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    Signal Amplitude Uncertainty of a Digiquartz Pressure Transducer Due to Static Calibration Error 

    Source: Journal of Atmospheric and Oceanic Technology:;1994:;volume( 011 ):;issue: 005:;page 1381
    Author(s): Boss, Edward F.; González, Frank I.
    Publisher: American Meteorological Society
    Abstract: Standard calibrations of Digiquartz pressure transducers are performed over a very wide range of pressure and temperature, typically 14?10 000 psia and 1°?125°C. Compared to this large calibration domain, deep ocean bottom ...
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    Corrections to Bottom Pressure Records for Dynamic Temperature Response 

    Source: Journal of Atmospheric and Oceanic Technology:;1995:;volume( 012 ):;issue: 004:;page 915
    Author(s): Boss, Edward F.; González, Frank I.
    Publisher: American Meteorological Society
    Abstract: Factory calibration of Digiquartz? transducers allows for static temperature corrections, assuming that the temperature changes slowly enough during deployment that the gauge is always in thermal equilibrium. Deep ocean ...
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    The Harmonic Constant Datum Method: Options for Overcoming Datum Discontinuities at Mixed–Diurnal Tidal Transitions 

    Source: Journal of Atmospheric and Oceanic Technology:;2004:;volume( 021 ):;issue: 001:;page 95
    Author(s): Mofjeld, Harold O.; Venturato, Angie J.; González, Frank I.; Titov, Vasily V.; Newman, Jean C.
    Publisher: American Meteorological Society
    Abstract: The harmonic constant datum (HCD) method is a computationally efficient way of estimating tidal datums relative to mean sea level, without the need to compute long time series. However, datum discontinuities can occur ...
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    Effects of Tides on Maximum Tsunami Wave Heights: Probability Distributions 

    Source: Journal of Atmospheric and Oceanic Technology:;2007:;volume( 024 ):;issue: 001:;page 117
    Author(s): Mofjeld, Harold O.; González, Frank I.; Titov, Vasily V.; Venturato, Angie J.; Newman, Jean C.
    Publisher: American Meteorological Society
    Abstract: A theoretical study was carried out to understand how the probability distribution for maximum wave heights (?m) during tsunamis depends on the initial tsunami amplitude (A) and the tides. It was assumed that the total ...
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