects of atmosphere-ocean couplingThe impact of a future solar minimum on climate change projections in the Northern HemisphereTropopause sharpening by data assimilationTropospheric QBO–ENSO Interactions and Differences between the Atlantic and PacificA case study of multi-annual temperature oscillations in the atmosphere: Middle EuropeQuantifying contributions to the recent temperature variability in the tropical tropopause layerSolar signals in CMIP-5 simulations: the ozone responseSolar signals in CMIP-5 simulations: the stratospheric pathwaySynoptic-scale behavior of the extratropical tropopause inversion layerUTLS temperature validation of MPI-ESM decadal hindcast experiments with GPS radio occultationsLow-frequency ocean bottom pressure variations in the North Pacific in response to time-variable surface windsObservations of stratospheric sudden warmings in Earth rotation variationsPersistent link between solar activity and Greenland climate during the Last Glacial Maximum
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description
deutsche Klimawissenschaftlerin
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hulumtuese
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Katja Matthes
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Katja Matthes
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Katja Matthes
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Katja Matthes
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Katja Matthes
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Katja Matthes
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Katja Matthes
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Katja Matthes
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Katja Matthes
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Katja Matthes
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Katja Matthes
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Katja Matthes
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Katja Matthes
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