Articles | Volume 9, issue 1
Earth Syst. Dynam., 9, 299–311, 2018
https://doi.org/10.5194/esd-9-299-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Special issue: The Earth system at a global warming of 1.5°C and 2.0°C
Research article 28 Mar 2018
Research article | 28 Mar 2018
Changes in extremely hot days under stabilized 1.5 and 2.0 °C global warming scenarios as simulated by the HAPPI multi-model ensemble
Michael Wehner et al.
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Cited
17 citations as recorded by crossref.
- Characterization of long period return values of extreme daily temperature and precipitation in the CMIP6 models: Part 2, projections of future change M. Wehner 10.1016/j.wace.2020.100284
- Change in the heatwave statistical characteristics over China during the climate warming slowdown X. Li et al. 10.1016/j.atmosres.2020.105152
- Global aridity changes due to differences in surface energy and water balance between 1.5 °C and 2 °C warming A. Takeshima et al. 10.1088/1748-9326/ab9db3
- High‐Temperature Extreme Events Over Africa Under 1.5 and 2 °C of Global Warming S. Nangombe et al. 10.1029/2018JD029747
- Heat wave Intensity Duration Frequency Curve: A Multivariate Approach for Hazard and Attribution Analysis O. Mazdiyasni et al. 10.1038/s41598-019-50643-w
- Historical and future anthropogenic warming effects on droughts, fires and fire emissions of CO<sub>2</sub> and PM<sub>2.5</sub> in equatorial Asia when 2015-like El Niño events occur H. Shiogama et al. 10.5194/esd-11-435-2020
- Contribution of mean climate to hot temperature extremes for present and future climates A. Di Luca et al. 10.1016/j.wace.2020.100255
- Mid-summer surface air temperature and its internal variability over China at 1.5 °C and 2 °C global warming S. YIN et al. 10.1016/j.accre.2020.09.005
- Projected changes in mid–high‐latitude Eurasian climate during boreal spring in a 1.5 and 2°C warmer world S. Chen et al. 10.1002/joc.6306
- Expansion of drylands in China with an additional half a degree warming Q. Yang et al. 10.1002/joc.7052
- Differential Impacts of 1.5 and 2 °C Warming on Extreme Events Over China Using Statistically Downscaled and Bias-Corrected CESM Low-Warming Experiment Y. Yang et al. 10.1029/2018GL079272
- Climatic suitability and spatial distribution for summer maize cultivation in China at 1.5 and 2.0 °C global warming Q. He et al. 10.1016/j.scib.2019.03.030
- Drylands climate response to transient and stabilized 2 °C and 1.5 °C global warming targets Y. Wei et al. 10.1007/s00382-019-04860-8
- Arctic amplification under global warming of 1.5 and 2 °C in NorESM1-Happi L. Graff et al. 10.5194/esd-10-569-2019
- Changes in extreme temperature over China when global warming stabilized at 1.5 °C and 2.0 °C C. Sun et al. 10.1038/s41598-019-50036-z
- Midlatitude atmospheric circulation responses under 1.5 and 2.0 °C warming and implications for regional impacts C. Li et al. 10.5194/esd-9-359-2018
- Changes in tropical cyclones under stabilized 1.5 and 2.0 °C global warming scenarios as simulated by the Community Atmospheric Model under the HAPPI protocols M. Wehner et al. 10.5194/esd-9-187-2018
15 citations as recorded by crossref.
- Characterization of long period return values of extreme daily temperature and precipitation in the CMIP6 models: Part 2, projections of future change M. Wehner 10.1016/j.wace.2020.100284
- Change in the heatwave statistical characteristics over China during the climate warming slowdown X. Li et al. 10.1016/j.atmosres.2020.105152
- Global aridity changes due to differences in surface energy and water balance between 1.5 °C and 2 °C warming A. Takeshima et al. 10.1088/1748-9326/ab9db3
- High‐Temperature Extreme Events Over Africa Under 1.5 and 2 °C of Global Warming S. Nangombe et al. 10.1029/2018JD029747
- Heat wave Intensity Duration Frequency Curve: A Multivariate Approach for Hazard and Attribution Analysis O. Mazdiyasni et al. 10.1038/s41598-019-50643-w
- Historical and future anthropogenic warming effects on droughts, fires and fire emissions of CO<sub>2</sub> and PM<sub>2.5</sub> in equatorial Asia when 2015-like El Niño events occur H. Shiogama et al. 10.5194/esd-11-435-2020
- Contribution of mean climate to hot temperature extremes for present and future climates A. Di Luca et al. 10.1016/j.wace.2020.100255
- Mid-summer surface air temperature and its internal variability over China at 1.5 °C and 2 °C global warming S. YIN et al. 10.1016/j.accre.2020.09.005
- Projected changes in mid–high‐latitude Eurasian climate during boreal spring in a 1.5 and 2°C warmer world S. Chen et al. 10.1002/joc.6306
- Expansion of drylands in China with an additional half a degree warming Q. Yang et al. 10.1002/joc.7052
- Differential Impacts of 1.5 and 2 °C Warming on Extreme Events Over China Using Statistically Downscaled and Bias-Corrected CESM Low-Warming Experiment Y. Yang et al. 10.1029/2018GL079272
- Climatic suitability and spatial distribution for summer maize cultivation in China at 1.5 and 2.0 °C global warming Q. He et al. 10.1016/j.scib.2019.03.030
- Drylands climate response to transient and stabilized 2 °C and 1.5 °C global warming targets Y. Wei et al. 10.1007/s00382-019-04860-8
- Arctic amplification under global warming of 1.5 and 2 °C in NorESM1-Happi L. Graff et al. 10.5194/esd-10-569-2019
- Changes in extreme temperature over China when global warming stabilized at 1.5 °C and 2.0 °C C. Sun et al. 10.1038/s41598-019-50036-z
2 citations as recorded by crossref.
- Midlatitude atmospheric circulation responses under 1.5 and 2.0 °C warming and implications for regional impacts C. Li et al. 10.5194/esd-9-359-2018
- Changes in tropical cyclones under stabilized 1.5 and 2.0 °C global warming scenarios as simulated by the Community Atmospheric Model under the HAPPI protocols M. Wehner et al. 10.5194/esd-9-187-2018
Saved (final revised paper)
Latest update: 21 Apr 2021
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Short summary
The United Nations Framework Convention on Climate Change challenged the scientific community to describe the impacts of stabilizing the global temperature at its 21st Conference of Parties. A specific target of 1.5 °C above preindustrial levels had not been seriously considered by the climate modeling community prior to the Paris Agreement. This paper analyzes heat waves in simulations designed for this target. We find there are reductions in extreme temperature compared to a 2 °C target.
The United Nations Framework Convention on Climate Change challenged the scientific community to...
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