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    A Station-Based Southern Annular Mode Index from 1884 to 2005 

    Source: Journal of Climate:;2009:;volume( 022 ):;issue: 004:;page 940
    Author(s): Visbeck, Martin
    Publisher: American Meteorological Society
    Abstract: Atmospheric pressure observations from the Southern Hemisphere are used to estimate monthly and annually averaged indexes of the southern annular mode (SAM) back to 1884. This analysis groups all relevant observations in ...
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    Deep Velocity Profiling Using Lowered Acoustic Doppler Current Profilers: Bottom Track and Inverse Solutions 

    Source: Journal of Atmospheric and Oceanic Technology:;2002:;volume( 019 ):;issue: 005:;page 794
    Author(s): Visbeck, Martin
    Publisher: American Meteorological Society
    Abstract: Lowered acoustic Doppler current profilers (LADCPs) have matured from an experimental instrument to an operational hydrographic tool to study ocean dynamics. The data processing, however, is still in a rather primitive ...
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    Analysis of Seasonal Current Variations in the Western Equatorial Indian Ocean: Direct Measurements and GFDL Model Comparison 

    Source: Journal of Physical Oceanography:;1992:;Volume( 022 ):;issue: 010:;page 1112
    Author(s): Visbeck, Martin; Schott, Friedrich
    Publisher: American Meteorological Society
    Abstract: The seasonal cycles found in moored current measurements in the equatorial Somali Current region and along the equator between 50° and 60°E are compared with the multilayer Geophysical Fluid Dynamics Laboratory model for ...
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    Reply 

    Source: Journal of Climate:;2004:;volume( 017 ):;issue: 011:;page 2255
    Author(s): Visbeck, Martin; Hall, Alex
    Publisher: American Meteorological Society
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    Synchronous Variability in the Southern Hemisphere Atmosphere, Sea Ice, and Ocean Resulting from the Annular Mode 

    Source: Journal of Climate:;2002:;volume( 015 ):;issue: 021:;page 3043
    Author(s): Hall, Alex; Visbeck, Martin
    Publisher: American Meteorological Society
    Abstract: Zonally symmetric fluctuations of the midlatitude westerly winds characterize the primary mode of atmospheric variability in the Southern Hemisphere during all seasons. This is true not only in observations but also in an ...
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    Is Bottom Boundary Layer Mixing Slowly Ventilating Greenland Sea Deep Water 

    Source: Journal of Physical Oceanography:;2000:;Volume( 030 ):;issue: 001:;page 215
    Author(s): Visbeck, Martin; Rhein, Monika
    Publisher: American Meteorological Society
    Abstract: Bottom water temperatures in the central Greenland Sea have been increasing for the last two decades. The warming is most likely related to the absence of deep convective mixing, which cools and freshens the deep water. ...
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    A Model of the Zonally Averaged Stratification and Overturning in the Southern Ocean 

    Source: Journal of Physical Oceanography:;2005:;Volume( 035 ):;issue: 007:;page 1190
    Author(s): Olbers, Dirk; Visbeck, Martin
    Publisher: American Meteorological Society
    Abstract: The ocean area south of the Antarctic Circumpolar Current (ACC) frontal system is a region of major watermass modification. Influx of North Atlantic Deep Water (NADW), small-scale mixing, eddy transport and diffusion, as ...
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    Sea Surface Conditions Remotely Sensed by Upward-Looking ADCPs 

    Source: Journal of Atmospheric and Oceanic Technology:;1994:;volume( 012 ):;issue: 001:;page 141
    Author(s): Visbeck, Martin; Fischer, Jorgen
    Publisher: American Meteorological Society
    Abstract: Surface data obtained from 153-kHz acoustic Doppler current profilers deployed in the Greenland Sea at about 350-m depth during the winter of 1988/89 were investigated under several aspects. First a method is described to ...
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    On the Linkage between Antarctic Surface Water Stratification and Global Deep-Water Temperature 

    Source: Journal of Climate:;2011:;volume( 024 ):;issue: 014:;page 3545
    Author(s): Keeling, Ralph F.; Visbeck, Martin
    Publisher: American Meteorological Society
    Abstract: he suggestion is advanced that the remarkably low static stability of Antarctic surface waters may arise from a feedback loop involving global deep-water temperatures. If deep-water temperatures are too warm, this promotes ...
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    Dynamics of Isolated Convective Regions in the Ocean 

    Source: Journal of Physical Oceanography:;1996:;Volume( 026 ):;issue: 009:;page 1721
    Author(s): Visbeck, Martin; Marshall, John; Jones, Helen
    Publisher: American Meteorological Society
    Abstract: An initially resting ocean of stratification N is considered, subject to buoyancy loss at its surface of magnitude B0 over a circular region of radius r, at a latitude where the Coriolis parameter is f. Initially the ...
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    DSpace software copyright © 2002-2015  DuraSpace
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