Articles | Volume 14, issue 2
https://doi.org/10.5194/esd-14-443-2023
© Author(s) 2023. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/esd-14-443-2023
© Author(s) 2023. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
18 Apr 2023
Research article |
| 18 Apr 2023
| 18 Apr 2023
The modelled climatic response to the 18.6-year lunar nodal cycle and its role in decadal temperature trends
School of Environmental Sciences, University of East Anglia, Norwich
NR4 7TJ, United Kingdom
Climatic Research Unit, University of East Anglia, Norwich NR4 7TJ,
United Kingdom
Robert A. Hall
School of Environmental Sciences, University of East Anglia, Norwich
NR4 7TJ, United Kingdom
David P. Stevens
School of Mathematics, University of East Anglia, Norwich NR4 7TJ,
United Kingdom
Ed Hawkins
National Centre for Atmospheric Science, Department of Meteorology,
University of Reading, Reading RG6 6BB, United Kingdom
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Short summary
The 18.6-year lunar nodal cycle arises from variations in the angle of the Moon's orbital plane and affects ocean tides. In this work we use a climate model to examine the effect of this cycle on the ocean, surface, and atmosphere. The timing of anomalies is consistent with the so-called slowdown in global warming and has implications for when global temperatures will exceed 1.5 ℃ above pre-industrial levels. Regional anomalies have implications for seasonal climate areas such as Europe.
The 18.6-year lunar nodal cycle arises from variations in the angle of the Moon's orbital plane...
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