渤海海冰中太阳辐射的光谱特征观测研究

曲平; 赵进平; 李淑江; 曹文熙; 许大志

渤海海冰中太阳辐射的光谱特征观测研究

1.
国家海洋局, 第一海洋研究所, 山东, 青岛, 266061
2.
中国海洋大学, 山东, 青岛, 266100
3.
中国科学院, 南海海洋研究所, 广东, 广州, 510301

基金项目: 国家“863”计划支持项目(2003AA639330)

计量
- 文章访问数: 1296
- HTML全文浏览量: 16
- PDF下载量: 1267
- 被引次数: 0
出版历程
- 收稿日期: 2008-05-15
- 修回日期: 2008-12-22

Spectral features of solar radiation in sea ice of Bohai Sea

1.
First Institute of Oceanography, State Oceanic Administration, Qingdao 266061, China
2.
Ocean University of China, Qingdao, 266100, China
3.
South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou 510301, China

摘要

摘要: 通过采用多光谱仪器,对渤海营口港一带的近岸固定冰进行了3个站位11个谱段的入射辐射、反射辐射和透射辐射随时间变化过程的观测和研究。结果表明,发生在海冰中的反射辐射和透射辐射与入射太阳辐射的谱分布有明显差别,而且有显著的日变化。文章确立了入射辐射、反射辐射和透射辐射随时间的变化与太阳高度角的正弦成精确的线性关系,海冰的积分反照率与太阳高度角的正弦满足二次函数关系,可将不同时刻的观测值归算到正午时刻的辐射值,使不同时刻的观测结果具有可比性。计算结果表明,海冰只衰减特定强度的辐射,衰减量与入射辐射光谱分布以及辐射的强度无关,导致绿光的透射辐射最强。该文是对渤海海冰透射辐射的初步尝试,所获得的结果对未来大范围海冰光学观测打下了基础。
- 渤海 /
- 海冰 /
- 光学 /
- 太阳辐射 /
- 谱分布
Abstract: Sea ice is a yearly occurred phenomenon in Bohai Sea of China.Optical feature of sea ice is important to the evolution of ice it self.In this study,a multi-spectral instrument system with 11 wavelengths was used to measure the incident,reflected,and transmitted radiations and their daily variations for the costal fastice in three locations near the Yingkou Harbor,west flank of the Liaodong Peninsula.Although the spectral distribution of arrived solar radiation was a double peaks structure,the reflectance and transmission were discrepant with it.Integrals of incidence,reflectance and transmission radiations are perfectly simulated by linear functions of solar height,and the albedo is simulated by a quadric function of solar height,which can revert the observation values in different time of day to that in noontime and make them comparable.The attenuation feature of sea ice for solar light is quite special that the at tenuated radiation by sea ice was independent of the solar radiation intensity and wavelength.As the ice thickness and of components in sea ice changed a little during the experiment,as a short coming of this paper,the impact from the thickness and microstructure of sea ice cannot be studied.
- Bohai Sea /
- sea ice /
- optics /
- solar radiation /
- spectral distribution

HTML全文

参考文献(27)

季顺迎,岳前进.渤海海冰特征厚度分析[J].海洋学报,2000,22(6):117-123.

张方俭.我国的海冰[M].北京:海洋出版社,1986:165.

STURM M D,PEROVICH K,HOLMGREN J.Thermal conductivity and heat transfer through the snow on the ice of the Beaufort Sea[J/OL].J Geophys Res,2002,107:doi: 10.1029/2000JC000409.

赵进平,侍茂崇,李诗新.低盐区及渤海低盐区的盐度特征[J].海洋科学集刊,1998,40:249-260.

PEROVICH D K.The Optical Properties of Sea Ice[M].Monograph 96-1,US Army Corps of Engineers,Cold Regions Research & Engineering Laboratory,1996.

赵进平,李涛,张树刚,等.北冰洋中央密集冰区海冰对太阳短波辐射能吸收的观测研究[J].地球科学进展,2009,24(1):34-42.

岳前进,陈祥余.海冰侧限剪切强度的实验方法[J].冰川与冻土,1994,16(1):75-79.

MAYKUT G A.The surface heat and mass balance[M]//UNTERSTEINER N.The Geophysics of Sea Ice,NATO ASI Series B:Physics Vol.146.New York:Plenum Press,1986:395-464.

HOIOLAND M M,BITZ C M,HUNKE E C,et al.Influence of the sea ice thickness distribution on polar climate in CCSm³[J].J Clim,2006,19(11):2398-2414.

CURRY J A,SCHRAMM J L,EBERT E E.Sea ice-albedo climate feedback mechanism[J].J Clim,1995,8:240-247.

SPANO A F.Results of an airborne albedo program in Antarctica[J].Mort Weather Rev,1965,93:697-703.

GRENFELL T C,PEROVICH D K.Spectral albedos of sea ice and incident solar irradiance in the southern Beaufort Sea[J].J Geophys Res,1984,89(C7):3573-3580.

ANDREAS E L,MAKSHTAS A P.Energy exchange over Antarctic sea ice in the spring[J].J Geophys Res,1985,90:7199-7212.

PEROVICH D K.The evolution of sea ice optical properties during fall freeze-up[M]//Ocean Optics 10.Proc.SPIE Int,Sec.Opt.Eng.,1990,1302:520-531.

ALLISON I,BRANDT R E.WARREN S G.East Antarctic sea ice:Albedo,thickness distribution,and snow cover[J].J Geophys Res,1993,98:12417-12429.

BRANDT R E,WARREN S G,WORBY A P,et al.Surface albedo at the Antarctic sea ice gone[J].J Clim,2005,18:3606-3622.

MULLEN P C,WARREN S G.Theory of the optical properties of lake ice[J].J Geophys Res,1988,93:8403-8414.

GRENFEIL T C The effect of ice thickness on the exchange of solar radiation over the polar oceans[J].J Glaciol,1979,22:305-320.

GRENFELlT C.A radiative transfer model for sea ice with vertical structure variations[J].J Geophys Res,1991,96:16991-17001.

MAYKUT G,GRENFELL T C.The spectral distribution of light beneath first-year sea ice in the Arctic Ocean[J].Limnology and Oce-anography,1975,20(4):554-563.

TRODAHL H J,BUCKLEY R G.Ultraviolet levels under spa ice during the Antarctic spring[J].Science,1989,245(4914):194-195.

DONALD K,PEROVICH D K.Observations of ultraviolet light reflection and transmission by first-year sea ice[J].Geophys Res Lett,1995,22(11):1349-1352.

HAMRE B,WINTHER J G,GERLAND S,et al.Modeled and measured optical transmittance of snow-covered first-year sea ice in Kongsfjorden,Svalbard[J/OL].J Geophys Res,2004,109:C10006.doi: 10.1029/2003JC001926.

岳前进,季顺迎,苗文东,等.辽东湾冰季太阳辐射分析[J].海洋与湖沼,2000,31(5):562-567.

许大志,曹文熙,孙兆华.辽东湾海冰光衰减特性[J].海洋通报.2007,26(1):12-19.

田烟忠司.物理海洋学(第四卷)[M].东京:东海大学出版会,1970:115-221.

LIGHT B,EICHEN H,MAYKUT G A,et al.The effect of induced particulates on the spectral albedo of sea ice[J].J Geophys Res,1998,103(C12):27739-27752.

施引文献

资源附件(0)

访问统计