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Advances in Science and Research Contributions in Applied Meteorology and Climatology
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Volume 6, issue 1
Adv. Sci. Res., 6, 63–67, 2011
https://doi.org/10.5194/asr-6-63-2011
© Author(s) 2011. This work is distributed under
the Creative Commons Attribution 3.0 License.
Adv. Sci. Res., 6, 63–67, 2011
https://doi.org/10.5194/asr-6-63-2011
© Author(s) 2011. This work is distributed under
the Creative Commons Attribution 3.0 License.

  31 Mar 2011

31 Mar 2011

Correlation between air-sea heat fluxes over the Aegean Sea and the total precipitable water over Europe and North Africa

V. P. Papadopoulos1, A. Bartzokas2, T. Chronis1, S. Ruiz3, N. Zarokanellos1, and G. Ferentinos4 V. P. Papadopoulos et al.
  • 1Hellenic Centre for Marine Research, Anavissos, Greece
  • 2Department of Physics, University of Ioannina, Greece
  • 3IMEDEA (CSIC-UIB), Mallorca, Spain
  • 4Department of Geology, University of Patras, Greece

Abstract. The relation between the air-sea heat fluxes in the Aegean Sea and the total precipitable water (TPW) over Europe and North Africa is investigated. An one-point linear correlation between the components of surface heat exchange and TPW is employed. During winter and for the shortwave radiation, a dipole of opposite correlation (see-saw teleconnection), is observed between the northeast Europe and the East Mediterranean Sea. This pattern is inverted for the longwave radiation and especially during the summer is limited to a strong positive south pole. Both spatial correlation patterns underline the influence of cloudiness during the winter season and the specific humidity during summer on the radiative fluxes behavior. Regarding the turbulent air-sea heat flux components – latent and sensible heat – the correlation pattern is enhanced. The winter pattern exhibits positive correlation over Europe with the highest values (r>0.75) over the Balkan Peninsula. The identified correlation patterns, although they remain dominant, weaken during the summer. The herein findings suggest that the stronger relation between the TPW and the turbulent fluxes is regulated by the wind regime.

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