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作 者:梁谷[1] 雷恒池[2] 李燕[1] 岳治国[1] 张晓庆[2] 高蓓[3]
机构地区:[1]陕西省人工影响天气中心,陕西西安710015 [2]中国科学院大气物理研究所,北京100029 [3]陕西省农业遥感信息中心,陕西西安710015
出 处:《高原气象》2007年第5期1105-1111,共7页Plateau Meteorology
基 金:国家科技部"西部开发科技行动"重点攻关计划(2001BA901A41)"黄河中游(陕甘宁)干旱与半干旱地区高效人工增雨(雪)技术开发与示范"课题资助
摘 要:通过对2003年4月18日在延安地区用单波长(0.95 cm)机载微波辐射计探测到的层状云云中液态水含量的分析,结果表明,层状云中的过冷水平均含量为0.0171 g.m-3。分析其变化,发现云中垂直向的液态水存在高值区,这一区有助于人工引晶催化增雨(雪)作业,有利于冰晶的增长,可提高人工催化作业的效果。与机载粒子测量系统(PMS)及地面711数字化雷达的探测结果进行比对,机载微波辐射计和PMS粒子测量系统的探测结果有较好的一致性;并且在垂直区域的探测上比PMS粒子测量系统更具有代表性;与711数字化雷达的探测结果也吻合。Using a single wavelength(0.95 cm) column cloud liquid water content by Airborne Upward-looking Microwave Radiometer measures the Cloud Liquid Water Content in stratiform clouds(CCLWC) in Yan′an area on April 18,2003.The analyzed results show that the average supper-cooled cloud liquid water content(SCCLWC) is 0.0171 g·m^-2.It was found that it had a high value range on the vertically CLW by analyzing the CLWC had changed in stratiform cloud.Which range was contribute to the operations of precipitation-enhancement,be good for enhancing ice crystal′s,improving effective on operations of catalyze.The Airborne Upward-looking Microware Radiometer is compared to the PMS radar and the 711 numerical radiometer on the ground surface,and its results are shown that the Airborne Upward-looking Microware Radiometer and PMS radar have the same measured;and that the Airborne Upward-looking Microware Radiometer is more topical of the PMS radar by measuring of the vertically range,and testimony tallies with the results of the 711 numerical radiometer on the ground surface.
分 类 号:P481[天文地球—大气科学及气象学]
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