Articles | Volume 8, issue 3
https://doi.org/10.5194/esd-8-849-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/esd-8-849-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article
| Highlight paper
| 
25 Sep 2017
Research article | Highlight paper |
| 25 Sep 2017
An explanation for the different climate sensitivities of land and ocean surfaces based on the diurnal cycle
Biospheric Theory and Modelling Group, Max-Planck-Institut für Biogeochemie, Jena, Germany
Maik Renner
Biospheric Theory and Modelling Group, Max-Planck-Institut für Biogeochemie, Jena, Germany
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Total article views: 5,429 (including HTML, PDF, and XML)
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Cited
20 citations as recorded by crossref.
- Radiation as the dominant cause of high-temperature extremes on the eastern Tibetan Plateau Y. Tian et al. 10.1088/1748-9326/acd805
- Radiative controls by clouds and thermodynamics shape surface temperatures and turbulent fluxes over land S. Ghausi et al. 10.1073/pnas.2220400120
- Working at the limit: a review of thermodynamics and optimality of the Earth system A. Kleidon 10.5194/esd-14-861-2023
- What limits photosynthesis? Identifying the thermodynamic constraints of the terrestrial biosphere within the Earth system A. Kleidon 10.1016/j.bbabio.2020.148303
- The Importance of Heat Storage for Estimating Lake Evaporation on Different Time Scales: Insights From a Large Shallow Subtropical Lake P. Bai & Y. Wang 10.1029/2023WR035123
- Year-long atmospheric characterization effort for laser weapon testing on the Potomac River Test Range at the Naval Surface Warfare Center Dahlgren Division E. Bates et al. 10.1117/1.OE.61.7.076105
- Diurnal land surface energy balance partitioning estimated from the thermodynamic limit of a cold heat engine A. Kleidon & M. Renner 10.5194/esd-9-1127-2018
- Understanding variations in downwelling longwave radiation using Brutsaert's equation Y. Tian et al. 10.5194/esd-14-1363-2023
- Evaporation from a large lowland reservoir – (dis)agreement between evaporation models from hourly to decadal timescales F. Jansen & A. Teuling 10.5194/hess-24-1055-2020
- Meta-pragmatic investigation of passive strategies from ‘UHI– climatology’ nexus perspective with digital twin as assessment mechanism M. Elnabawi & R. Raveendran 10.1016/j.jum.2024.03.002
- A Maximum Entropy Production Hypothesis for Time Varying Climate Problems: Illustration on a Conceptual Model for the Seasonal Cycle V. Labarre et al. 10.3390/e22090966
- Evaporation from a large lowland reservoir – observed dynamics and drivers during a warm summer F. Jansen et al. 10.5194/hess-26-2875-2022
- Using phase lags to evaluate model biases in simulating the diurnal cycle of evapotranspiration: a case study in Luxembourg M. Renner et al. 10.5194/hess-23-515-2019
- The second law of thermodynamics, life and Earth‘s planetary machinery revisited A. Kleidon 10.1016/j.plrev.2024.10.009
- Do Surface and Air Temperatures Contain Similar Imprints of Evaporative Conditions? A. Panwar et al. 10.1029/2019GL082248
- How aerosols and greenhouse gases influence the diurnal temperature range C. Stjern et al. 10.5194/acp-20-13467-2020
- Sonne oder Treibhauseffekt? A. Kleidon 10.1002/piuz.202001560
- Testing a maximum evaporation theory over saturated land: implications for potential evaporation estimation Z. Tu et al. 10.5194/hess-26-1745-2022
- Diurnal Cycle of Surface Air Temperature within China in Current Reanalyses: Evaluation and Diagnostics J. Du et al. 10.1175/JCLI-D-17-0773.1
- Stronger Global Warming on Nonrainy Days in Observations From China M. Du et al. 10.1029/2019JD031792
20 citations as recorded by crossref.
- Radiation as the dominant cause of high-temperature extremes on the eastern Tibetan Plateau Y. Tian et al. 10.1088/1748-9326/acd805
- Radiative controls by clouds and thermodynamics shape surface temperatures and turbulent fluxes over land S. Ghausi et al. 10.1073/pnas.2220400120
- Working at the limit: a review of thermodynamics and optimality of the Earth system A. Kleidon 10.5194/esd-14-861-2023
- What limits photosynthesis? Identifying the thermodynamic constraints of the terrestrial biosphere within the Earth system A. Kleidon 10.1016/j.bbabio.2020.148303
- The Importance of Heat Storage for Estimating Lake Evaporation on Different Time Scales: Insights From a Large Shallow Subtropical Lake P. Bai & Y. Wang 10.1029/2023WR035123
- Year-long atmospheric characterization effort for laser weapon testing on the Potomac River Test Range at the Naval Surface Warfare Center Dahlgren Division E. Bates et al. 10.1117/1.OE.61.7.076105
- Diurnal land surface energy balance partitioning estimated from the thermodynamic limit of a cold heat engine A. Kleidon & M. Renner 10.5194/esd-9-1127-2018
- Understanding variations in downwelling longwave radiation using Brutsaert's equation Y. Tian et al. 10.5194/esd-14-1363-2023
- Evaporation from a large lowland reservoir – (dis)agreement between evaporation models from hourly to decadal timescales F. Jansen & A. Teuling 10.5194/hess-24-1055-2020
- Meta-pragmatic investigation of passive strategies from ‘UHI– climatology’ nexus perspective with digital twin as assessment mechanism M. Elnabawi & R. Raveendran 10.1016/j.jum.2024.03.002
- A Maximum Entropy Production Hypothesis for Time Varying Climate Problems: Illustration on a Conceptual Model for the Seasonal Cycle V. Labarre et al. 10.3390/e22090966
- Evaporation from a large lowland reservoir – observed dynamics and drivers during a warm summer F. Jansen et al. 10.5194/hess-26-2875-2022
- Using phase lags to evaluate model biases in simulating the diurnal cycle of evapotranspiration: a case study in Luxembourg M. Renner et al. 10.5194/hess-23-515-2019
- The second law of thermodynamics, life and Earth‘s planetary machinery revisited A. Kleidon 10.1016/j.plrev.2024.10.009
- Do Surface and Air Temperatures Contain Similar Imprints of Evaporative Conditions? A. Panwar et al. 10.1029/2019GL082248
- How aerosols and greenhouse gases influence the diurnal temperature range C. Stjern et al. 10.5194/acp-20-13467-2020
- Sonne oder Treibhauseffekt? A. Kleidon 10.1002/piuz.202001560
- Testing a maximum evaporation theory over saturated land: implications for potential evaporation estimation Z. Tu et al. 10.5194/hess-26-1745-2022
- Diurnal Cycle of Surface Air Temperature within China in Current Reanalyses: Evaluation and Diagnostics J. Du et al. 10.1175/JCLI-D-17-0773.1
- Stronger Global Warming on Nonrainy Days in Observations From China M. Du et al. 10.1029/2019JD031792
Latest update: 20 Nov 2024
Short summary
We provide an explanation why land temperatures respond more strongly to global warming than ocean temperatures, a robust finding in observations and models that has so far not been understood well. We explain it by the different ways by which ocean and land surfaces buffer the strong variation in solar radiation and demonstrate this with a simple, physically based model. Our explanation also illustrates why nighttime temperatures warm more strongly, another robust finding of global warming.
We provide an explanation why land temperatures respond more strongly to global warming than...
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