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Yavor Chapanov , E-mail: chapanov@clg.bas.bg

Yavor Chapanov , E-mail: chapanov@clg.bas.bg Central Laboratory for Geodes at Bulgarian Academy of Sciences “Acad. G. Bonchev” Str., Bl.1, Sofia 1113, Bulgaria. Daniel Gambis , Е -mail: daniel.gambis@obspm.fr IERS EOP PC , Observatoire de Paris 61,

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Yavor Chapanov , E-mail: chapanov@clg.bas.bg

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  1. Yavor Chapanov, E-mail: chapanov@clg.bas.bg Central Laboratory for Geodes at Bulgarian Academy of Sciences “Acad. G. Bonchev” Str., Bl.1, Sofia 1113, Bulgaria Daniel Gambis, Е-mail: daniel.gambis@obspm.fr IERS EOP PC, Observatoire de Paris 61, Аvenue de l'Observatoire, 75014 Paris, France

  2. BALWOIS 2010 CONFERENCE, 25-29 May 2010, Ohrid, Republic of Macedonia EARTH ROTATION DATA -Length of Day (LOD) and Universal Time (UT1) - 1623-2010 SOLAR DATA -Wolf’s numbers Wn and extended 22-year Wn/22a - 1700-2010 -Total Solar Irradiance (TSI) - 1610-2010 -Sunspot areas of Southern Ss and Northern Snhemispheres, Equatorial solar asymmetry Sa=(Ss-Sn)/(Ss+Sn) - 1874-2010 MEAN SEA LEVEL DATA from maregraph stations: -Stockholm 1774-2000 -Other stations ICE THICKNESS DATA -Antarctic station Lomonosovfonna 1657-1973, -Greenland station Agassiz Ice Cap 1622-1983

  3. BALWOIS 2010 CONFERENCE, 25-29 May 2010, Ohrid, Republic of Macedonia

  4. BALWOIS 2010 CONFERENCE, 25-29 May 2010, Ohrid, Republic of Macedonia Global water redistribution TSI increase during solar maxima Additional water evaporation MSL decrease Continentalice thicknessincrease Axial moment of inertia decrease Angular velocity increase LOD decrease UT1 increase

  5. BALWOIS 2010 CONFERENCE, 25-29 May 2010, Ohrid, Republic of Macedonia 11-year oscillations 22-year oscillations 45-year oscillations COMMON 11-, 22- AND 45-YEAR CYCLES Maximal TSI amplitudes 0.2–0.5W/m2

  6. BALWOIS 2010 CONFERENCE, 25-29 May 2010, Ohrid, Republic of Macedonia Table 1. Amplitudes A11, A22.5, A45, of the 11.25-year, 22.5-year and 45-year oscillations of the mean sea level for some maregraph stations.

  7. BALWOIS 2010 CONFERENCE, 25-29 May 2010, Ohrid, Republic of Macedonia Separation between solar and Earth liquid core effects

  8. BALWOIS 2010 CONFERENCE, 25-29 May 2010, Ohrid, Republic of Macedonia CONCLUSIONS • The model of global water redistribution during solar cycles depends on the proper value of the transfer coefficient between the homogeneous elastic sphere and the real Earth. The value of the transfer coefficient k varies between 5.4 and 10.5. In case of great MSL changes, the value of k is 10.5 and in case of small MSL amplitudes this coefficient is closed to 6. It is possible to determine the value of k by means of all data of temporal changes of the continental water storage. • The proposed model of global water redistribution determine the relationships between the observed periodical oscillations at the solar activity frequencies of the Earth rotation, mean sea level and ice thickness accumulation rate over the polar continental ice sheets. It is possible to reconstruct the periodical behavior of the global hydrological cycles by means of available astronomical data, or to reconstruct Earth rotation data by means of available hydrological and glacial data.

  9. BALWOIS 2010 CONFERENCE, 25-29 May 2010, Ohrid, Republic of Macedonia THANK YOU END

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