Florian E. Roemer
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View article: Variation in shortwave water vapour continuum and impact on clear-sky shortwave radiative feedback
Variation in shortwave water vapour continuum and impact on clear-sky shortwave radiative feedback Open
This work assesses the impact of the current differences in the strength of the shortwave water vapour continuum on clear-sky calculations of shortwave radiative feedback. Three continuum models were used: the MT_CKD (Mlawer–Tobin–Clough–K…
View article: How to think about the clear-sky shortwave water vapor feedback
How to think about the clear-sky shortwave water vapor feedback Open
Earth’s climate feedback quantifies the response of Earth’s energy budget to temperature changes and thus determines climate sensitivity. The climate feedback is largely controlled by water vapor which absorbs both longwave radiation emitt…
View article: Observations of the Clear-Sky Spectral Longwave Feedback at Surface Temperatures between 210 and 310 K
Observations of the Clear-Sky Spectral Longwave Feedback at Surface Temperatures between 210 and 310 K Open
The longwave feedback λ characterizes how Earth’s outgoing longwave radiation changes with near-surface air temperature T as , directly impacting climate sensitivity. Compared to λ , its spectrally resolved counterpart λ ν offers deeper in…
View article: The atmospheric radiative transfer simulator ARTS, version 2.6 — Deep python integration
The atmospheric radiative transfer simulator ARTS, version 2.6 — Deep python integration Open
View article: How to think about the shortwave water vapor feedback
How to think about the shortwave water vapor feedback Open
Earth's climate feedback quantifies how Earth's energy budget responds to temperature changes and thus directly determines climate sensitivity. To a large extent, the climate feedback is controlled by water vapor, the most powerful greenho…
View article: Variation in shortwave water vapour continuum and impact on clear-sky shortwave radiative feedback
Variation in shortwave water vapour continuum and impact on clear-sky shortwave radiative feedback Open
This work assesses the impact of the current differences in the strength of the shortwave water vapour continuum on clear-sky calculations of shortwave radiative feedback. Four continuum models were used: the MT_CKD (Mlawer-Tobin-Clough-Kn…
View article: Observations of the Clear-Sky Spectral Longwave Feedback at Surface Temperatures Between 210 K and 310 K
Observations of the Clear-Sky Spectral Longwave Feedback at Surface Temperatures Between 210 K and 310 K Open
View article: Effect of Uncertainty in Water Vapor Continuum Absorption on CO<sub>2</sub> Forcing, Longwave Feedback, and Climate Sensitivity
Effect of Uncertainty in Water Vapor Continuum Absorption on CO<sub>2</sub> Forcing, Longwave Feedback, and Climate Sensitivity Open
We investigate the effect of uncertainty in water vapor continuum absorption at terrestrial wavenumbers on CO 2 forcing , longwave feedback λ , and climate sensitivity at surface temperatures T s between 270 and 330 K. We calculate this un…
View article: Observations of the Clear-Sky Spectral Longwave Feedback at Surface Temperatures Between 210K and 310K
Observations of the Clear-Sky Spectral Longwave Feedback at Surface Temperatures Between 210K and 310K Open
The longwave feedback λ characterizes how Earth’s outgoing longwave radiation changes with surface temperature Ts, making it an important quantity to estimate Earth’s climate sensitivity. Compared to the traditionally studied λ, its spectr…
View article: Supplementary data for "Effect of Uncertainty in Water Vapor Continuum Absorption on CO2 Forcing, Longwave Feedback, and Climate Sensitivity"
Supplementary data for "Effect of Uncertainty in Water Vapor Continuum Absorption on CO2 Forcing, Longwave Feedback, and Climate Sensitivity" Open
This dataset is supplementary to the article "Effect of Uncertainty in Water Vapor Continuum Absorption on CO2 Forcing, Longwave Feedback, and Climate Sensitivity". spectral_olr.nc This file contains the spectral outgoing longwave radiatio…
View article: Effect of Uncertainty in Water Vapor Continuum Absorption on CO2 Forcing, Longwave Feedback, and Climate Sensitivity
Effect of Uncertainty in Water Vapor Continuum Absorption on CO2 Forcing, Longwave Feedback, and Climate Sensitivity Open
We assess the effect of uncertainty in water vapor continuum absorption on CO2 forcing F, longwave feedback λ, and climate sensitivity S at surface temperatures Ts between 270K and 330K. We calculate this uncertainty using a line-by-l…
View article: The Atmospheric Radiative Transfer Simulator Arts, Version 2.6 — Deep Python Integration
The Atmospheric Radiative Transfer Simulator Arts, Version 2.6 — Deep Python Integration Open
View article: Supplementary data for "Effect of Uncertainty in Water Vapor Continuum Absorption on CO2 Forcing, Longwave Feedback, and Climate Sensitivity"
Supplementary data for "Effect of Uncertainty in Water Vapor Continuum Absorption on CO2 Forcing, Longwave Feedback, and Climate Sensitivity" Open
This dataset is supplementary to the article "Effect of Uncertainty in Water Vapor Continuum Absorption on CO2 Forcing, Longwave Feedback, and Climate Sensitivity". spectral_olr.nc This file contains the spectral outgoing longwave radiatio…
View article: Effect of Uncertainty in Water Vapor Continuum Absorption on CO2 Forcing, Longwave Feedback, and Climate Sensitivity
Effect of Uncertainty in Water Vapor Continuum Absorption on CO2 Forcing, Longwave Feedback, and Climate Sensitivity Open
We assess the effect of uncertainty in water vapor continuum absorption on radiative forcing F, longwave feedback λ, and climate sensitivity S at surface temperatures Ts between 270K and 330K. We calculate this uncertainty using a line-by-…
View article: Supplementary data for "Effect of Uncertainty in Water Vapor Continuum Absorption on CO2 Forcing, Longwave Feedback, and Climate Sensitivity"
Supplementary data for "Effect of Uncertainty in Water Vapor Continuum Absorption on CO2 Forcing, Longwave Feedback, and Climate Sensitivity" Open
This dataset contains the spectral outgoing longwave radiation (OLR) calculated using the line-by-line radiative transfer model ARTS and the radiative-convective equilibrium model konrad. It contains spectral OLR for surface temperatures f…
View article: Publisher Correction: Direct observation of Earth’s spectral long-wave feedback parameter
Publisher Correction: Direct observation of Earth’s spectral long-wave feedback parameter Open
View article: Direct observation of Earth’s spectral long-wave feedback parameter
Direct observation of Earth’s spectral long-wave feedback parameter Open
View article: Direct observation of Earth’s spectral longwave feedback parameter
Direct observation of Earth’s spectral longwave feedback parameter Open
The spectral longwave feedback parameter λν represents how Earth’s outgoing longwave radiation adjusts to temperature changes and is thus the detailed fingerprint of all longwave feedbacks, directly impacting Earth’s …