光谱学与光谱分析
光譜學與光譜分析
광보학여광보분석
SPECTROSCOPY AND SPECTRAL ANALYSIS
2014年
3期
614-618
,共5页
王婷婷%赵云升%张洪岩%张霞%张丽莉
王婷婷%趙雲升%張洪巖%張霞%張麗莉
왕정정%조운승%장홍암%장하%장려리
光谱学%热红外%偏振%冰%多角度
光譜學%熱紅外%偏振%冰%多角度
광보학%열홍외%편진%빙%다각도
Spectroscopy%Thermal radiation%Polarization%Ice%Multi-angle
冰作为全球能量平衡、气候、水文和生态模型中的重要参数,直接影响到地气系统能量平衡、天气和气候变化等,利用热红外波段对冰偏振特性研究国内外尚未见报道,运用热红外技术对冰热辐射偏振研究有重要意义。研究结果表明,波段、探测角、偏振角对冰热辐射偏振特性均有较大影响,而方位角影响不显著。振辐亮度表现为:LCH1> LCH3> LCH4> LCH2,偏振亮温表现为 TCH4> TCH1> TCH2> TCH3,对冰热辐射偏振特性研究选择第三通道偏振亮温数据更优。探测角对冰热辐射特性影响极其显著且受偏振角影响,冰在探测角10°、偏振角30°处偏振亮温最低,这非偶然因素造成,与冰自身特性有关,探测角对冰偏振度影响表现为 P0< P40< P10< P20< P50< P30,偏振度大小与各偏振角的亮温差异大小直接相关,方位角对冰偏振亮温影响不显著,表面粗糙程度与组织结构差异直接导致冰在不同方位角发射辐射差异,利用偏振度对冰理化特性监测具有重要作用。
冰作為全毬能量平衡、氣候、水文和生態模型中的重要參數,直接影響到地氣繫統能量平衡、天氣和氣候變化等,利用熱紅外波段對冰偏振特性研究國內外尚未見報道,運用熱紅外技術對冰熱輻射偏振研究有重要意義。研究結果錶明,波段、探測角、偏振角對冰熱輻射偏振特性均有較大影響,而方位角影響不顯著。振輻亮度錶現為:LCH1> LCH3> LCH4> LCH2,偏振亮溫錶現為 TCH4> TCH1> TCH2> TCH3,對冰熱輻射偏振特性研究選擇第三通道偏振亮溫數據更優。探測角對冰熱輻射特性影響極其顯著且受偏振角影響,冰在探測角10°、偏振角30°處偏振亮溫最低,這非偶然因素造成,與冰自身特性有關,探測角對冰偏振度影響錶現為 P0< P40< P10< P20< P50< P30,偏振度大小與各偏振角的亮溫差異大小直接相關,方位角對冰偏振亮溫影響不顯著,錶麵粗糙程度與組織結構差異直接導緻冰在不同方位角髮射輻射差異,利用偏振度對冰理化特性鑑測具有重要作用。
빙작위전구능량평형、기후、수문화생태모형중적중요삼수,직접영향도지기계통능량평형、천기화기후변화등,이용열홍외파단대빙편진특성연구국내외상미견보도,운용열홍외기술대빙열복사편진연구유중요의의。연구결과표명,파단、탐측각、편진각대빙열복사편진특성균유교대영향,이방위각영향불현저。진복량도표현위:LCH1> LCH3> LCH4> LCH2,편진량온표현위 TCH4> TCH1> TCH2> TCH3,대빙열복사편진특성연구선택제삼통도편진량온수거경우。탐측각대빙열복사특성영향겁기현저차수편진각영향,빙재탐측각10°、편진각30°처편진량온최저,저비우연인소조성,여빙자신특성유관,탐측각대빙편진도영향표현위 P0< P40< P10< P20< P50< P30,편진도대소여각편진각적량온차이대소직접상관,방위각대빙편진량온영향불현저,표면조조정도여조직결구차이직접도치빙재불동방위각발사복사차이,이용편진도대빙이화특성감측구유중요작용。
As an important parameter of the global energy balance ,climate ,hydrological and ecological model ,ice directly af-fects the energy balance of the earth-atmosphere system ,weather and climate .It is of great significance to use the thermal infra-red polarization technology to study ice thermal radiation .For the ice monitoring and the impact of global climate change on the ice ,studies on ice thermal radiation polarization characteristics were conducted based on the wavelength ,detection angle and azi-muth angle .The results show that the wavelength has an obvious impact on the ice thermal radiation polarization properties .The polarized radiance of four bands shows that LCH1 > LCH3 > LCH4 > LCH2 while the polarization brightness temperature shows that TCH4 > TCH1 > TCH2 > TCH3 .It’s better to use the brightness temperature of the third channel than the radiance to study the ther-mal radiation polarization .The detection angle affects the ice thermal radiation polarization characteristics greatly and there are some differences between the polarization angles .The brightness temperature of ice is the lowest in the detection angle of 10° and the polarization angle of 30° ,which are non-accidental factors .These was closely related to ice physical and chemical properties . The degree of ice polarization performance shows that P0 < P40 < P30 < P50 < P10 < P20 and is affected by the detection angle , which is directly related to the differences in the brightness temperature at different polarization angles .The degree of polariza-tion changes with the azimuth angles and plays an important role in ice physical and chemical characteristics monitoring .The im-pact of azimuth angle on the ice thermal radiation polarization characteristics was not significant .And it is affected by the rough-ness of the surface ,organizational structure and other factors which are direct results of ice emitted radiation at different azimuth ang les .