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Notholt, Justus
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Additional programs for GRL paper by Notholt et al. (2023) ...
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Additional programs for GRL paper by Notholt et al. (2023) ...
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Heterogeneous conversion of HCl and ClONO2 during the Arctic winter 1992/93 init...
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Properties of coastal Antarctic aerosol from combined FTIR spectrometer and sun...
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Hochauflösende FT-IR/UV/Vis Spektroskopie von stratosphärischen Spurengasen in d...
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Direct thermal radiative forcing of tropospheric aerosol in the Arctic measured...
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Stratospheric trace gas concentrations in the Arctic drived by FTIR-specctroscop...
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Summertime evolution of ozone in the high Arctic
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Microphysical Cloud Parameters and water paths retrieved from EM-FTIR spectra, m...
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Updated microphysical cloud parameters retrieved from EM-FTIR spectra, measured...
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Updated microphysical cloud parameters retrieved from EM-FTIR spectra, measured...
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Microphysical Cloud Parameters and water paths retrieved from EM-FTIR spectra, m...
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Can increasing CO2 cool Antarctica?
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Ground-based FTIR measurements of CLONO2 vertical column amounts in the Arctic
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Influences of biomass burning events on Arctic trace gases detected from long te...
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Carbon Monoxide Variability in the Northern and Southern Hemisphere Measured by...
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Increasing CO2 cools Antarctica
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How increasing CO2 leads to an increased negative greenhouse effect in Antarctic...
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Where does CO2 in Antarctica cool the atmosphere ?
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How does the sulfur get into the stratosphere?
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