Articles | Volume 16, issue 20
https://doi.org/10.5194/acp-16-12925-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/acp-16-12925-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article
| 
19 Oct 2016
Research article |
| 19 Oct 2016
How can we understand the global distribution of the solar cycle signal on the Earth's surface?
Kunihiko Kodera
CORRESPONDING AUTHOR
Institute for Space-Earth Environmental Research, Nagoya University, Nagoya, 464-8601, Japan
Rémi Thiéblemont
Laboratoire Atmosphères Milieux Observations Spatiales, 78280 Guyancourt, France
Seiji Yukimoto
Meteorological Research Institute, Tsukuba, 305-0052, Japan
Katja Matthes
Research Division Ocean Circulation and Climate, GEOMAR Helmholtz
Centre for Ocean Research, 24105 Kiel, Germany
Christian-Albrechts Universität zu Kiel, 24105 Kiel, Germany
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34 citations as recorded by crossref.
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- Changing response of the North Atlantic/European winter climate to the 11 year solar cycle H. Ma et al. 10.1088/1748-9326/aa9e94
33 citations as recorded by crossref.
- Solar activity modulates the El Niño‐Southern Oscillation‐induced precipitation anomalies over southern China in early spring H. Ma et al. 10.1002/joc.7214
- Complex imprint of solar variability on tree rings A. Land et al. 10.1088/2515-7620/abc063
- Delayed North Atlantic Response to Solar Forcing of the Stratospheric Polar Vortex S. Yukimoto et al. 10.2151/sola.2017-010
- Stratospheric tropical warming event and its impact on the polar and tropical troposphere K. Kodera et al. 10.5194/acp-17-615-2017
- Influence of the Solar Cycle on the North Atlantic Oscillation Y. Kuroda et al. 10.1029/2021JD035519
- Combined effect of the solar activity and ENSO on the tropical cyclone genesis frequency in the southeastern part of the western North Pacific S. Li et al. 10.3389/feart.2023.1139699
- 11-year solar cycle influences on the late-wintertime South Asian jet variability H. Ma et al. 10.3389/feart.2023.1203954
- Modulation of the solar activity on the connection between the NAO and the tropical pacific SST variability W. Huo et al. 10.3389/feart.2023.1147582
- A Reconstruction of Subtropical Western North Pacific SST Variability Back to 1578, Based on a Porites Coral Sr/Ca Record from the Northern Ryukyus, Japan Y. Kawakubo et al. 10.1002/2017PA003203
- Zonally asymmetric influences of the quasi-biennial oscillation on stratospheric ozone W. Wang et al. 10.5194/acp-22-13695-2022
- Equilibrium Climate after Spectral and Bolometric Irradiance Reduction in Grand Solar Minimum Simulations N. Tartaglione et al. 10.3390/cli12010001
- Analysis of solar cycle-like signal in the North Atlantic Oscillation index A. Gruzdev & V. Bezverkhnii 10.1016/j.jastp.2019.03.009
- The possible impact of solar activity on the summer temperature distribution over Eurasia W. Lu et al. 10.3389/feart.2022.1087737
- Impact of Solar Activity and ENSO on the Early Summer Asian Monsoon During the Last Millennium P. Chen et al. 10.1029/2023GL105668
- Solar wind signal in the wintertime North Atlantic oscillation and Northern Hemispheric circulation Z. Zhu et al. 10.1002/joc.6461
- Energy transmission processes in the effectuation chain of solar forcing to the terrestrial atmosphere—a review J. Wang et al. 10.3389/feart.2023.1164636
- The Sun's role in decadal climate predictability in the North Atlantic A. Drews et al. 10.5194/acp-22-7893-2022
- Asymmetric modulation of solar activity on tropical cyclone frequency over the western North Pacific and the possible mechanism D. Li et al. 10.3389/feart.2023.1169685
- On the Origin of the Solar Cycle Modulation of the Southern Annular Mode Y. Kuroda 10.1002/2017JD027091
- Lagged Responses of the Tropical Pacific to the 11-yr Solar Cycle Forcing and Possible Mechanisms W. Huo et al. 10.1007/s13351-021-0137-8
- Preferred solar signal and its transfer in the Asian–Pacific subtropical jet region D. Li et al. 10.1007/s00382-018-4443-5
- Simulating the atmospheric response to the 11-year solar cycle forcing with the UM-UKCA model: the role of detection method and natural variability E. Bednarz et al. 10.5194/acp-19-5209-2019
- Influences of the 11-yr Sunspot Cycle and Polar Vortex Oscillation on Observed Winter Temperature Variations in China C. Lu & B. Zhou 10.1007/s13351-018-7101-2
- Variability of Sunlight Duration in Tomsk in 1961–2018 T. Sklyadneva & B. Belan 10.1134/S1024856020030112
- The Footprint of the 11‐Year Solar Cycle in Northeastern Pacific SSTs and Its Influence on the Central Pacific El Niño Y. Lin et al. 10.1029/2020GL091369
- Influences of Solar Forcing at Ultraviolet and Longer Wavelengths on Climate D. Shindell et al. 10.1029/2019JD031640
- Separating the role of direct radiative heating and photolysis in modulating the atmospheric response to the amplitude of the 11-year solar cycle forcing E. Bednarz et al. 10.5194/acp-19-9833-2019
- Interdisciplinary studies of solar activity and climate change Z. XIAO et al. 10.1080/16742834.2017.1321951
- Modulations of solar activity on El Niño Modoki and possible mechanisms W. Huo & Z. Xiao 10.1016/j.jastp.2017.05.008
- The Combined Effects of ENSO and Solar Activity on Mid-Winter Precipitation Anomalies Over Southern China R. Wang et al. 10.3389/feart.2021.771234
- Robust Solar Signature in Late Winter Precipitation Over Southern China H. Ma et al. 10.1029/2019GL084083
- Role Of the Sun and the Middle atmosphere/thermosphere/ionosphere In Climate (ROSMIC): a retrospective and prospective view W. Ward et al. 10.1186/s40645-021-00433-8
- Detecting Relationship between the North–South Difference in Extreme Precipitation and Solar Cycle in China J. Liu et al. 10.3390/atmos15020175
1 citations as recorded by crossref.
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Discussed (final revised paper)
Latest update: 20 Nov 2024
Short summary
The spatial structure of the solar cycle signals on the Earth's surface is analysed to identify the mechanisms. Both tropical and extratropical solar surface signals can result from circulation changes in the upper stratosphere through (i) a downward migration of wave zonal mean flow interactions and (ii) changes in the stratospheric mean meridional circulation. Amplification of the solar signal also occurs through interaction with the ocean.
The spatial structure of the solar cycle signals on the Earth's surface is analysed to identify...
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