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Climate Dynamics

, Volume 47, Issue 1–2, pp 667–678 | Cite as

Global patterns of solar influence on high cloud cover

  • Mihai Dima
  • Mirela Voiculescu
Article

Abstract

One of the main sources of uncertainty in climate projections is represented by clouds, which have a profound influence on the Earth’s radiation budget through the feedbacks in which they are involved. The improvement of clouds representation in General Circulation Models relies largely on constraints derived from observations and on correct identification of processes that influence cloud formation or lifetime. Here we identify solar forced high cloud cover (HCC) patterns in reanalysis and observed data extending over the 1871–2009 period, based on their associations with known fingerprints of the same forcing on surface air temperature, sea surface temperature (SST) and sea level pressure fields. The solar influence on HCC has maximum amplitudes over the Pacific basin, where HCC anomalies are distributed in bands of alternating polarities. The colocation of the HCC and SST anomalies bands indicates a thermal influence on high clouds through convection and an amplification of the HCC anomalies by a positive feedback of long-wave fluxes, which increases the solar signal. Consistent with numerical simulations, the solar forced HCC pattern appears to be generated through a constructive interference between the so-called “top-down” and “bottom-up” mechanisms of solar influence on climate and is amplified by ocean–atmosphere positive feedbacks.

Keywords

High clouds Solar forcing Pacific Ocean Convection 

Notes

Acknowledgments

This work was supported by project PN-II-ID-PCE-2011-3-0709, SOLACE (IDEI 283) of the Romanian National Authority for Scientific Research, CNCS, UEFISCDI. ISCCP project is acknowledged for the cloud data. Support for the Twentieth Century Reanalysis Project dataset is provided by the U.S. Department of Energy, Office of Science Innovative and Novel Computational Impact on Theory and Experiment program, and Office of Biological and Environmental Research, and by the National Oceanic and Atmospheric Administration Climate Program Office. We thank two anonymous reviewers for their constructive comments, which contributed to a significant improvement of the manuscript.

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Copyright information

© Springer-Verlag Berlin Heidelberg 2015

Authors and Affiliations

  1. 1.Faculty of PhysicsUniversity of BucharestBucharestRomania
  2. 2.University “Dunărea de Jos” of GalaţiGalaţiRomania

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