<?xml version="1.0" encoding="utf-8" standalone="no"?>
<!DOCTYPE article SYSTEM "http://www.ocean-sci.net/inc/os/copernicus.dtd">
<article language="en">
	<journal>
		<journal_title>Ocean Science</journal_title>
		<journal_url>www.ocean-sci.net</journal_url>
		<issn>1812-0784</issn>
		<eissn>1812-0792</eissn>
		<volume_number>5</volume_number>
		<issue_number>4</issue_number>
		<publication_year>2009</publication_year>
	</journal>
	<doi>10.5194/os-5-435-2009</doi>
	<article_url>http://www.ocean-sci.net/5/435/2009/</article_url>
	<abstract_html>http://www.ocean-sci.net/5/435/2009/os-5-435-2009.html</abstract_html>
	<fulltext_pdf>http://www.ocean-sci.net/5/435/2009/os-5-435-2009.pdf</fulltext_pdf>
	<start_page>435</start_page>
	<end_page>445</end_page>
	<publication_date>2009-10-26</publication_date>
	<article_title content_type="html">Observations of turbulence beneath sea ice in southern McMurdo Sound, Antarctica</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>C. L. Stevens</name>
			<email>c.stevens@niwa.cri.nz</email>
		</author>
		<author numeration="2" affiliations="1,2">
			<name>N. J. Robinson</name>
		</author>
		<author numeration="3" affiliations="1">
			<name>M. J. M. Williams</name>
		</author>
		<author numeration="4" affiliations="3">
			<name>T. G. Haskell</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">National Institute for Water and Atmospheric Research (NIWA), Greta Point Wellington, New Zealand</affiliation>
		<affiliation numeration="2" content_type="html">University of Otago, Dunedin, New Zealand</affiliation>
		<affiliation numeration="3" content_type="html">Industrial Research Ltd (IRL), Gracefield, Lower Hutt, New Zealand</affiliation>
	</affiliations>
	<abstract content_type="html">The first turbulence profiler observations beneath land fast sea ice which
is directly adjacent to an Antarctic ice shelf are described. The
stratification in the 325 m deep water column consisted of a layer of
supercooled water in the upper 40 m lying above a quasi-linearly stratified
water column with a sharp step in density at mid-depth. Turbulent energy
dissipation rates were on average 3&amp;times;10&lt;sup&gt;&amp;minus;8&lt;/sup&gt; m&lt;sup&gt;2&lt;/sup&gt; s&lt;sup&gt;&amp;minus;3&lt;/sup&gt; with peak
bin-averaged values reaching 4&amp;times;10&lt;sup&gt;&amp;minus;7&lt;/sup&gt; m&lt;sup&gt;2&lt;/sup&gt; s&lt;sup&gt;&amp;minus;3&lt;/sup&gt;. The local
dissipation rate per unit area was estimated to be 10 m Wm&lt;sup&gt;&amp;minus;2&lt;/sup&gt; on average
with a peak of 50 m Wm&lt;sup&gt;&amp;minus;2&lt;/sup&gt;. These values are consistent with a moderate
baroclinic response to the tides. The small-scale turbulent energetics lie
on the boundary between isotropy and buoyancy-affected. This will likely
influence the formation and aggregation of frazil ice crystals within the
supercooled layer. The data suggest that the large crystals observed in
McMurdo Sound will transition from initial growth at scales smaller than the
Kolmogorov lengthscale to sizes substantially (1–2 orders of magnitude)
greater than the Kolmogorov scale. An estimate of the experiment-averaged
vertical diffusivity of mass &lt;i&gt;K&lt;/i&gt;&amp;rho;&lt;/sub&gt; yields a coefficient of around
2&amp;times;10&lt;sup&gt;&amp;minus;4&lt;/sup&gt; m&lt;sup&gt;2&lt;/sup&gt;s&lt;sup&gt;&amp;minus;1&lt;/sup&gt; although this increased by a factor of 2 near
the surface. Combining this estimate of &lt;i&gt;K&lt;/i&gt;&amp;rho;&lt;/sub&gt; with available
observations of average and maximum currents suggests the layer of
supercooled water can persist for a distance of ~250 km from the front
of the McMurdo Ice Shelf.</abstract>
	<references>
		<reference numeration="1" content_type="text"> % vor jede Referenz Albrecht, N., Vennell, R., Williams, M., Stevens, C., Langhorne, P., Leonard, G., and Haskell, T.: Observation of sub-inertial internal tides in McMurdo Sound, Antarctica, Geophys. Res. Lett., 33, L24606, doi:10.1029/2006GL027377, 2006. </reference>
		<reference numeration="2" content_type="text"> Arrigo, K. R., van Dijken, G., and Long, M.: Coastal Southern Ocean: A strong anthropogenic CO&lt;sub&gt;2&lt;/sub&gt; sink, Geophys. Res. Lett., 35, L21602, doi:10.1029/2008GL035624, 2008. </reference>
		<reference numeration="3" content_type="text"> Dempsey, D., Langhorne, P. J., Robinson, N. J., Williams, M. W. M., Haskell, T. G., and Frew, R.: Observation and modeling of platelet ice fabric in McMurdo Sound, Antarctica, to appear, J. Geophys. Res., doi:10.1029/2008JC005264, in press, 2009. </reference>
		<reference numeration="4" content_type="text"> Dillon, T. M.: Vertical Overturns: A Comparison of Thorpe and Ozmidov Length Scales, J. Geophys. Res., 87(C12), 9601–9613, 1982. </reference>
		<reference numeration="5" content_type="text"> Fer, I. and Widell, K.: Early spring turbulent mixing in an ice-covered Arctic fjord during transition to melting, Cont. Shelf Res., 27, 1980–1999, 2007. </reference>
		<reference numeration="6" content_type="text"> Galbraith, P. S. and Kelley, D. E.: Identifying overturns in CTD profiles, J. Atmos. Ocean. Tech., 13, 688–702, 1996. </reference>
		<reference numeration="7" content_type="text"> Goring, D. G. and Pyne, A.: Observations of sea-level variability in Ross Sea, Antarctica, N. Z. J. Mar. Freshwater Res., 37, 241–249, 2003. </reference>
		<reference numeration="8" content_type="text"> Hellmer, H. H.: Impact of Antarctic ice shelf melting on sea ice and deep ocean properties, Geophys. Res. Lett., 31, L10307, doi:10.1029/2004GL019506, 2004. </reference>
		<reference numeration="9" content_type="text"> Holland, P. R., Feltham, D. R., and Jenkins, A.: Ice Shelf Water plume flow beneath Filchner-Ronne Ice Shelf, Antarctica, J. Geophys. Res., 112, C05044, doi:10.1029/2006JC003915, 2007. </reference>
		<reference numeration="10" content_type="text"> Imberger, J. and Boashash, B.: Application of the Wigner-Ville distribution to temperature gradient microstructure: a new technique to study small-scale variations, J. Phys. Oceanogr., 16, 1997–2012, 1986. </reference>
		<reference numeration="11" content_type="text"> Imberger, J. and Ivey, G. N.: On the nature of turbulence in a stratified fluid. Part II: Observations, J. Phys. Oceanogr., 21, 659–675, 1991. </reference>
		<reference numeration="12" content_type="text"> Jacobs, S. S., Huppert, H. E., Holdsworth, G., and Drewry, D. J.: Thermohaline steps induced by melting of the Erebus Glacier Tongue, J. Geophys. Res., 86, 6547–6555, 1981. </reference>
		<reference numeration="13" content_type="text"> Jacobs, S., Hellmer, H. H., and Jenkins, A.: Antarctic ice sheet melting in the Southeast Pacific. Geophys. Res. Lett., 23, 957–960, 1996. </reference>
		<reference numeration="14" content_type="text"> Keeler, R. N., Bondur, V. G., and Gibson, C. H.: Optical satellite imagery detection of internal wave effects from a submerged turbulent outfall in the stratified ocean, Geophys. Res. Lett., 32, L12610, doi:10.1029/2005GL022390, 2005. </reference>
		<reference numeration="15" content_type="text"> Leonard, G. H., Purdie, C. R., Langhorne, P. J., Haskell, T. G., Williams, M. J. M., and Frew, R. D.: Observations of platelet ice growth and oceanographic conditions during the winter of 2003 in McMurdo Sound, Antarctica, J. Geophys. Res., 111, C04012, doi:10.1029/2005JC002952, 2006. </reference>
		<reference numeration="16" content_type="text"> Lueck, R.: Horizontal and vertical turbulence profilers, in: Marine Turbulence: Theories, Observations and Models, edited by: Baumert, H. Z., Simpson, J. H., and Sundermann, J., Cambridge Univ. Press, 89–100, 2005. </reference>
		<reference numeration="17" content_type="text"> Macoun, P. and Lueck, R. G.: Modelling the spatial response of the air-foil shear probe using different sized probes, J. Atmos. Ocean. Tech., 21, 284–297, 2004. </reference>
		<reference numeration="18" content_type="text"> McGuiness, M. J., Williams, M. J. M., Langhorne, P. J., Purdie, C., and Crook, J.: Frazil deposition under growing sea ice, J. Geophys. Res., 114, C07014, doi:10.1029/2007JC004414, 2009. </reference>
		<reference numeration="19" content_type="text"> McPhee, M. G.: Turbulent heat flux in the upper ocean under sea ice, J. Geophys. Res., 97, 5365–5379, 1992. </reference>
		<reference numeration="20" content_type="text"> McPhee, M. G.: Turbulent stress at the ice/ocean interface and bottom surface hydraulic roughness during the SHEBA drift, J. Geophys. Res., 107, 8037, doi:10.1029/2000JC000633, 2002. </reference>
		<reference numeration="21" content_type="text"> McPhee, M. G.: A spectral technique for estimating turbulent stress, scalar flux magnitude, and eddy viscosity in the ocean boundary layer under pack ice, J. Phys. Oceanogr., 34, 2180–2188, 2004. </reference>
		<reference numeration="22" content_type="text"> McPhee, M. G.: Air-ice-ocean-interaction: Turbulent Ocean Boundary Layer Exchange Processes, Springer, 215~pp., 2008. </reference>
		<reference numeration="23" content_type="text"> McPhee, M. G. and Morison, J. H.: Turbulence and diffusion: Under-ice boundary layer, in: Encyclopedia of Ocean Sciences, Academic Press, London, 3071–3078, 2001. </reference>
		<reference numeration="24" content_type="text"> McPhee, M. G. and Stanton, T. P.: Turbulence in the statically unstable oceanic boundary layer under Arctic leads, J. Geophys. Res., 101(C3), 6409–6428, 1996. </reference>
		<reference numeration="25" content_type="text"> Mitchell, W. M. and Bye, J. A. T.: Observations in the boundary layer under the sea ice in McMurdo Sound, in: Oceanology of the Antarctic Continental Shelf, edited by: Jacobs, S. S., Antarctic Research Series, 63, 167–176, 1985. </reference>
		<reference numeration="26" content_type="text"> Morison, J. H., Andersen, R. H., Larsen, N., D&apos;Asaro, E. A., and Boyd, T.: The correction for thermal inertia effects in Sea-Bird CTD data, J. Atmos. Ocean. Tech., 11, 1151–1164, 1994. </reference>
		<reference numeration="27" content_type="text"> Muench, R., Padman, L., Gordon, A., and Orsi, A.: A dense water outflow from the Ross Sea, Antarctica: Mixing and the contribution of tides, J. Mar. Sys., 77, 369–387, doi:10.1016/j.jmarsys.2008.11.003, 2009. </reference>
		<reference numeration="28" content_type="text"> Osborn, T.: Estimates of the local rate of vertical diffusion from dissipation measurements, J. Phys. Oceanogr., 10, 83–89, 1980. </reference>
		<reference numeration="29" content_type="text"> Payne, A. J., Holland, P. R., Shepherd, A. P., Rutt, I. C., Jenkins, A., and Joughin, I.: Numerical modeling of ocean-ice interactions under Pine Island Bay&apos;s ice shelf, J. Geophys. Res., 112, C10019, doi:10.1029/2006JC003733, 2007. </reference>
		<reference numeration="30" content_type="text"> Pease, C. H., Salo, S. A., and Overland, J. E.: Drag measurements for first-year sea ice over a shallow sea, J. Geophys. Res., 88, 2853–2862, 1983. </reference>
		<reference numeration="31" content_type="text"> Prandke, H.: Microstructure sensors, in: Marine Turbulence: Theories, Observations and Models, edited by: Baumert, H. Z., Simpson, J. H., and Sundermann, J., Cambridge Univ. Press, 101–109, 2005. </reference>
		<reference numeration="32" content_type="text"> Rainville, L., Winsor, P.: Mixing across the Arctic Ocean: Microstructure observations during the Beringia 2005 Expedition, Geophys. Res. Lett., 35, L08606, doi:10.1029/2008GL033532, 2008. </reference>
		<reference numeration="33" content_type="text"> Robertson, R. A., Padman, L., and Levine, M. D.: Finestructure, microstructure, and vertical mixing processes in the western Weddell Sea, J. Geophys Res., 100, 18517–18535, 1995. </reference>
		<reference numeration="34" content_type="text"> Robinson, N. J., Williams, M. J. W., Barrett, P. J., and Pyne, A. R.: Observations of flow and ice-ocean interactions beneath the McMurdo Ice Shelf, Antarctica, J. Geophys. Res., accepted, 2009. </reference>
		<reference numeration="35" content_type="text"> Roget, E., Lozovatsky, I., Sanchez, X., and Figueroa, M.: Microstructure measurements in natural waters: Methodology and applications, Prog. Oceanogr., 70, 126–148, 2006. </reference>
		<reference numeration="36" content_type="text"> Shaw, W. J., Stanton, T. P., McPhee, M. G., Morison, J. H., and Martinson, D. G.: Role of the upper ocean in the energy budget of Arctic sea ice during SHEBA, J. Geophys. Res., 114, C06012, doi:10.1029/2008JC004991, 2009. </reference>
		<reference numeration="37" content_type="text"> Shih, L. H., Koseff, J. R., Ivey, G. N., and Ferziger, J. H.: Parameterization of turbulent fluxes and scales using homogeneous sheared stably stratified turbulence simulations, J. Fluid Mech., 525, 193–214, 2005. </reference>
		<reference numeration="38" content_type="text"> Smedsrud, L. H. and Jenkins, A.: Frazil ice formation in an ice shelf water plume, J. Geophys. Res., 109, C03025, doi:10.1029/2003JC001851, 2004. </reference>
		<reference numeration="39" content_type="text"> Stacey, M. T., Monismith, S. G., and Burau, J. R.: Observations of turbulence in a partially stratified estuary, J. Phys. Oceanogr., 29, 1950–1970, 1999. </reference>
		<reference numeration="40" content_type="text"> Stacey, M. T., Burau, J. R., and Monismith, S. G.: Creation of residual flows in a partially stratified estuary. J. Geophys. Res., 106, 17013–17037, 2001. </reference>
		<reference numeration="41" content_type="text"> Stevens, C.: Turbulence in an Estuarine Embayment: Observations from Beatrix Bay, New Zealand, J. Geophys. Res., 108(C2), 3030, doi:10.1029/2001JC001221, 2003. </reference>
		<reference numeration="42" content_type="text"> Stevens, C. L. and Smith, M. J.: Temperature microstructure beneath surface gravity waves, J. Atmos. Ocean. Tech. 21, 1747–1757, 2004. </reference>
		<reference numeration="43" content_type="text"> Stevens, C. L., Williams, M. J. M, Robinson, N. J., Albrecht, N., and Haskell, T. G.: Observations of the Stratified Turbulent Boundary-layer and Platelet Ice Beneath McMurdo Sound Sea Ice, Proc. Sixth International Symposium on Stratified Flows, edited by: Ivey, G. N., Perth, Australia, 2006. </reference>
		<reference numeration="44" content_type="text"> St Laurent, L.: Turbulent dissipation on the margins of the South China Sea, Geophys. Res. Lett., 35, L23615, doi:10.1029/2008GL035520, 2008. </reference>
		<reference numeration="45" content_type="text"> Stroeve, J., Holland, M. M., Meier, W., Scambos, T., and Serreze, M.: Arctic sea ice decline: Faster than forecast, Geophys. Res. Lett., 34, L09501, doi:10.1029/2007GL029703, 2007. </reference>
		<reference numeration="46" content_type="text"> Svensson, U. and Omstedt, A.: Simulation of supercooling and size distribution in frazil ice dynamics, Cold Reg. Sci. Technol., 22, 221–233, 1994. </reference>
		<reference numeration="47" content_type="text"> Tennekes, H. and Lumley, J. L.: A First Course in Turbulence, MIT Press, 300~pp., 1972. </reference>
		<reference numeration="48" content_type="text"> Wesson, J. C. and Gregg, M. C.: Mixing at Camarinal Sill in the Strait of Gibraltar, J. Geophys. Res., 99, 9847–9878, 1994. </reference>
		<reference numeration="49" content_type="text"> Williams, M. J. M., Grosfeld, K., Warner, R. C., Gerdes, R., and Determann, J.: Ocean circulation and ice-ocean interaction beneath the Amery Ice Shelf, Antarctica, J. Geophys. Res., 106, 22383–22399, 2001. </reference>
		<reference numeration="50" content_type="text"> Zaron, E. D. and Egbert, G. D.: Estimating open-ocean barotropic tidal dissipation: The Hawaiian Ridge, J. Phys. Oceanogr., 36, 1019–1035, 2006. </reference>
	</references>
</article>

