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1)  sea ice shelf
浮冰洲
2)  drifting ice
浮冰
1.
WT5BZ] The variations of meteorological elements such as temperature, pressure, humidity, wind speed, cloud cover, radiation components and ice temperature, the weather process as well are presented based on the data obtained by Chinese National Arctic Expedition on a drifting ice at (75°N,160°W) in Arctic Ocean in August 19-24,1999.
利用中国首次北极科学考察队观测的气象资料 ,初步分析研究了 1 999年 8月 1 9~ 2 4日北冰洋浮冰 ( 75°N,1 60°W)上的温、压、湿、风、云量、辐射、海表温度、冰面及冰中温度等气象要素变化特征 ,并结合 50 0 h Pa高度场分析了该期间的天气过程。
2.
Characteristics of heat balance parameters of Arctic Ocean drifting ice and open sea are presented based on the profile flux method and the data obtained by the First Chinese National Arctic Research Expedition during Aug.
利用中国首次北极考察队于 1 999年 8月 1 9日~ 2 4日在北冰洋浮冰区获得的大气近地层垂直廓线和辐射等资料 ,依据相似理论方法 ,对比分析了北冰洋无冰海面和冰面上热平衡参数的变化特征。
3)  pack ice
浮冰
1.
The recent progress in the studies of Arctic pack ice ecology;
北极浮冰生态学研究进展
4)  floe [英][fləʊ]  [美][flo]
浮冰
1.
Based on the marine hydrographic data observed in the sea area(64°00′ to 69°15′S,68°00′ to 76°00′E) during the 22nd Antarctic Expedition of China in the 2005/2006 austral summer,the water mass characteristics in the floe area near the north edge of Emery ice shelf in the Prydz Bay are analyzed.
根据2005-2006年夏季中国南极第22次南极科学考察的海洋水文资料(64°00′~69°15′S,68°00′~76°00′E),分析了普里兹湾内Emery冰架北缘浮冰区的水团性质。
5)  pack ice
浮冰;块冰
6)  iceland crystal
冰洲石
1.
With dual beam path spectrophotometer,the transmitted spectra of the five natural iceland crystal samples with different appearance colour have been tested.
利用岛津分光光度计双光路法测试了 5种外观颜色不同的天然冰洲石晶体的透射光谱 ;结果表明 ,冰洲石样品外观为微黄色的晶体 ,在紫外透光性能最好 ,是制作紫外偏光镜的理想材料。
2.
The authors deduced a dispersion equation of Iceland crystal by fitting with computer, it agreeded very well with the experimental findings in the spectral reigon from near ultraviolet band to near infrared band.
利用计算机拟和技术推导出了冰洲石晶体的色散方程 ,由此方程计算的冰洲石晶体折射率在近紫外、可见和近红外光谱区域与实验数据符合的很好 。
补充资料:浮冰块

fúbīngkuài

[floe] 海面上或其他水面上的大片浮冰

说明:补充资料仅用于学习参考,请勿用于其它任何用途。
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