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Fig. 1. Locations of the observation sites used in this study. An open square, a diamond, open circles, and closed circles indicate the tidal gravity, continuous GPS, continuous tide gauges, and temporal tide gauges installed by UAF (Larsen, 2003), respectively. 11764
Fig. 2. Phasor plots for the observed and predicted tides at four sites of EGAN (gravity) and AB48, AB50, and AB51 (displacement). Units of both the horizontal and vertical axes are in Gal and cm for the gravity and displacement, respectively. For the displacement, the vector sums of three components of NS, EW and UD are plotted. The six combinations of the predicted body tide and the regional ocean tide model (Model A or B) are plotted with the following symbols; (1) Cross denoted with ‘+’: Predictions from WAHR and Model A, (2) Stars: DDW_EL_HY and Model A; (3) Open circle: DDW_IE_NH and Model A, (4) Cross denoted with ‘ x’: WAHR and Model B, (5) Open square: DDW_EL_HY and Model B, and (6) Open triangle: DDW_IE_NH and Model B. See Section 5 of the text for the abbreviations of the body tides. 11765
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Page 6 and 7: BIM 146 December 15, 2010 New Chall
Page 8 and 9: 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
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Page 24 and 25: the dense seismic observation netwo
Page 26 and 27: difference of loading effects of oc
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 60 and 61: Figure 6: Residuals of gravity tide
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
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Figure 7: Variation of phase shift,
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Figure 8: Induced gravity load and
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The instrumentation of the tidal st
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4. Tidal analysis The tidal analysi
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References Banka, D., Crossley, D.
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1. Introduction The estimation of a
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Figure 1 Air density distributions
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temperature effect is considered, t
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Figure 4 Attraction effect from the
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a ) up to 0.5° , b) 0.5°- 1.5° ,
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Figure 7 Atmospheric reductions for
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Figure 9 Amplitude spectra of diffe
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Figure 10 SG observation and gravit
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eduction in the long-period tides r
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oceans. The effect has a peak-to-pe
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Figure 1. Local earthquakes recorde
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4. Recording of Data The recorded d
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Table 1: Adjusted tidal parameters
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Acknowledgements: The authors are i
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