Results 251 to 260 of about 1,391,406 (302)
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2010
After a general theoretical consideration of basic mathematical aspects, we give numerical and physical details for the last two decades, where global and reliable data are available. The concept of a “mean sea level” is in itself rather artificial, because sea level varies at various temporal and spatial scales.
Luciana Fenoglio-Marc, Erwin Groten
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After a general theoretical consideration of basic mathematical aspects, we give numerical and physical details for the last two decades, where global and reliable data are available. The concept of a “mean sea level” is in itself rather artificial, because sea level varies at various temporal and spatial scales.
Luciana Fenoglio-Marc, Erwin Groten
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Mean Sea Level studies in the Aegean Sea
Physics and Chemistry of the Earth, Part A: Solid Earth and Geodesy, 2000A study of Mean Sea Level (MSL) determination in the Aegean Sea is carried out. First, MSL values have been computed at a number of tide gauge stations. Then, Sea Surface Heights (SSHs) have been determined based on GEOSAT altimeter data of Geodetic Mission (GM). The computed SSHs were fitted to the tide gauge MSL values using a 4-parameters model. The
V.D Andritsanos +3 more
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Marine Geodesy, 1997
This article focuses mainly on variations in mean sea level along the coast of Bangladesh. Six tidal stations along the coast of Bangladesh were selected for this study. The monthly, annual, and 5‐year variations of mean sea level for the period 1977–1990 are presented. The monthly mean at all six stations with respect to the 14 years average are taken
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This article focuses mainly on variations in mean sea level along the coast of Bangladesh. Six tidal stations along the coast of Bangladesh were selected for this study. The monthly, annual, and 5‐year variations of mean sea level for the period 1977–1990 are presented. The monthly mean at all six stations with respect to the 14 years average are taken
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Seasonal cycle of mean sea-level
Il Nuovo Cimento C, 1985The seasonal cycle of rainfall, evaporation and local effect of Atlantic water inflow explains the annual variation of mean sea-level and of surface salinity.
A. Palumbo, A. Mazzarella
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Updated Mean Sea-Level Analysis: Australia
Journal of Coastal Research, 2020Watson, P.J., 2020. Updated mean sea-level analysis: Australia. Journal of Coastal Research, 36(5), 915–931. Coconut Creek (Florida), ISSN 0749-0208.As an island nation with 60,000 km of open coastline and extensive margins of increasingly urbanised intertidal estuarine foreshores, Australia is critically exposed to the global threat posed by rising ...
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Mean sea level and its interpretation
Marine Geodesy, 1980Abstract The term “mean sea level”; is discussed, and a number of factors known to cause changes in mean sea level are reviewed. These factors include changes in water density ("steric”; sea level, or “dynamic height") and atmospheric pressure. In the open ocean, these factors, in addition to tides, are the main sources of variation recognized by ...
B. V. Hamon, J. S. Godfrey
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A seasonal mean sea-level indicator
Deep Sea Research (1953), 1960Abstract By means of oil capillaries the indicator attenuates the tidal rise and fall of the sea surface, as well as all fluctuations of higher frequencies. The time constant of the response is chosen so that the smaller, slower fluctuation of sea level is transmitted with very little change of amplitude and phase. There is no recorder.
Jean Filloux, Gordon Groves
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Marine Geodesy, 1987
Abstract Secular trends in mean sea level have been measured at a number of tide gauge stations around the U.K. coast. Four of the longest time series (from Aberdeen, North Shields, Sheerness and Newlyn) span the common epoch 1916–82, during which sea level has been rising at all four stations at rates of the order of 1–2 mm/year.
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Abstract Secular trends in mean sea level have been measured at a number of tide gauge stations around the U.K. coast. Four of the longest time series (from Aberdeen, North Shields, Sheerness and Newlyn) span the common epoch 1916–82, during which sea level has been rising at all four stations at rates of the order of 1–2 mm/year.
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Global Mean Sea Level Change: Correction
Science, 1997An error was recently discovered in the computer software that processes data from the National Aeronautics and Space Administration altimeter on the TOPEX/POSEIDON satellite ([1][1]). The error caused a small measurement drift of less than 1 centimeter per year.
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