Response of the Atlantic Ocean circulation to Greenland Ice Sheet melting in a strongly-eddying ocean model

W. Weijer; M.E. Maltrud; M.W. Hecht; H.A. Dijkstra; M. Kliphuis

doi:10.1029/2012GL051611

Response of the Atlantic Ocean circulation to Greenland Ice Sheet melting in a strongly-eddying ocean model

W. Weijer, M.E. Maltrud, M.W. Hecht, H.A. Dijkstra, M. Kliphuis

extern

Research output: Contribution to journal › Article › Academic › peer-review

Abstract

The sensitivity of the Atlantic Meridional Overturning Circulation (AMOC) to high-latitude freshwater input is one of the key uncertainties in the climate system. Considering the importance of the AMOC for global heat transports, and the vulnerability of the Greenland Ice Sheet (GrIS) to global warming, assessing this sensitivity is critical for climate change projections. Here we present a unique set of computational experiments to investigate the adjustment of the AMOC to enhanced melt water from the GrIS under present-day conditions. For the first time, the response in a global, strongly-eddying ocean model is systematically compared to that of an ocean model typical of IPCC-class climate models. We find that the overall decline of the AMOC on decadal time scales is quantitatively similar (

Original language	English
Article number	L09606
Pages (from-to)	L09606/1-L09606/6
Number of pages	6
Journal	Geophysical Research Letters
Volume	39
DOIs	https://doi.org/10.1029/2012GL051611
Publication status	Published - 2012

UN SDGs

This output contributes to the following UN Sustainable Development Goals (SDGs)

Access to Document

10.1029/2012GL051611

Embargoed Document

2012GL051611
Final published version, 1.55 MB
Embargo ends: 1/01/50
Request copy

Cite this

@article{b5fe7b6d57c6424693ebd260c62c6176,

title = "Response of the Atlantic Ocean circulation to Greenland Ice Sheet melting in a strongly-eddying ocean model",

abstract = "The sensitivity of the Atlantic Meridional Overturning Circulation (AMOC) to high-latitude freshwater input is one of the key uncertainties in the climate system. Considering the importance of the AMOC for global heat transports, and the vulnerability of the Greenland Ice Sheet (GrIS) to global warming, assessing this sensitivity is critical for climate change projections. Here we present a unique set of computational experiments to investigate the adjustment of the AMOC to enhanced melt water from the GrIS under present-day conditions. For the first time, the response in a global, strongly-eddying ocean model is systematically compared to that of an ocean model typical of IPCC-class climate models. We find that the overall decline of the AMOC on decadal time scales is quantitatively similar (",

author = "W. Weijer and M.E. Maltrud and M.W. Hecht and H.A. Dijkstra and M. Kliphuis",

year = "2012",

doi = "10.1029/2012GL051611",

language = "English",

volume = "39",

pages = "L09606/1--L09606/6",

journal = "Geophysical Research Letters",

issn = "0094-8276",

publisher = "John Wiley and Sons Inc.",

}

TY - JOUR

T1 - Response of the Atlantic Ocean circulation to Greenland Ice Sheet melting in a strongly-eddying ocean model

AU - Weijer, W.

AU - Maltrud, M.E.

AU - Hecht, M.W.

AU - Dijkstra, H.A.

AU - Kliphuis, M.

PY - 2012

Y1 - 2012

N2 - The sensitivity of the Atlantic Meridional Overturning Circulation (AMOC) to high-latitude freshwater input is one of the key uncertainties in the climate system. Considering the importance of the AMOC for global heat transports, and the vulnerability of the Greenland Ice Sheet (GrIS) to global warming, assessing this sensitivity is critical for climate change projections. Here we present a unique set of computational experiments to investigate the adjustment of the AMOC to enhanced melt water from the GrIS under present-day conditions. For the first time, the response in a global, strongly-eddying ocean model is systematically compared to that of an ocean model typical of IPCC-class climate models. We find that the overall decline of the AMOC on decadal time scales is quantitatively similar (

AB - The sensitivity of the Atlantic Meridional Overturning Circulation (AMOC) to high-latitude freshwater input is one of the key uncertainties in the climate system. Considering the importance of the AMOC for global heat transports, and the vulnerability of the Greenland Ice Sheet (GrIS) to global warming, assessing this sensitivity is critical for climate change projections. Here we present a unique set of computational experiments to investigate the adjustment of the AMOC to enhanced melt water from the GrIS under present-day conditions. For the first time, the response in a global, strongly-eddying ocean model is systematically compared to that of an ocean model typical of IPCC-class climate models. We find that the overall decline of the AMOC on decadal time scales is quantitatively similar (

U2 - 10.1029/2012GL051611

DO - 10.1029/2012GL051611

M3 - Article

SN - 0094-8276

VL - 39

SP - L09606/1-L09606/6

JO - Geophysical Research Letters

JF - Geophysical Research Letters

M1 - L09606

ER -

Response of the Atlantic Ocean circulation to Greenland Ice Sheet melting in a strongly-eddying ocean model

Abstract

UN SDGs

Access to Document

Embargoed Document

Fingerprint

Cite this