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Relevant bibliographies by topics / Rapid-MOCHA array

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Journal articles

Academic literature on the topic 'Rapid-MOCHA array'

Author: Grafiati

Published: 2 June 2025

Last updated: 31 July 2025

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Journal articles on the topic "Rapid-MOCHA array"

1

Baehr, Johanna. "Influence of the 26°N RAPID–MOCHA Array and Florida Current Cable Observations on the ECCO–GODAE State Estimate." Journal of Physical Oceanography 40, no. 5 (2010): 865–79. http://dx.doi.org/10.1175/2009jpo4118.1.

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Abstract The incorporation of local temperature and salinity observations from the Rapid Climate Change–Meridional Overturning Circulation and Heatflux Array (RAPID–MOCHA), as well as the cable estimates of volume transport in the Florida Current (FC), is tested in the Estimating the Circulation and Climate of the Ocean–Global Ocean Data Assimilation Experiment (ECCO–GODAE) estimation system for their impact on the estimate of the meridional overturning circulation (MOC) and the meridional heat transport in the Atlantic. An experimental setup covering the first deployment period of RAPID–MOCHA

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2

Balan Sarojini, B., J. M. Gregory, R. Tailleux, et al. "High frequency variability of the Atlantic meridional overturning circulation." Ocean Science 7, no. 4 (2011): 471–86. http://dx.doi.org/10.5194/os-7-471-2011.

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Abstract. We compare the variability of the Atlantic meridional overturning circulation (AMOC) as simulated by the coupled climate models of the RAPID project, which cover a wide range of resolution and complexity, and observed by the RAPID/MOCHA array at about 26° N. We analyse variability on a range of timescales, from five-daily to interannual. In models of all resolutions there is substantial variability on timescales of a few days; in most AOGCMs the amplitude of the variability is of somewhat larger magnitude than that observed by the RAPID array, while the time-mean is within about 10 %

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3

Baehr, J., S. Cunnningham, H. Haak, P. Heimbach, T. Kanzow, and J. Marotzke. "Observed and simulated estimates of the meridional overturning circulation at 26.5° N in the Atlantic." Ocean Science 5, no. 4 (2009): 575–89. http://dx.doi.org/10.5194/os-5-575-2009.

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Abstract. Daily timeseries of the meridional overturning circulation (MOC) estimated from the UK/US RAPID/MOCHA array at 26.5° N in the Atlantic are used to evaluate the MOC as simulated in two global circulation models: (I) an 8-member ensemble of the coupled climate model ECHAM5/MPI-OM, and (II) the ECCO-GODAE state estimate. In ECHAM5/MPI-OM, we find that the observed and simulated MOC have a similar variability and time-mean within the 99% confidence interval. In ECCO-GODAE, we find that the observed and simulated MOC show a significant correlation within the 99% confidence interval. To in

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4

Elipot, Shane, Eleanor Frajka-Williams, Chris W. Hughes, Sofia Olhede, and Matthias Lankhorst. "Observed Basin-Scale Response of the North Atlantic Meridional Overturning Circulation to Wind Stress Forcing." Journal of Climate 30, no. 6 (2017): 2029–54. http://dx.doi.org/10.1175/jcli-d-16-0664.1.

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Abstract The response of the North Atlantic meridional overturning circulation (MOC) to wind stress forcing is investigated from an observational standpoint, using four time series of overturning transports below and relative to 1000 m, overlapping by 3.6 yr. These time series are derived from four mooring arrays located on the western boundary of the North Atlantic: the RAPID Western Atlantic Variability Experiment (WAVE) array (42.5°N), the Woods Hole Oceanographic Institution Line W array (39°N), RAPID–MOC/MOCHA (26.5°N), and the Meridional Overturning Variability Experiment (MOVE) array (1

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5

Baehr, J., S. Cunnningham, H. Haak, P. Heimbach, T. Kanzow, and J. Marotzke. "Observed and simulated estimates of the meridional overturning circulation at 26.5° N in the Atlantic." Ocean Science Discussions 6, no. 2 (2009): 1333–67. http://dx.doi.org/10.5194/osd-6-1333-2009.

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Abstract. Daily timeseries of the meridional overturning circulation (MOC) estimated from the UK/US RAPID/MOCHA array at 26.5° N in the Atlantic are used to evaluate the MOC as simulated in two global circulation models: (i) an 8-member ensemble of the coupled climate model ECHAM5/MPI-OM, and (ii) the ECCO-GODAE state estimate. In ECHAM5/MPI-OM, we find that the observed and simulated MOC have a similar variability and time-mean within the 99 percent confidence interval. In ECCO-GODAE, we find that the observed and simulated MOC show a significant correlation within the 99 percent confidence i

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6

Köhl, A. "Influence of assimilating transports and in situ data from the Rapid-MOCHA array into the GECCO2 ocean synthesis." Dynamics of Atmospheres and Oceans 72 (October 1, 2015): 38–51. https://doi.org/10.5281/zenodo.34697.

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By assimilating information required for the estimation of the Atlantic meridional overturning circulation (AMOC) by the Rapid-MOCHA array, we investigate how transports should be constrained. For the period 2004–2011, we find that even the large adjustments in Florida Strait transport (FST) imposed by assimilating FST data do not impact the AMOC strength at 26.5° N while the AMOC away from this section changes due to the baroclinic response. Moreover, the high correlation between the FST and AMOC previously reported cannot be confirmed for this longer period. When assimilating

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7

Köhl, Armin. "Influence of assimilating transports and in situ data from the Rapid-MOCHA array into the GECCO2 ocean synthesis." Dynamics of Atmospheres and Oceans 72 (December 2015): 38–51. http://dx.doi.org/10.1016/j.dynatmoce.2015.09.001.

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8

Worthington, Emma L., Ben I. Moat, David A. Smeed, Jennifer V. Mecking, Robert Marsh, and Gerard D. McCarthy. "A 30-year reconstruction of the Atlantic meridional overturning circulation shows no decline." Ocean Science 17, no. 1 (2021): 285–99. http://dx.doi.org/10.5194/os-17-285-2021.

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Abstract. A decline in Atlantic meridional overturning circulation (AMOC) strength has been observed between 2004 and 2012 by the RAPID-MOCHA-WBTS (RAPID – Meridional Overturning Circulation and Heatflux Array – Western Boundary Time Series, hereafter RAPID array) with this weakened state of the AMOC persisting until 2017. Climate model and paleo-oceanographic research suggests that the AMOC may have been declining for decades or even centuries before this; however direct observations are sparse prior to 2004, giving only “snapshots” of the overturning circulation. Previous studies have used l

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9

Jamet, Quentin, William K. Dewar, Nicolas Wienders, Bruno Deremble, Sally Close, and Thierry Penduff. "Locally and Remotely Forced Subtropical AMOC Variability: A Matter of Time Scales." Journal of Climate 33, no. 12 (2020): 5155–72. http://dx.doi.org/10.1175/jcli-d-19-0844.1.

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AbstractMechanisms driving the North Atlantic meridional overturning circulation (AMOC) variability at low frequency are of central interest for accurate climate predictions. Although the subpolar gyre region has been identified as a preferred place for generating climate time-scale signals, their southward propagation remains under consideration, complicating the interpretation of the observed time series provided by the Rapid Climate Change–Meridional Overturning Circulation and Heatflux Array–Western Boundary Time Series (RAPID–MOCHA–WBTS) program. In this study, we aim at disentangling the

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10

Balan Sarojini, B., J. M. Gregory, R. Tailleux, et al. "High frequency variability of the Atlantic meridional overturning circulation." Ocean Science Discussions 8, no. 1 (2011): 219–46. http://dx.doi.org/10.5194/osd-8-219-2011.

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Abstract. We compare the variability of the Atlantic meridional overturning circulation (AMOC) as simulated by the coupled climate models of the RAPID project, which cover a wide range of resolution and complexity, and observed by the RAPID/MOCHA array at about 26° N. We analyse variability on a range of timescales. In models of all resolutions there is substantial variability on timescales of a few days; in most AOGCMs the amplitude of the variability is of somewhat larger magnitude than that observed by the RAPID array, while the amplitude of the simulated annual cycle is similar to observat

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