Thorsten Mauritsen
Mauritsen, Thorsten, 1977-
VIAF ID: 24584233 (Personal)
Permalink: http://viaf.org/viaf/24584233
Preferred Forms
- 100 1 _ ‡a Mauritsen, Thorsten ‡d 1977-
- 100 1 _ ‡a Mauritsen, Thorsten ‡d 1977-
- 100 1 _ ‡a Mauritsen, Thorsten, ‡d 1977-
- 100 0 _ ‡a Thorsten Mauritsen
4xx's: Alternate Name Forms (4)
5xx's: Related Names (7)
- 510 2 _ ‡a Max-Planck-Institut für Meteorologie ‡4 affi ‡4 https://d-nb.info/standards/elementset/gnd#affiliation ‡e Affiliation
- 510 2 _ ‡a Max-Planck-Institut für Meteorologie
- 551 _ _ ‡a Sonderburg ‡4 ortg ‡4 https://d-nb.info/standards/elementset/gnd#placeOfBirth
- 510 2 _ ‡a Stockholms universitet. Meteorologiska institutionen
- 510 2 _ ‡a Stockholms universitet ‡b Meteorologiska institutionen
- 510 2 _ ‡a Universität Hamburg ‡b Fachbereich Geowissenschaften ‡4 affi ‡4 https://d-nb.info/standards/elementset/gnd#affiliation ‡e Affiliation
- 510 2 _ ‡a Universität Hamburg ‡b Fachbereich Geowissenschaften
Works
Title | Sources |
---|---|
Amplification of El Niño by cloud longwave coupling to atmospheric circulation | |
Analysis of the Moberg et al. (2005) hemispheric temperature reconstruction | |
Arctic amplification dominated by temperature feedbacks in contemporary climate models | |
An Arctic CCN-limited cloud-aerosol regime | |
Arctic Clouds and Surface Radiation – a critical comparison of satellite retrievals and the ERA-Interim reanalysis | |
The Arctic Summer Cloud Ocean Study (ASCOS): overview and experimental design | |
An assessment of Earth's climate sensitivity using multiple lines of evidence | |
The Atlantic Multidecadal Oscillation without a role for ocean circulation. | |
Atmospheric component of the MPI-M Earth System Model: ECHAM6 | |
Blocking prediction in an ensemble forecasting system | |
Bounding Global Aerosol Radiative Forcing of Climate Change | |
Climate and carbon cycle changes from 1850 to 2100 in MPI-ESM simulations for the Coupled Model Intercomparison Project phase 5 | |
Climate feedback efficiency and synergy | |
The climate of a retrograde rotating Earth | |
Cloud feedbacks in extratropical cyclones: insight from long-term satellite data and high-resolution global simulations | |
Clouds cooled the Earth | |
Comments on “Current GCMs' Unrealistic Negative Feedback in the Arctic” | |
Committed warming inferred from observations | |
Compensation of Hemispheric Albedo Asymmetries by Shifts of the ITCZ and Tropical Clouds | |
Developments in the MPI-M Earth System Model version 1.2 (MPI-ESM 1.2) and its response to increasing CO2 | |
Enhanced warming constrained by past trends in equatorial Pacific sea surface temperature gradient | |
Equilibrium Climate Sensitivity Estimated by Equilibrating Climate Models | |
Forcing and feedback in the MPI-ESM-LR coupled model under abruptly quadrupled CO2 | |
Graversen et al. reply | |
A Higher-resolution Version of the Max Planck Institute Earth System Model (MPI-ESM1.2-HR) | |
Historical warming and climate sensitivity | |
Historische Erwärmung und Klimasensitivität | |
Impact of melt ponds on Arctic sea ice in past and future climates as simulated by MPI-ESM | |
The impact of parametrized convection on cloud feedback | |
Improving a global model from the boundary layer: Total turbulent energy and the neutral limit Prandtl number | |
The Influence of Cloud Feedbacks on Equatorial Atlantic Variability | |
The influence of internal variability on Earth's energy balance framework and implications for estimating climate sensitivity | |
MACv2-SP: a parameterization of anthropogenic aerosol optical properties and an associated Twomey effect for use in CMIP6 | |
Mesoscale Variability in the Summer Arctic Boundary Layer | |
Mixed-phase clouds cause climate model biases in Arctic wintertime temperature inversions | |
Model Description | |
Model Evaluation | |
Modelling atmospheric structure, cloud and their response to CCN in the central Arctic: ASCOS case studies | |
New Generation of Climate Models Track Recent Unprecedented Changes in Earth's Radiation Budget Observed by CERES | |
A New Perspective for Future Precipitation Change from Intense Extratropical Cyclones | |
Observations of Stably Stratified Shear-Driven Atmospheric Turbulence at Low and High Richardson Numbers | |
The Observed Hemispheric Symmetry in Reflected Shortwave Irradiance | |
On the Effect of Historical SST Patterns on Radiative Feedback | |
On the Potential for Abrupt Arctic Winter Sea Ice Loss | |
On the sensitivity of anthropogenic aerosol forcing to model-internal variability and parameterizing a Twomey effect | |
On the use of shear-dependent turbulent length-scales | |
Performance of an Eddy Diffusivity–Mass Flux Scheme for Shallow Cumulus Boundary Layers | |
Radiative convective equilibrium as a framework for studying the interaction between convection and its large-scale environment | |
The respective roles of surface temperature driven feedbacks and tropospheric adjustment to CO2 in CMIP5 transient climate simulations | |
Separation of Contributions from Radiative Feedbacks to Polar Amplification on an Aquaplanet | |
Simulating the Role of Subtropical Stratocumulus Clouds in Driving Pacific Climate Variability | |
Single-Column Model Intercomparison for a Stably Stratified Atmospheric Boundary Layer | |
Small global-mean cooling due to volcanic radiative forcing | |
The subtle origins of surface-warming hiatuses | |
A transitioning Arctic surface energy budget: the impacts of solar zenith angle, surface albedo and cloud radiative forcing | |
Tuning the climate of a global model | |
Turbulence energetics in stably stratified geophysical flows: Strong and weak mixing regimes | |
The Turbulent Structure of the Arctic Summer Boundary Layer During The Arctic Summer Cloud-Ocean Study | |
Understanding the Intermodel Spread in Global-Mean Hydrological Sensitivity* | |
Vertical structure of recent Arctic warming | |
Warm winds from the Pacific caused extensive Arctic sea-ice melt in summer 2007 | |
Wave Flow Simulations Over Arctic Leads | |
Why is it so difficult to represent stably stratified conditions in numerical weather prediction (NWP) models? |