Variability of Internal Wave Strain Over the Western Boundary Region in the North Atlantic
Based on the CTD profiles and mooring measurements of the Line W program in the North Atlantic about 35°N/70°W, we investigated the spatial variability of internal wave-induced strain variance along the Line W section and the associated reasons. The results showed that the internal wave strain varia...
Main Authors: | Liming Fan, Xin Wang |
---|---|
Format: | Article |
Language: | English |
Published: |
Frontiers Media S.A.
2022-04-01
|
Series: | Frontiers in Earth Science |
Subjects: | |
Online Access: | https://www.frontiersin.org/articles/10.3389/feart.2022.855644/full |
Similar Items
-
How does the SST variability over the western North Atlantic Ocean control Arctic warming over the Barents–Kara Seas?
by: Ok Jung, et al.
Published: (2017-01-01) -
Drivers of North Atlantic Oscillation Events
by: Iris Manola, et al.
Published: (2013-06-01) -
Observations of interaction between the internal wavefield and low frequency flows in the North Atlantic.
by: Ruddick, Barry Raymond
Published: (2010) -
Summer Russian heat waves and their links to Greenland’s ice melt and sea surface temperature anomalies over the North Atlantic and the Barents–Kara Seas
by: Hejing Wang, et al.
Published: (2020-01-01) -
Connecting North Atlantic SST Variability to European Heat Events over the Past Decades
by: Julian Krüger, et al.
Published: (2023-11-01)