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首页> 外文期刊>Journal of Geophysical Research. Biogeosciences >Observations by the Lidar In-Space Technology Experiment (LITE) of high-altitude cirrus clouds over the equator in regions exhibiting extremely cold temperatures
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Observations by the Lidar In-Space Technology Experiment (LITE) of high-altitude cirrus clouds over the equator in regions exhibiting extremely cold temperatures

机译:激光雷达太空技术实验(LITE)对极端寒冷地区赤道上方的高空卷云的观测

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Data from the Lidar In-Space Technology Experiment (LITE) were used to locate clouds near the equatorial tropopause and retrieve temperatures in cloud layers. The experiment was conducted aboard the space shuttle Discovery on September 9-20, 1994. LITE observations over the equator frequently exhibit cloud layers near the tropopause with scattering ratios as high as 2.5 at 532 nm. These clouds have been characterized as cirrus and subvisible cirrus. The clouds were observed near the tropopause with cloud top temperatures ranging from 185 to 200 K, Statistical averages of two optical properties observed by LITE in the 5 degreesN to 15 degreesS latitude band, the wavelength dependence of the extinction due to aerosols (Angstrom coefficient) and scattering ratios, were computed. The Angstrom coefficients show that a significant number (31%) of these high-altitude cirrus clouds observed by LITE in the 5 degreesN to 15 degreesS latitude band have optical similarities to type la polar stratospheric cloud (PSC) pal-tides. Sixty-six percent of the clouds observed are thin, with scattering ratios ranging from 1.1 to 1.5. Since these clouds are most likely to form at temperatures of 185 +/- 2.5 It (a 90% chance), particles of a size and composition similar to type la PSCs must be considered a possibility. Since these high-altitude tropical cirrus clouds may have significant implications for both ozone chemistry and radiative transfer, a closer examination of their composition and phase (using, for example, both in situ methods and depolarization lidar) together with simultaneous meteorological measurements are needed. [References: 26]
机译:来自激光雷达太空技术实验(LITE)的数据用于定位赤道对流层顶附近的云层并获取云层中的温度。该实验是在1994年9月9日至20日在发现号航天飞机上进行的。在赤道上进行的LITE观测经常显示出对流层顶附近的云层,在532 nm处的散射比高达2.5。这些云的特征是卷云和亚可见卷云。在对流层顶附近观测到云层,云层最高温度为185至200 K,LITE在5°N至15°S纬度带观测到的两个光学特性的统计平均值,由于气溶胶引起的消光的波长依赖性(埃斯特罗姆系数)计算散射比。埃系数表明,LITE在5°N至15°S纬度带中观测到的这些高空卷云中,有很大一部分(31%)与极地平流层云(PSC)拍潮有光学相似性。观察到的百分之六十六的云很薄,散射比在1.1到1.5之间。由于这些云最有可能在185 +/- 2.5 It(90%的机会)的温度下形成,因此必须考虑其大小和成分类似于Ia PSC型粒子的可能性。由于这些高空热带卷云可能会对臭氧化学和辐射转移产生重大影响,因此需要对它们的组成和相态进行更仔细的检查(例如,使用原位方法和去极化激光雷达),同时还要进行气象测量。 [参考:26]

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