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Cited by 329

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Is a Decline of AMOC Causing the Warming Hole above the North Atlantic in Observed and Modeled Warming Patterns?

Open access
Drijfhout, Sybren, van Oldenborgh, Geert Jan, Cimatoribus, Andrea·2012·Journal of Climate

Abstract

The pattern of global mean temperature (GMT) change is calculated by regressing local surface air temperature (SAT) to GMT for an ensemble of CMIP5 models and for observations over the last 132 years. Calculations are based on the historical period and climate change scenarios. As in the observations the warming pattern contains a warming hole over the subpolar North Atlantic. Using a bivariate regression of SAT to GMT and an index of the Atlantic meridional overturning circulation (AMOC), the warming pattern is decomposed in a radiatively forced part and an AMOC fingerprint. The North Atlantic warming hole is associated with a decline of the AMOC. The AMOC fingerprint resembles Atlantic multidecadal variability (AMV), but details of the pattern change when the AMOC decline increases, underscoring the nonlinearity in the response. The warming hole is situated south of deep convection sites, indicating that it involves an adjustment of the gyre circulation, although it should be noted that some models feature deep convection in the middle of the subpolar gyre. The warming hole is already prominent in historical runs, where the response of the AMOC to GMT is weak, which suggests that it is involved in an ocean adjustment that precedes the AMOC decline. In the more strongly forced scenario runs, the warming hole over the subpolar gyre becomes weaker, while cooling over the Nordic seas increases, consistent with previous findings that deep convection in the Labrador and Irminger Seas is more vulnerable to changes in external forcing than convection in the Nordic seas, which only reacts after a threshold is passed.

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Metadata

Authors
Drijfhout, S., van Oldenborgh, G. J., & Cimatoribus, A.
Venue
Journal of Climate
Published
2012-12-15
Volume
25
Issue
24
Pages
8373-8379
ISSN
  • 0894-8755 (ISSN-L)
  • 1520-0442
OpenAlex
W2070541435
Cited by
329
References
18
FWCI
8.08
Type
journal article
Language
en
Open access
bronze

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CoChat. (2026). Citation check: Is a Decline of AMOC Causing the Warming Hole above the North Atlantic in Observed and Modeled Warming Patterns? https://app.cochat.ai/papers/10.1175/jcli-d-12-00490.1
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Drijfhout, S., van Oldenborgh, G. J., & Cimatoribus, A. (2012). Is a Decline of AMOC Causing the Warming Hole above the North Atlantic in Observed and Modeled Warming Patterns? Journal of Climate. https://doi.org/10.1175/jcli-d-12-00490.1

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