检索规则说明:AND代表“并且”;OR代表“或者”;NOT代表“不包含”;(注意必须大写,运算符两边需空一格)
检 索 范 例 :范例一: (K=图书馆学 OR K=情报学) AND A=范并思 范例二:J=计算机应用与软件 AND (U=C++ OR U=Basic) NOT M=Visual
作 者:党张利 张京朋 曲宗希 赵慧[1] 张北斗[1] 张文煜[1]
机构地区:[1]兰州大学大气科学学院甘肃省干旱气候变化与减灾重点实验室,甘肃兰州730000
出 处:《干旱气象》2015年第2期340-343,共4页Journal of Arid Meteorology
基 金:国家杰出青年科学基金项目(41225018);国家自然科学基金(41305027)共同资助
摘 要:利用兰州大学半干旱气候与环境观测站2007~2010年夏季地基12通道微波辐射计观测数据,对半干旱区降水前和非降水过程的水汽含量和云液态水含量的变化特征进行分析。结果表明:(1)水汽含量达到2.20 cm可以作为半干旱区降水预报的阈值。水汽含量随时间变化比较平缓,变率约为0.06 cm/h,且降水前24 h内水汽含量均〉2.20 cm;或者水汽含量开始较小,但降水前水汽含量随时间出现拐点,之后变率开始增加,可达0.19 cm/h以上,进而使水汽含量〉2.20 cm。这2种情况均可预报可能有降水产生;(2)云液态水含量达到0.20 mm可以作为降水预报的阈值,且降水前云液态水含量随时间变化出现拐点,之后变率开始增加,可以预报1 h后可能有降水。Based on the observation data of TP/WVP - 3000 Microwave Radiometer from the Semi - Arid Climate Observatory and Laboratory of Lanzhou University, the characteristics of water vapor and cloud liquid water content before precipitation and during non - precipitation processes were analyzed in arid and semi -arid region in summer from 2001 to 2010. Results are as follows:( 1 ) The value of water vapor content reached 2.20 cm can be used as a threshold of precipitation forecast in semi - arid area. When the water va- por content is greater than 2.20 cm within 24 hours before the rainfall and its variability rate reaches 0.06 cm/h, or the water vapor content is small at the beginning, and then exceeds 2.20 cm with the increase of variability of the water vapor content to 0.19 cm/h be- fore the precipitation, which may be forecast precipitation in future. (2) The cloud liquid water content with 0.20 mm can be used as a threshold of precipitation forecast, and when it appears a turning- point before precipitation with time, subsequently the variability rate increases, which can be used to forecast precipitation after one hour.
分 类 号:P457.6[天文地球—大气科学及气象学]
正在载入数据...
正在载入数据...
正在载入数据...
正在载入数据...
正在载入数据...
正在载入数据...
正在载入数据...
正在链接到云南高校图书馆文献保障联盟下载...
云南高校图书馆联盟文献共享服务平台 版权所有©
您的IP:216.73.216.3