Irminger Sea deep convection injects oxygen and anthropogenic carbon to the ocean interior
Deep convection in the Irminger Sea has been shown to be highly variable on annual timescales. Here, the authors provide a direct link between atmospheric forcing and anthropogenic carbon storage and oxygen ventilation based on a unique cruise dataset acquired during active deep water formation.
Saved in:
Main Authors: | F. Fröb, A. Olsen, K. Våge, G. W. K. Moore, I. Yashayaev, E. Jeansson, B. Rajasakaren |
---|---|
Format: | article |
Language: | EN |
Published: |
Nature Portfolio
2016
|
Subjects: | |
Online Access: | https://doaj.org/article/6d88c940e6d64668ad0b973af490a91d |
Tags: |
Add Tag
No Tags, Be the first to tag this record!
|
Similar Items
-
Ocean convection linked to the recent ice edge retreat along east Greenland
by: Kjetil Våge, et al.
Published: (2018) -
High reactivity of deep biota under anthropogenic CO2 injection into basalt
by: Rosalia Trias, et al.
Published: (2017) -
An updated version of the global interior ocean biogeochemical data product, GLODAPv2.2021
by: S. K. Lauvset, et al.
Published: (2021) -
Bacteriophage Distributions and Temporal Variability in the Ocean’s Interior
by: Elaine Luo, et al.
Published: (2017) -
Influence of environmental and anthropogenic acoustic cues in sea-finding of hatchling leatherback (Dermochelys coriacea) sea turtles.
by: Bethany Holtz, et al.
Published: (2021)