Open AccessSurface Pressure and Wind Stress Effects on Sea Level Change Estimations from TOPEX/Poseidon Satellite Altimetry in the Mediterranean Sea
Author(s) -
Sylvain Mangiarotti,
Florent Lyard
Publication year - 2008
Publication title -
journal of atmospheric and oceanic technology
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.774
H-Index - 124
eISSN - 1520-0426
pISSN - 0739-0572
DOI - 10.1175/2006jtecho419.1
Subject(s) - barotropic fluid , altimeter , sea level , climatology , sea surface height , geology , forcing (mathematics) , wind stress , geodesy , barometer , standard deviation , mediterranean sea , meteorology , mediterranean climate , physics , mathematics , oceanography , geography , statistics , archaeology
0739-0572International audienceUsing the classical inverse barometer (113) correction and the Modele d'Onde de Gravite A 2 Dimensions (MOG2D) barotropic model in the Mediterranean Sea during the 1993-2002 period, it is shown that surface pressure and wind stress forcing significantly contribute to sea level elevation variations observed with Ocean Topography Experiment (TOPEX)/Poseidon (T/P) satellite altimetry. The barotropic model allows the authors to estimate the high-frequency atmospheric ocean response that is aliased into the altimetric sea level. Applying the model barotropic correction allows them to reduce the T/P standard deviation by a mean of 21% over the whole basin, whereas the classical IB correction reduces the standard deviation by only 16%. The trend in sea level rise is also strongly affected due to the aliasing effect, especially when short periods are considered. On a 3-yr period, the correction associated with either of these two models can reach 10-12 mm yr(-1). Applying the barotropic model correction rather than the IB correction can also affect the linear trend estimations by more than 6-7 mm yr(-1). For a 9-yr window, the IB/MOG2D correction can contribute 1.8-2 mm yr(-1) in magnitude. The local corrected linear trends confirm the previous analysis pattern but on a local scale, with the linear trend magnitudes reaching values between -24 and +29 mm yr(-1)