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  • 1.
    Borenäs, Karin
    et al.
    SMHI, Core Services.
    Lake, Irene
    Lundberg, P A
    On the intermediate water masses of the Faroe-Bank Channel overflow2001In: Journal of Physical Oceanography, ISSN 0022-3670, E-ISSN 1520-0485, Vol. 31, no 7, p. 1904-1914Article in journal (Refereed)
    Abstract [en]

    A review of available hydrographic data from the Faroe-Bank Channel indicates that North Icelandic/Arctic Intermediate water masses are present in the passage to a larger extent than was previously believed. The presently compiled statistics, including results on the seasonality, are discussed in relation to previous investigations. Finally, a high quality subset of the hydrographic data is used for an analysis of the alongchannel mixing of the intermediate water masses.

  • 2. Enmar, Linda
    et al.
    Borenäs, Karin
    SMHI, Core Services.
    Lake, Irene
    SMHI, Core Services.
    Lundberg, Peter
    Comments on "Is the Faroe Bank Channel Overflow Hydraulically Controlled?''2009In: Journal of Physical Oceanography, ISSN 0022-3670, E-ISSN 1520-0485, Vol. 39, no 6, p. 1534-1538Article in journal (Other academic)
    Abstract [en]

    In a recent paper Girton et al., due to what appears to be a misunderstanding, stated that a critical-flow analysis of the deep-water transport through the Faroe Bank Channel had been undertaken by Lake et al. on the basis of rotating hydraulic theory for a channel of parabolic cross section. In fact, this quoted investigation dealt with a rectangular passage. In the present comment it is demonstrated how the use of parabolic bathymetry leads to significant improvements of the Froude number results.

  • 3. Enmar, Linda
    et al.
    Lake, Irene
    SMHI, Research Department, Oceanography.
    Lundberg, Peter
    Sigray, Peter
    A note on ADCP-based indirect observations of turbulence2016In: Boreal environment research, ISSN 1239-6095, E-ISSN 1797-2469, Vol. 21, no 1-2, p. 44-52Article in journal (Refereed)
    Abstract [en]

    A 70-day data set from bottom-mounted ADCPs on the two sides of the Faroe-Bank Channel was analysed using the recorded flow variance and echo intensity in the deeper reaches of the passage as proxies for turbulence. A consistent picture emerged, not least since the data losses (which were ascribed to turbulence-induced activation of the fish-elimination option in the ADCP software) could be shown to co-vary with the internal M-2 tide affecting the vertical shear, which in turn proved to be correlated with the flow variance.

  • 4. Enmar, Linda
    et al.
    Lake, Irene
    SMHI, Research Department.
    Lundberg, Peter
    Sigray, Peter
    A note on ADCP-based indirect observations of turbulence2016In: Boreal environment research, ISSN 1239-6095, E-ISSN 1797-2469, Vol. 21, no 1-2, p. 44-52Article in journal (Refereed)
  • 5.
    Hordoir, Robinson
    et al.
    SMHI, Research Department, Oceanography.
    Axell, Lars
    SMHI, Research Department, Oceanography.
    Höglund, Anders
    SMHI, Research Department, Oceanography.
    Dieterich, Christian
    SMHI, Research Department, Oceanography.
    Fransner, Filippa
    Groger, Matthias
    SMHI, Research Department, Oceanography.
    Liu, Ye
    SMHI, Research Department, Oceanography.
    Pemberton, Per
    SMHI, Research Department, Oceanography.
    Schimanke, Semjon
    SMHI, Research Department, Oceanography.
    Andersson, Helén
    SMHI, Research Department, Oceanography.
    Ljungemyr, Patrik
    SMHI, Core Services.
    Nygren, Petter
    SMHI, Core Services.
    Falahat, Saeed
    SMHI, Core Services.
    Nord, Adam
    SMHI, Core Services.
    Jönsson, Anette
    SMHI, Core Services.
    Lake, Irene
    SMHI, Core Services. SMHI, Research Department, Climate research - Rossby Centre.
    Doos, Kristofer
    Hieronymus, Magnus
    SMHI, Research Department, Oceanography.
    Dietze, Heiner
    Loeptien, Ulrike
    Kuznetsov, Ivan
    Westerlund, Antti
    Tuomi, Laura
    Haapala, Jari
    Nemo-Nordic 1.0: a NEMO-based ocean model for the Baltic and North seas - research and operational applications2019In: Geoscientific Model Development, ISSN 1991-959X, E-ISSN 1991-9603, Vol. 12, no 1, p. 363-386Article in journal (Refereed)
  • 6.
    Lake, Irene
    et al.
    SMHI, Core Services.
    Borenäs, Karin
    SMHI, Core Services.
    Lundberg, P
    Potential-vorticity characteristics of the Faroe Bank Channel deep-water overflow2005In: Journal of Physical Oceanography, ISSN 0022-3670, E-ISSN 1520-0485, Vol. 35, no 6, p. 921-932Article in journal (Refereed)
    Abstract [en]

    Results from a 71-day deployment of three ADCP current meters on a section across the sill region of the Faroe Bank Channel are reported. The characteristic density structure of the channel, with warm, highly saline North Atlantic Ocean surface water overlying colder, less-saline deep water originating from the Nordic seas, lends itself well to a two-layer description of flow processes in this region. The dataset has been analyzed to describe the spatial and temporal characteristics of the deep-water potential vorticity. The most striking feature is a persistent cross-channel variation of this quantity, with higher values on the Faroe Bank side. In the 11/2-layer hydraulic calculations that were undertaken the potential vorticity was approximated as a linear distribution. The ADCP observations indicated that the deep-water flow was hydraulically controlled, and, using the direct observed transport, the analysis yielded diagnostic results for the upstream reservoir interface level that were in good agreement with observations. It was also concluded that the deviation of the potential vorticity from a constant value had no significant effects on the deep-water transport.

  • 7.
    Lake, Irene
    et al.
    SMHI, Research Department, Climate research - Rossby Centre.
    Gutowski, William
    Giorgi, Filipo
    Lee, Boram
    CORDEX Climate Research and Information for Regions2017In: Bulletin of The American Meteorological Society - (BAMS), ISSN 0003-0007, E-ISSN 1520-0477, Vol. 98, no 8, p. ES189-ES192Article in journal (Refereed)
  • 8.
    Lake, Irene
    et al.
    SMHI, Core Services.
    Lundberg, Peter
    Seasonal barotropic modulation of the deep-water overflow through the Faroe Bank Channel2006In: Journal of Physical Oceanography, ISSN 0022-3670, E-ISSN 1520-0485, Vol. 36, no 12, p. 2328-2339Article in journal (Refereed)
    Abstract [en]

    As a joint Nordic project, an upward-looking ADCP has been maintained at the sill of the Faroe Bank Channel from 1995 onward. Records from a period in 1998 with three current meters deployed across the channel were used to demonstrate that the Faroe Bank Channel deep-water transport from the Norwegian Sea into the North Atlantic Ocean proper can be reasonably well estimated from one centrally located ADCP. The long-term average of this transport over the period 1995-2001 was found to be 2.1 Sv ( Sv 10(6) m(-3) s(-1)). The transport record demonstrates a pronounced seasonality. Satellite altimetry shows that this is caused by the northbound Atlantic surface water inflow giving rise to a barotropic modulation of the deep-water flow through the Faroe-Shetland Channel and the southern reaches of the Norwegian Sea.

1 - 8 of 8
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