Boundary-Layer Meteorology

, Volume 146, Issue 1, pp 133–147 | Cite as

Transport of Snow by the Wind: A Comparison Between Observations in Adélie Land, Antarctica, and Simulations Made with the Regional Climate Model MAR

  • Hubert Gallée
  • Alexandre Trouvilliez
  • Cécile Agosta
  • Christophe Genthon
  • Vincent Favier
  • Florence Naaim-Bouvet
Article

Abstract

For the first time a simulation of blowing snow events was validated in detail using one-month long observations (January 2010) made in Adélie Land, Antarctica. A regional climate model featuring a coupled atmosphere/blowing snow/snowpack model is forced laterally by meteorological re-analyses. The vertical grid spacing was 2 m from 2 to 20 m above the surface and the horizontal grid spacing was 5 km. The simulation was validated by comparing the occurrence of blowing snow events and other meteorological parameters at two automatic weather stations. The Nash test allowed us to compute efficiencies of the simulation. The regional climate model simulated the observed wind speed with a positive efficiency (0.69). Wind speeds higher than 12 m s−1 were underestimated. Positive efficiency of the simulated wind speed was a prerequisite for validating the blowing snow model. Temperatures were simulated with a slightly negative efficiency (−0.16) due to overestimation of the amplitude of the diurnal cycle during one week, probably because the cloud cover was underestimated at that location during the period concerned. Snowfall events were correctly simulated by our model, as confirmed by field reports. Because observations suggested that our instrument (an acoustic sounder) tends to overestimate the blowing snow flux, data were not sufficiently accurate to allow the complete validation of snow drift values. However, the simulation of blowing snow occurrence was in good agreement with the observations made during the first 20 days of January 2010, despite the fact that the blowing snow flux may be underestimated by the regional climate model during pure blowing snow events. We found that blowing snow occurs in Adélie Land only when the 30-min wind speed value at 2 m a.g.l. is >10 m s−1. The validation for the last 10 days of January 2010 was less satisfactory because of complications introduced by surface melting and refreezing.

Keywords

Antarctica Blowing snow Regional climate model Surface mass balance 

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References

  1. Agosta C, Favier V, Genthon C, Gallée H, Krinner G (2011) A 40-year surface accumulation dataset in Adélie Land coastal area (66°S, 139°E) and its application for atmospheric model validation. Clim Dyn. doi:10.1007/s00382-011-1103-4
  2. Andreas EL (1995) Physically based model of the form drag associated with sastrugi. CRREL Report No CR 95-16, pp 12Google Scholar
  3. Andreas EL, Jordan RE, Makshtas AP (2005) Parameterizing turbulent exchange over sea ice: the ice station Weddell results. Boundary-Layer Meteorol 114: 439–460CrossRefGoogle Scholar
  4. Bellot H, Trouvilliez A, Naaim-Bouvet F, Genthon C, Gallée H (2011) Present weather-sensor tests for measuring drifting snow. Ann Glaciol 58: 176–184CrossRefGoogle Scholar
  5. Bintanja R (1998) The interaction between drifting snow and atmospheric turbulence. Ann Glaciol 26: 167–173Google Scholar
  6. Bintanja R (2000) Snowdrift suspension and atmospheric turbulence. Part I: theoretical background and model description. Boundary-Layer Meteorol 95: 343–368CrossRefGoogle Scholar
  7. Bintanja R (2001) Modification of the wind speed profile caused by snowdrift: results from observations. Q J R Meteorol Soc 127: 2417–2434. doi:10.1002/qj.49712757712 CrossRefGoogle Scholar
  8. Bromwich DH (1988) Snowfall in high southern latitudes. Rev Geophys 26: 149–168CrossRefGoogle Scholar
  9. Budd WF, Dingle WRJ, Radok U (1965) The Byrd snow drift project: outline and basic results. Am Geophys Union Antarct Res Ser 7: 71–134Google Scholar
  10. Cassano JJ, Parish TR (2000) An analysis of the nonhydrostatic dynamics in numerically simulated Antarctic katabatic flows. J Atmos Sci 57: 891–898CrossRefGoogle Scholar
  11. Chritin V, Bolognesi R, Gubler H (1999) FlowCapt: a new acoustic sensor to measure snowdrift and wind veocity for avalanche forecasting. Cold Reg Sci Technol 30: 125–133CrossRefGoogle Scholar
  12. Cierco F-X, Naaim-Bouvet F, Bellot H (2007) Acoustic sensors for snowdrift measurements: how should they be used for research purposes. Cold Reg Sci Technol 49: 74–89CrossRefGoogle Scholar
  13. State of the climate in 2009: (2010) Surface manned and automatic weather station observations. Bull Am Meteorol Soc 91(7): S128–S129Google Scholar
  14. Dee DP, Uppala SM, Simmons AJ, Berrisford P, Poli P, Kobayashi S, Andrae U, Balmaseda MA, Balsamo G, Bauer P, Bechtold P, Beljaars ACM, van de Berg L, Bidlot J, Bormann N, Delsol C, Dragani R, Fuentes M, Geer AJ, Haimberger L, Healy SB, Hersbach H, Hólm EV, Isaksen L, Kållberg P, Köhler M, Matricardi M, McNally AP, Monge-Sanz BM, Morcrette J-J, Park B-K, Peubey C, de Rosnay P, Tavolato C, Thépaut J-N, Vitart F (2011) The ERA-Interim reanalysis: configuration and performance of the data assimilation system. Q J R Meteorol Soc 137: 553–597. doi:10.1002/qj.828 CrossRefGoogle Scholar
  15. De Ridder K, Gallée H (1998) Land surface-induced regional climate change in Southern Israel. J Appl Meteorol 37: 1470–1485. doi:10.1175/1520-0450 CrossRefGoogle Scholar
  16. Duynkerke PG, Driedonks AGM (1987) A model for the turbulent structure of the stratocumulus-topped atmospheric boundary layer. J Atmos Sci 44: 43–64CrossRefGoogle Scholar
  17. Favier V, Agosta C, Genthon C, Arnaud L, Trouvillez A, Gallée H (2011) Modeling the mass and surface heat budgets in a coastal blue ice area of Adelie Land, Antarctica. J Geophys Res 116: F03017. doi:10.1029/2010JF001939 CrossRefGoogle Scholar
  18. Frezzotti M, Gandolfi S, La Marca F, Urbini S (2002) Snow dunes and glazed surfaces in Antarctica: new field and remote-sensing data. An Glaciol 34(1): 81–88CrossRefGoogle Scholar
  19. Gallée H (1995) Simulation of the mesocyclonic activity in the Ross Sea, Antarctica. Mon Weather Rev 123: 2051–2069CrossRefGoogle Scholar
  20. Gallée H (1998) A simulation of blowing snow over the Antarctic ice sheet. Ann Glaciol 26: 203–205Google Scholar
  21. Gallée H, Gorodetskaya I (2010) Validation of a limited area model over Dome C, Antarctic Plateau, during winter. Clim Dyn 23(1): 61–72. doi:10.1007/s00382-008-0499-y CrossRefGoogle Scholar
  22. Gallée H, Pettré P (1998) Dynamical constraints on katabatic wind cessation in Adélie Land, Antarctica. J Atmos Sci 55: 1755–1770CrossRefGoogle Scholar
  23. Gallée H, Schayes G (1994) Development of a three-dimensional meso-gamma primitive equations model, katabatic winds simulation in the area of Terra Nova Bay, Antarctica. Mon Weather Rev 122: 671–685CrossRefGoogle Scholar
  24. Gallée H, Guyomarc’h G, Brun E (2001) Impact of snow drift on the ntarctic ice sheet surface mass balance. Possible sensitivity to snow surface properties. Boundary-Layer Meterorol 99: 1–19CrossRefGoogle Scholar
  25. Gallée H, Pettré P, Schayes G (1996) Sudden cessation of katabatic winds in Adélie Land, Antarctica. J Appl Meteorol 35: 1142–1152CrossRefGoogle Scholar
  26. Gallée H, Peyaud V, Goodwin I (2005) Simulation of the net snow accumulation along the Wilkes land transect, Antarctica, with a regional climate model. Ann Glaciol 41: 17–22CrossRefGoogle Scholar
  27. Genthon C, Lardeux P, Krinner G (2007) The surface accumulation and ablation of a blue ice area near Cap Prudhomme, Adélie Land, Antarctica. J Glaciol 183(53): 635–645CrossRefGoogle Scholar
  28. Genthon C, Six D, Favier V, Lazzara M, Keller L (2011) Atmospheric temperature measurement biases on the Antarctic Plateau. J Atmos Ocean Technol (28):1598–1605Google Scholar
  29. Gosink JP (1989) The extension of a density current model of katabatic winds to include the effects of blowing snow and sublimation. Boundary-Layer Meterorol 49(4): 367–394. doi:10.1007/BF00123650 CrossRefGoogle Scholar
  30. Kessler E (1969) On the distribution and continuity of water substance in atmospheric circulations. Met. Monograph 10, No. 32. American Meteorological Society, Boston, pp 84Google Scholar
  31. Kodama Y, Wendler G, Gosink J (1985) The effect of blowing snow on katabatic winds in Antarctica. Ann Glaciol 6: 59–62Google Scholar
  32. Kotlyakov VM (1961) Results of a study of the processes of formation and structure of the upper layer of the ice sheet in Eastern Antarctica. Antarctic glaciology 55. IAHS Press, Wallingford, pp 88–99Google Scholar
  33. König-Langlo G, King JC, Pettré P (1998) Climatology of the three coastal Antarctic stations Dumont d’Urville, Neumayer, and Halley. J Geophys Res 103(D9): 10935–10946. doi:10.1029/97JD00527 CrossRefGoogle Scholar
  34. König-Langlo GC, Loose B (2007) The meteorological observatory at Neumayer stations (GvN and NM-II), Antarctica. Polarforschung 76: 25–38Google Scholar
  35. Lenaerts JTM, van den Broeke MR, Déry SJ, König-Langlo G, Ettema J, Kuipers Munneke P (2010) Modelling snowdrift sublimation on an Antarctic ice shelf. Cryosphere Discuss 4: 121–152. doi:10.5194/tcd-4-121-2010 CrossRefGoogle Scholar
  36. Lenaerts JTM, van den Broeke MR, van de Berg WJ, van Meijgaard E, Kuipers Munneke P (2012) A new, high resolution surface mass balance map of Antarctica (1979–2010) based on regional climate modeling. Geophys Res Lett 39: L04501. doi:10.1029/2011GL050713 CrossRefGoogle Scholar
  37. Lenaerts JTM, van den Broeke MR, Déry SJ, van Meijgaard E, van de Berg WJ, Palm SP, Sanz Rodrigo J (2012) Modeling drifting snow in Antarctica with a regional climate model, Part I: methods and model evaluation. J Geophys Res 117: D05108. doi:10.1029/2011JD016145 CrossRefGoogle Scholar
  38. Levkov L, Rockel B, Kapitza H, Raschke E (1992) 3D meso-scale numerical studies of cirrus and stratus clouds by their time and space evolution. Contrib Atmos Phys 65: 35–58Google Scholar
  39. Lin YJ, Farley RD, Orville HD (1983) Bulk parameterization of the snow-field in a cloud model. J Clim Appl Meteorol 22: 1065–1092CrossRefGoogle Scholar
  40. Mahesh A, Eager R, Campbell JR, Spinhirne JD (2003) Observations of blowing snow at the South Pole. J Geophys Res 108(D22): 4707. doi:10.1029/2002JD003327 CrossRefGoogle Scholar
  41. Male DH (1980) The seasonal snow cover. In: Colbeck SA (ed) Dynamics of snow and ice masses. Academic Press Inc., New York, pp 305–395CrossRefGoogle Scholar
  42. Mann GW, Anderson PS, Mobbs SD (2000) Profile measurements of blowing snow at Halley, Antarctica. J Geophys Res 105: 24491–24508CrossRefGoogle Scholar
  43. Marticorena B, Bergametti G (1995) Modeling the atmospheric dust cycle: 1. Design of a soil-derived dust emission scheme. J Geophys Res 100: 16415–16430CrossRefGoogle Scholar
  44. Mellor M, Fellers G (1986) Concentration and flux of wind-blown snow, US Army Corps of Engineers, Special Report 86-11Google Scholar
  45. Meyers MP, DeMott PJ, Cotton WR (1992) New primary ice nucleation parameterizations in an explicit cloud model. J Appl Meteorol 31: 708–721CrossRefGoogle Scholar
  46. Morcrette J-J (2002) Assessment of the ECMWF model cloudiness and surface radiation fields at the ARM-SGP site. Mon Weather Rev 130: 257–277CrossRefGoogle Scholar
  47. Naaim-Bouvet F, Bellot H, Naaim M (2010) Back analysis of drifting snow measurements over an instrumented mountainous site. Ann Glaciol 51(54): 207–217CrossRefGoogle Scholar
  48. Nash JE, Sutcliffe JV (1970) River flow forecasting through conceptual models part I. A discussion of principles. J Hydrol 10(3): 282–290. doi:10.1016/0022-1694(70)90255-6 CrossRefGoogle Scholar
  49. Parish TR (1988) Surface winds over the Antarctic continent: a review. Rev Geophys 26(1): 169–180. doi:10.1029/RG026i001p00169 CrossRefGoogle Scholar
  50. Scarchilli C, Frezzotti M, Grigioni P, Silvestri L, Agnoletto L, Dolci S (2010) Extraordinary blowing snow transport events in East Antarctica. Clim Dyn 34(7–8): 1195–2306CrossRefGoogle Scholar
  51. Solomon S, Qin D, Manning M, Chen Z, Marquis M, Averyt KB, Tignor M, Miller HL (eds.) (2007) Contribution of working group I to the fourth assessment report of the intergovernmental panel on climate change. Cambridge University Press, Cambridge, p 996Google Scholar
  52. Stearns CR, Wendler G (1988) Research results from Antarctic automatic weather stations. Rev Geophys 26(1): 45–61CrossRefGoogle Scholar
  53. Takahashi S (1985) Characteristics of drifting snow at Mizuho Station, Antarctica. Ann Glaciol 6: 71–75Google Scholar
  54. Walden Von P, Warren SG, Tuttle E (2003) Atmospheric ice crystals over the Antarctic Plateau in Winter. J Appl Meteor 42: 1391–1405CrossRefGoogle Scholar
  55. Wamser C, Lykossov VN (1995) On the friction velocity during blowing snow. Contrib Atmos Phys 68: 85–94Google Scholar

Copyright information

© Springer Science+Business Media B.V. 2012

Authors and Affiliations

  • Hubert Gallée
    • 1
  • Alexandre Trouvilliez
    • 1
    • 2
  • Cécile Agosta
    • 1
  • Christophe Genthon
    • 1
  • Vincent Favier
    • 1
  • Florence Naaim-Bouvet
    • 2
  1. 1.UJF–Grenoble 1 / CNRSLaboratoire de Glaciologie et Géophysique de l’Environnement (LGGE) UMR 5183GrenobleFrance
  2. 2.IRSTEA, UR ETGR Erosion Torrentielle Neige AvalanchesDomaine universitaireSaint-Martin-d’HèresFrance

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