nerc.ac.uk

Intermittent Intense Turbulent Mixing under Ice in the Laptev Sea Continental Shelf

Lenn, Yueng-Djern; Rippeth, Tom P.; Old, Chris P.; Bacon, Sheldon ORCID: https://orcid.org/0000-0002-2471-9373; Polyakov, Igor; Ivanov, Vladimir; Hölemann, Jens. 2011 Intermittent Intense Turbulent Mixing under Ice in the Laptev Sea Continental Shelf. Journal of Physical Oceanography, 41 (3). 531-547. https://doi.org/10.1175/2010JPO4425.1

Full text not available from this repository. (Request a copy)

Abstract/Summary

Vertical mixing in the bottom boundary layer and pycnocline of the Laptev Sea is evaluated from a rapidly sampled 12-h time series of microstructure temperature, conductivity, and shear observations collected under 100% sea ice during October 2008. The bottom boundary turbulent kinetic energy dissipation was observed to be enhanced (ϵ 10−4 W m−3) beyond background levels (ϵ 10−6 W m−3), extending up to 10 m above the seabed when simulated tidal currents were directed on slope. Upward heat fluxes into the halocline-class waters along the Laptev Sea seabed peaked at 4–8 W m−2, averaging out to 2 W m−2 over the 12-h sampling period. In the Laptev Sea pycnocline, an isolated 2-h episode of intense dissipation (ϵ 10−3 W m−3) and vertical diffusivities was observed that was not due to a localized wind event. Observations from an acoustic Doppler current meter moored in the central Laptev Sea near the M2 critical latitude are consistent with a previous model in which mixing episodes are driven by an enhancement of the pycnocline shear resulting from the alignment of the rotating pycnocline shear vector with the under-ice stress vector. Upward cross-pycnocline heat fluxes from the Arctic halocline peaked at 54 W m−2, resulting in a 12-h average of 12 W m−2. These results highlight the intermittent nature of Arctic shelf sea mixing processes and how these processes can impact the transformation of Arctic Ocean water masses. The observations also clearly demonstrate that absence or presence of sea ice profoundly affects the availability of near-inertial kinetic energy to drive vertical mixing on the Arctic shelves.

Item Type: Publication - Article
Digital Object Identifier (DOI): https://doi.org/10.1175/2010JPO4425.1
ISSN: 00223670
Additional Keywords: Mixing, Sea ice, Continental shelf/slope
Date made live: 03 May 2011 13:42 +0 (UTC)
URI: https://nora.nerc.ac.uk/id/eprint/283783

Actions (login required)

View Item View Item

Document Downloads

Downloads for past 30 days

Downloads per month over past year

More statistics for this item...