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Rzepecka, Zofia and Birylo, Monika, 2024. Attempts to Determine the Velocity Variations in Ocean Geostrothrophic Currents Based on GRACE Solutions. Remote Sensing, 17(1):76, doi:10.3390/rs17010076.
• from the NASA Astrophysics Data System • by the DOI System •
@ARTICLE{2024RemS...17...76R,
author = {{Rzepecka}, Zofia and {Birylo}, Monika},
title = "{Attempts to Determine the Velocity Variations in Ocean Geostrothrophic Currents Based on GRACE Solutions}",
journal = {Remote Sensing},
keywords = {GRACE L2 solution, ocean bottom pressure, Navier{\textendash}Stokes equation, geostrophic currents, AMOC},
year = 2024,
month = dec,
volume = {17},
number = {1},
eid = {76},
pages = {76},
abstract = "{The paper shows the idea of using GRACE solutions to determine the
velocity of the Atlantic geostrophic currents at a depth of 2000
m, where the assumptions of geostrophic motion are met. The
relationship between the water velocity variations and the OBP,
determined based on the L2 GRACE solutions, is shown. The
velocities obtained were compared with the results of a direct
ocean current measurement program, the RAPID AMOC, carried out
in the Atlantic area. The upper North Atlantic Deep Water layer
transport was used for comparisons performed. An analysis of the
obtained results, their summary, and discussion are shown. The
research covers the period from November 2004 to March 2022. As
a result of flow calculations through the parallel, a
satisfactory agreement was obtained between the GRACE and RAPID
AMOC fitted functions. The correlation between the GRACE and
RAPID AMOC time series observations exceeded the significance
level.}",
doi = {10.3390/rs17010076},
adsurl = {https://ui.adsabs.harvard.edu/abs/2024RemS...17...76R},
adsnote = {Provided by the SAO/NASA Astrophysics Data System}
}
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