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  • 1
    Online Resource
    Online Resource
    American Association for the Advancement of Science (AAAS) ; 1994
    In:  Science Vol. 263, No. 5144 ( 1994-01-14), p. 218-221
    In: Science, American Association for the Advancement of Science (AAAS), Vol. 263, No. 5144 ( 1994-01-14), p. 218-221
    Type of Medium: Online Resource
    ISSN: 0036-8075 , 1095-9203
    RVK:
    RVK:
    Language: English
    Publisher: American Association for the Advancement of Science (AAAS)
    Publication Date: 1994
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    SSG: 11
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  • 2
    Online Resource
    Online Resource
    American Geophysical Union (AGU) ; 2008
    In:  Geophysical Research Letters Vol. 35, No. 24 ( 2008-12-18)
    In: Geophysical Research Letters, American Geophysical Union (AGU), Vol. 35, No. 24 ( 2008-12-18)
    Type of Medium: Online Resource
    ISSN: 0094-8276
    Language: English
    Publisher: American Geophysical Union (AGU)
    Publication Date: 2008
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    detail.hit.zdb_id: 7403-2
    SSG: 16,13
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  • 3
    Online Resource
    Online Resource
    American Geophysical Union (AGU) ; 1998
    In:  Geophysical Research Letters Vol. 25, No. 10 ( 1998-05-15), p. 1729-1732
    In: Geophysical Research Letters, American Geophysical Union (AGU), Vol. 25, No. 10 ( 1998-05-15), p. 1729-1732
    Type of Medium: Online Resource
    ISSN: 0094-8276
    Language: English
    Publisher: American Geophysical Union (AGU)
    Publication Date: 1998
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    detail.hit.zdb_id: 7403-2
    SSG: 16,13
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  • 4
    In: Bulletin of the American Meteorological Society, American Meteorological Society, Vol. 83, No. 2 ( 2002-02), p. 255-275
    Type of Medium: Online Resource
    ISSN: 0003-0007 , 1520-0477
    Language: English
    Publisher: American Meteorological Society
    Publication Date: 2002
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  • 5
    Online Resource
    Online Resource
    American Geophysical Union (AGU) ; 1995
    In:  Journal of Geophysical Research: Oceans Vol. 100, No. C12 ( 1995-12-15), p. 24691-24703
    In: Journal of Geophysical Research: Oceans, American Geophysical Union (AGU), Vol. 100, No. C12 ( 1995-12-15), p. 24691-24703
    Abstract: Data from the 1975 Arctic Ice Dynamics Joint Experiment (AIDJEX) are used to examine energy exchange between the Arctic mixed layer and the ice pack. Conductivity‐temperature‐depth profiles from four drifting stations reveal significant heat storage in the upper 50 m of the water column during summer, with mixed layer temperature elevation above freezing δ T reaching as high as 0.4°C. Combining δ T with turbulent friction velocity obtained from local ice motion provides an estimate of heat flux from the ocean to the ice F w which was found to be strongly seasonal, with maximum values reaching 40–60 W m −2 in August. The annual average value of F w was 5.1 W m −2 , about half again as large as oceanic heat flux inferred from bottom ablation measurements in undeformed ice at the central station. Solar heat input to the upper ocean through open leads and thin ice, estimated using an ice thickness distribution model, totaled about 150 MJ m −2 , in general agreement with integrated values of F w . Results indicate that oceanic heat flux to the ice in the central Arctic is derived mainly from shortwave radiation entering the ocean through the ice pack, rather than from diffusion of warm water from below. Indeed, during the AIDJEX project the mixed layer appears to have contributed 15–20 MJ m −2 of heat to the upper pycnocline. During the summer, F w was found to vary by as much as 10–30 W m −2 over separations of 100 to 200 km and thus represents an important term in the surface heat budget not controlled by purely local deformation and thermodynamics.
    Type of Medium: Online Resource
    ISSN: 0148-0227
    Language: English
    Publisher: American Geophysical Union (AGU)
    Publication Date: 1995
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    detail.hit.zdb_id: 2403298-0
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    detail.hit.zdb_id: 161667-5
    detail.hit.zdb_id: 2969341-X
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    detail.hit.zdb_id: 3094268-8
    detail.hit.zdb_id: 710256-2
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    detail.hit.zdb_id: 3094181-7
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    SSG: 16,13
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  • 6
    Online Resource
    Online Resource
    American Meteorological Society ; 2004
    In:  Journal of Physical Oceanography Vol. 34, No. 10 ( 2004-10), p. 2180-2188
    In: Journal of Physical Oceanography, American Meteorological Society, Vol. 34, No. 10 ( 2004-10), p. 2180-2188
    Type of Medium: Online Resource
    ISSN: 0022-3670 , 1520-0485
    Language: English
    Publisher: American Meteorological Society
    Publication Date: 2004
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  • 7
    Online Resource
    Online Resource
    American Geophysical Union (AGU) ; 1996
    In:  Journal of Geophysical Research: Oceans Vol. 101, No. C3 ( 1996-03-15), p. 6409-6428
    In: Journal of Geophysical Research: Oceans, American Geophysical Union (AGU), Vol. 101, No. C3 ( 1996-03-15), p. 6409-6428
    Abstract: Measurements of turbulent stress, heat flux, salinity flux, and turbulent kinetic energy (TKE) dissipation were made in the oceanic boundary layer under freezing leads during the 1992 Lead Experiment project in the Arctic Ocean north of Alaska. Results from two instrument systems, one comprising a vertical array of four turbulence‐measuring instrument clusters, the other an automated, loose‐tethered microstructure profiler, show that forcing by modest surface fluxes (surface friction velocity u *0 ∼ 0.7 cm s −1 , surface buoyancy flux 〈 w ′ b ′〉 0 ∼ −0.7 × 10 −7 W kg −1 ) substantially changes the scales and character of boundary layer turbulence relative to forcing by stress alone. Despite continuous freezing at the surface, a diurnal cycle of heating and cooling of the mixed layer was seen, with downward oceanic heat flux as high as 70 W m −2 observed at middepth in the mixed layer near solar noon. Heat flux was determined both by direct eddy covariance of temperature and vertical velocity at fixed levels and from TKE and thermal dissipation estimates from the profiling instrument, with reasonable agreement. Similarly, there was close correspondence between TKE dissipation estimates obtained from inertial subrange spectral levels at the fixed instruments and from microstructure shear profiles. TKE production was dominated by buoyancy flux through most of the boundary layer. Thermal and saline eddy diffusivities were computed from directly measured fluxes and mixed layer temperature and salinity gradients, with mean values of 0.046 and 0.049 m 2 s −1 for temperature and salinity, respectively. Kolmogorov constants for relating thermal and saline dissipations to inertial subrange spectral levels were found to be 0.9 and 1.0, respectively, but with large scatter.
    Type of Medium: Online Resource
    ISSN: 0148-0227
    Language: English
    Publisher: American Geophysical Union (AGU)
    Publication Date: 1996
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    detail.hit.zdb_id: 3094104-0
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    detail.hit.zdb_id: 2016800-7
    detail.hit.zdb_id: 161666-3
    detail.hit.zdb_id: 161667-5
    detail.hit.zdb_id: 2969341-X
    detail.hit.zdb_id: 161665-1
    detail.hit.zdb_id: 3094268-8
    detail.hit.zdb_id: 710256-2
    detail.hit.zdb_id: 2016804-4
    detail.hit.zdb_id: 3094181-7
    detail.hit.zdb_id: 3094219-6
    detail.hit.zdb_id: 3094167-2
    detail.hit.zdb_id: 2220777-6
    detail.hit.zdb_id: 3094197-0
    SSG: 16,13
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  • 8
    Online Resource
    Online Resource
    American Geophysical Union (AGU) ; 1987
    In:  Journal of Geophysical Research: Oceans Vol. 92, No. C7 ( 1987-06-30), p. 6977-6986
    In: Journal of Geophysical Research: Oceans, American Geophysical Union (AGU), Vol. 92, No. C7 ( 1987-06-30), p. 6977-6986
    Abstract: A first‐order model for vertical flux of momentum and scalars in a rotational boundary layer is applied to the oceanic boundary layer beneath sea ice. Model eddy viscosity is proportional to the product of the local friction velocity u * and a master length scale for vertical exchange, which is a function of the rotational length scale u * /ƒ and the local Obukhov length L . The ratio of eddy diffusivity to eddy viscosity is 1 when turbulence is energetic but falls to lower values when turbulence levels are low and stratification high, according to an empirical relation. There are three empirical constants in the theory: ξ N , the ratio of the master length scale to the rotational length scale; R c , the critical flux Richardson number; and a shape factor describing the falloff of the eddy diffusivity ratio at high gradient Richardson numbers. For an idealized simulation of melting and freezing conditions representative of the marginal ice zone, the model agrees closely with a similar implementation of the Mellor‐Yamada level 2.5 model. The model is demonstrated by performing a simulation of surface drift and mixed‐layer properties observed during the 1984 Marginal Ice Zone Experiment field study in the Greenland Sea.
    Type of Medium: Online Resource
    ISSN: 0148-0227
    Language: English
    Publisher: American Geophysical Union (AGU)
    Publication Date: 1987
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    detail.hit.zdb_id: 161667-5
    detail.hit.zdb_id: 2969341-X
    detail.hit.zdb_id: 161665-1
    detail.hit.zdb_id: 3094268-8
    detail.hit.zdb_id: 710256-2
    detail.hit.zdb_id: 2016804-4
    detail.hit.zdb_id: 3094181-7
    detail.hit.zdb_id: 3094219-6
    detail.hit.zdb_id: 3094167-2
    detail.hit.zdb_id: 2220777-6
    detail.hit.zdb_id: 3094197-0
    SSG: 16,13
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  • 9
    Online Resource
    Online Resource
    American Meteorological Society ; 1980
    In:  Journal of Physical Oceanography Vol. 10, No. 6 ( 1980-06), p. 870-884
    In: Journal of Physical Oceanography, American Meteorological Society, Vol. 10, No. 6 ( 1980-06), p. 870-884
    Type of Medium: Online Resource
    ISSN: 0022-3670 , 1520-0485
    Language: English
    Publisher: American Meteorological Society
    Publication Date: 1980
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    detail.hit.zdb_id: 184162-2
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  • 10
    Online Resource
    Online Resource
    American Meteorological Society ; 1979
    In:  Journal of Physical Oceanography Vol. 9, No. 2 ( 1979-03), p. 388-400
    In: Journal of Physical Oceanography, American Meteorological Society, Vol. 9, No. 2 ( 1979-03), p. 388-400
    Type of Medium: Online Resource
    ISSN: 0022-3670 , 1520-0485
    Language: English
    Publisher: American Meteorological Society
    Publication Date: 1979
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    detail.hit.zdb_id: 184162-2
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