Articles

The Shortwave Solar Radiation Energy Absorbed by Packed Sea Ice in the Central Arctic

  • ZHAO Jinping ,
  • ZHANG Shugang ,
  • JIAO Yutian ,
  • LI Tao
Expand
  • Ocean University of China, Qingdao 266100, China

Received date: 2008-11-28

  Revised date: 2008-12-15

  Online published: 2009-01-10

Abstract

The solar energy is the main energy source to melt sea ice in the Arctic. The solar energy absorbed by the packed ice in the central Arctic is studied in this paper based on the optical observations of the Third Chinese Arctic Expedition on an ice camp during the period of August 21-27, 2008. The transmission, albedo, and the absorption rates of the sea ice and their variation with ice thickness are calculated from the observed data. On average, the absorption rate of sea ice for shortwave solar radiation is about 16%, meanwhile, about 77% of the incident energy is reflected back to the space. A three-day optical observation was conducted to determine the amount of the arriving solar radiation. Although the solar radiation arriving on the upper atmosphere was still strong in August, but about 57% of them was reduced by the atmosphere, as the coverage of cloud and fog caused obvious absorption to the shortwave radiation. Therefore, the heat flux absorbed by sea ice was only 10.2W/m2, corresponding to the heat in melting 2.6 mm ice per day or 1 m ice within 380 days. It means that the weak heat flux did not provide sufficient heat to melt the sea ice there. Therefore, the packed ice still covers the central Arctic Ocean even though the ice coverage becomes nearly the minimum in the whole Arctic. However, the result also indicated that some other factors, if appeared, could cause the increased melting of the packed ice, such as the decrease of cloud and fog, the total melting of snow layer, the reduction of ice thickness, and the increase of the ponds which could especially endanger the permanent packed ice. In the future, it is possible for the sea ice in central Arctic to collapse if more heat is absorbed under the condition different to that of the summer of 2008.

Cite this article

ZHAO Jinping , ZHANG Shugang , JIAO Yutian , LI Tao . The Shortwave Solar Radiation Energy Absorbed by Packed Sea Ice in the Central Arctic[J]. Advances in Earth Science, 2009 , 24(1) : 33 -41 . DOI: 10.11867/j.issn.1001-8166.2009.01.0033

References

[1] Parkinson C L, Cavalieri D J, Gloersen P, et al. Arctic sea ice extents, areas and trends, 1978-1996[J].Journal of  Geophysical Research,1999, 104(C9): 20 837-20 856.
[2] Tucker III W B, Weatherly J W, Eppler D T, et al. Evidence for rapid thinning of sea ice in the western Arctic Ocean at the end of the 1980s[J].Geophysical Research Letters,2001, 28: 2 851-2 854.
[3] Lindsay R W, Zhang J. The thinning of Arctic sea ice, 1988-2003: Have we passed a tipping point?[J].Journal of Climate, 2005, 18(22): 4 879-4 894.
[4] Perovich D K. The Optical Properties of Sea Ice[R]. Monograph 96-1, US Army Corps of Engineers, Cold Regions Research & Engineering Laboratory, 1996:31.
[5] Holland M M, Bitz C M, Hunke E C, et al. Influence of the sea ice thickness distribution on polar climate in CCSM3[J].Journal of Climate, 2006,19(11):2 398-2 414.
[6] Grenfell T C, Maykut G A. The optical properties of ice and snow in the Arctic basin[J].Journal of Glaciol,1977, 18: 445-463.
[7] Perovich D K, Roesler C S, Pegau W S. Variability in Arctic sea ice optical properties[J].Journal of Geophysical Research, 1998, 103: 1 193-1 208.
[8] Light B, Grenfell T C, Perovich D K. Transmission and absorption of solar radiation by Arctic sea ice during the melt season[J]. Journal of Geophysical Research, 2008, 113, C03023, doi: 10.1029/2006JC003977.
[9] Maykut G A, Grenfell T C. The spectral distribution of light beneath first-year sea ice in the Arctic Ocean[J].Limnology and Oceanography, 1975, 20(4): 554-563.
[10] Perovich D K, Cota G F, Maykut G A, et al. Biooptical observations of 1st-year Arctic sea-ice[J].Geophysical Research Letters, 1993, 20: 1 059-1 062.
[11] Mobley C D, Cota G F, Grenfell T C, et al.Modeling light propagation in sea ice[J].IEEE Transactions on Geoscience and Remote Sensing, 1998,36:1 743-1 749.
[12] Perovich D K, Longacre J, Barber D G, et al. Field observations of the electromagnetic properties of first-year sea ice[J]. IEEE Transactions on Geoscience and Remote Sensing, 1998, 36: 1 705-1 715.
[13] Pegau W S, Zaneveld J R V. Field measurements of in-ice radiance[J].Cold Regions Science and Technology, 2000, 31: 33-46.
[14] Barber D G, Massom R A. The role of sea ice in Arctic and Antarctic Polynyas[C]//Smith W O,Barber  D G,eds. Polynyas: Windows to the World. Elsevier Oceanography Series, 2007, 74: 1-54.
[15] Hanesiak J M, Barber D G, DeAbreu R A, et al. Local and regional albedo observations of Arctic first-year sea ice during melt ponding[J].Journal of Geophysical Research, 2001, 106(C1): 1 005-1 016.
[16] Maykut G A. Largescale heat exchange and ice production in the central Arctic[J].Journal of Geophysical Research, 1982, 87(C10):7 971-7 984.
[17] Weller G. Radiation flux investigations[J].AIDJEX Bulletin, 1972,14:28-30.
[18] Maykut G A, Light B. Refractive index measurements in freezing sea ice and sodium chloride brines[J].Applied Optics,1995, 34:950-961.
[19] Zhao Jinping, Li Tao, Barber D G, et al. Attenuation of artificial lateral propagating light in winter Arctic sea ice[J].Journal of Geophysical Research, 2009.
[20] Gill A E. Atmosphere-Ocean Dynamics[M]. San Diego: Academic, 1982:662.
[21] Duffie J A, Beckman W A. Solar Engineering of Thermal Processes (third edition)[M]. New York: Wiley & Sons, 2006.
[22] Hobbs P V. Ice Physics[M]. London: Oxiford University Press, 1974.

Outlines

/