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Figure 6: Residuals of gravity tides, observed with gravimeter D-218 at Aswan station (from 2002 to 2004). Acknowledgements: The authors are indebted to the Department of Geophysics, Faculty of Science, Cairo University and the National Research Institute of Astronomy and Geophysics (NRIAG) for the encouragement of this work. We thank the Regional Seismological Center at Aswan for providing the facilities for the measurements. Finally we are grateful to the German Academic Exchange Service (DAAD) for supporting the work by travel funds to RMH and GJ. Figure 7: Fourier amplitude spectrum of residual gravity tide at Aswan station. References Agnew, D. C., 1996. SPOTL: Some programs for ocean - tide loading. Scripps Institution of Oceanography. SIO Reference Series 96-8. Dehant, V., 1987. Tidal parameters for an inelastic Earth. PEPI, Vol. pp. 97-116. Eanes, J., 1994. Diurnal and semidiurnal tides from TOPEX/POSEIDON altimetry (Abstract). Eos Trans. AGU, vol. 75(No. 16), Spring Meet. Suppl., 108p. Hartmann, T. and Wenzel, H. G., 1995a. The HW95 tidal potential catalogue. Geophys. Res. Lett., vol. 22, pp. 3553-3556. 11804
Hartmann, T. and Wenzel, H. G., 1995b. Catalogue HW95 of the tidal potential Bull. Inf. Marèes Terrestres, vol. 123, pp. 9278-9301. Hassan, R. M., 2007. Tidal gravity observations at Nasser Lake area, Aswan, Egypt. Dissertation, Geophysics Department, Faculty of Science, Cairo University, 147 pp. Jentzsch, G., 1995. Report of the Working Group on 'High Precision Tidal Data Processing'. Proc. 12th Int. Symp. Earth Tides, Beijing, August 1993, Science Press, Beijing, 1924. Jentzsch, G. and Koß, S., 1997. Interpretation of long-period tilt records at Blå Sjǿ, Southern Norway, with respect to the variations of the lake level. Phys. Chem. Earth, vol. 22, pp. 25 – 31. Weise, A., Jentzsch, G., Kiviniemi, A. and Kääriäinen, J., 1999. Comparison of long period tilt measurements: Results from the two clinomatic stations Metsähovi and Lohjia / Finland. J. of Geodynamics, vol. 27, pp. 237 – 257. Wenzel, H. G., 1994. PRETERNA a preprocessor for digitally recorded tidal data. Bull. d’Inf. Marèes Terr., vol. 118, pp. 8722 – 8734. Wenzel, H. G., 1996a. The nanogals software: Earth tide data processing package ETERNA 3.30. Bulletin d’Inf. Marèes Terr., vol. 124, pp. 9425 9439. Wenzel, H. G., 1997. Analysis of the Earth tide observations In: Wilhelm, H.,W. Zürn and H. -G. Wenzel (Eds),Tidal Phenomena. Lecture Notes in Earth Sciences, Springer Verlag, Berlin, Germany, pp. 59-75. Zahran, K. H., Jentzsch, G. and Seeber, G., 2005. World – wide synthetic tide parameters for gravity and vertical and horizontal displacements. J. Geod., vol. 79, pp. 293-299. Zahran, K. H., 2005. Benefit of tidal observations to gravity and GPS networks. Egyptian Geophys. Soc. Journal, vol. 3, No. 1, pp 89-98. 11805
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MAREES TERRESTRES BULLETIN D'INFORM
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1994), and TPXO.6 (Egbert et al., 1
Page 10 and 11: 4. An attempt to improve the region
Page 12 and 13: From Fig. 2, we also see that, the
Page 14 and 15: GPS network called GEONET (GPS Eart
Page 16 and 17: References Bos, M. S., Baker, T. F.
Page 18 and 19: Planets Space, 59, 307-311. Sato, T
Page 20 and 21: Fig. 1. Locations of the observatio
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Page 24 and 25: the dense seismic observation netwo
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Page 28 and 29: is done with an optical lever using
Page 30 and 31: 6. Application of laser interferome
Page 32 and 33: Figure 11. Strain seismograms of th
Page 34 and 35: Higashi, T., 1996, A study on chara
Page 38 and 39: 2. Fundamentals and techniques At t
Page 40 and 41: 100 low frequencies earth tide freq
Page 42 and 43: Tab. 4: Averages of noise levels at
Page 44 and 45: References Asch, G., Elstner, C., J
Page 46 and 47: The 1 / s part is also worth mentio
Page 48 and 49: As it was mentioned before the resu
Page 50 and 51: Fig. 9. Morlet Wavelet Spectrum, su
Page 52 and 53: 9. CONCLUSIONS This investigation w
Page 54 and 55: 2. Objectives of Aswan Tidal Gravit
Page 56 and 57: 5. Recording of Data The data logge
Page 58 and 59: Figure 5: Pre-processed hourly data
Page 64 and 65: time. In addition, models for gravi
Page 66 and 67: Fig. 3 (Zahran, 2005) shows gravity
Page 68 and 69: during the years 2003 and 2004. It
Page 70 and 71: Figure 7: Variation of phase shift,
Page 72 and 73: Figure 8: Induced gravity load and
Page 76 and 77: The instrumentation of the tidal st
Page 78 and 79: 4. Tidal analysis The tidal analysi
Page 80 and 81: References Banka, D., Crossley, D.
Page 82 and 83: 1. Introduction The estimation of a
Page 84 and 85: Figure 1 Air density distributions
Page 86 and 87: temperature effect is considered, t
Page 88 and 89: Figure 4 Attraction effect from the
Page 90 and 91: a ) up to 0.5° , b) 0.5°- 1.5° ,
Page 92 and 93: Figure 7 Atmospheric reductions for
Page 94 and 95: Figure 9 Amplitude spectra of diffe
Page 96 and 97: Figure 10 SG observation and gravit
Page 98 and 99: eduction in the long-period tides r
Page 100 and 101: oceans. The effect has a peak-to-pe
Page 104 and 105: Figure 1. Local earthquakes recorde
Page 106 and 107: 4. Recording of Data The recorded d
Page 108 and 109: Table 1: Adjusted tidal parameters
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Acknowledgements: The authors are i
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