Attempts to Determine the Velocity Variations in Ocean Geostrothrophic Currents Based on GRACE Solutions
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,...
Saved in:
| Main Authors: | Zofia Rzepecka, Monika Birylo |
|---|---|
| Format: | Article |
| Language: | English |
| Published: |
MDPI AG
2024-12-01
|
| Series: | Remote Sensing |
| Subjects: | |
| Online Access: | https://www.mdpi.com/2072-4292/17/1/76 |
| Tags: |
Add Tag
No Tags, Be the first to tag this record!
|
Similar Items
-
Proxy representation of Arctic ocean bottom pressure variability: Bridging gaps in GRACE observations
by: Cecilia Peralta‐Ferriz, et al.
Published: (2016-09-01) -
The Navier-Stokes problem. Solution of a millennium problem related to the Navier-Stokes equations
by: Alexander Ramm
Published: (2024-01-01) -
On the solution of weak nonlinear variational problem connected with navier - stokes stationary homogeneous problem
by: A. A. Fonarev
Published: (2016-11-01) -
When Simplification Leads to Ambiguity: A Look at Two Ocean Metrics for the Subpolar North Atlantic
by: Léon Chafik, et al.
Published: (2025-02-01) -
ON BEHAVIOR OF TRAJECTORIES OF WEAK SOLUTIONS OF N-DIMENSIONAL STOCHASTIC NAVIER-STOKES EQUATIONS
by: D. A. Khrychev
Published: (2017-06-01)