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青海中北部边界层高度与不同灾害天气的关系 被引量:11
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作者 马元仓 李岩瑛 +3 位作者 杨吉萍 曾婷 张爱萍 张春燕 《高原气象》 CSCD 北大核心 2019年第5期1048-1057,共10页
利用2013-2017年逐日07:00(北京时,下同)高空压温湿常规资料,19:00每隔50 m高空气温、气压、湿度和风速等加密资料,分别采用T-logP法和5点平滑位温梯度法计算了青海省茫崖、格尔木、都兰和西宁4个高空站的边界层高度,结合地面2006-2017... 利用2013-2017年逐日07:00(北京时,下同)高空压温湿常规资料,19:00每隔50 m高空气温、气压、湿度和风速等加密资料,分别采用T-logP法和5点平滑位温梯度法计算了青海省茫崖、格尔木、都兰和西宁4个高空站的边界层高度,结合地面2006-2017年逐时、日资料,进一步分析其影响因子及其与灾害性天气的关系。结果表明:在研究区边界层高度西北高于东南,春季35月较高,4月茫崖最高达4500 m以上;边界层高度主要与最大地气温差、极大风速、气温日较差和降水有关,高原上地气温差越大、风速越大,湿度越小,边界层高度越高。浮尘边界层高度3月较高,为3578 m;其他风沙边界层高度均为4月较高,达3800~4000 m。沙尘暴持续时间越长,边界层高度越高;高原沙尘暴主要集中在下午到夜间,46月较高,夜间45月为3100~4200 m。降水对边界层高度有很大影响,随着降雨强度增强,边界层高度也随之降低,发生小、中、大雨时的边界层高度分别为3354,1855和1300 m;相应的边界层气压分别在480~640,590~720和650~710 hPa。高温边界层高度6月最高达5210 m,78月达3600 m以上;而雷暴边界层高度4月较高,达5050 m,56月在2100 m左右,79月降低至1100 m左右。由于510月95%以上雷暴伴有降水,因而雷暴边界层高度较低。 展开更多
关键词 青海中北部 边界层高度 大风沙尘暴 降水 高温和雷暴
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The influence of plant root system architectural properties upon the stability of loess hillslopes,Northeast Qinghai,China 被引量:22
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作者 FU Jiang-tao HU Xia-song +5 位作者 BRIERLEY Gary QIAO Na YU Qin-qin LU Hai-jing LI Guo-rong ZHU Hai-li 《Journal of Mountain Science》 SCIE CSCD 2016年第5期785-801,共17页
To investigate the influence of root system architectural properties of three indigenous (cold- adapted) shrubs on the hillslope stability of loess deposits in the Xining Basin, northeast part of Qinghai-Tibet Plate... To investigate the influence of root system architectural properties of three indigenous (cold- adapted) shrubs on the hillslope stability of loess deposits in the Xining Basin, northeast part of Qinghai-Tibet Plateau (QTP), indoor direct shear tests have been conducted on the remolded rooted soil of three shrubs. Test results show that root system architectural indices (root area ratio (RAR), root length density (RLD) and root density (RD)) of the shrubs decline with depth and the relationship between RAR, RD and depth is exponential, while a power relationship describes the relationship between RLD and depth. The cohesion force of remolded rooted soil for the shrubs initially increases with depth, but it then demonstrates a slightly decreasing trend, which can be described with a power relationship. Power relationships also describe relationships between cohesion force and RAR, RLD and RD for the shrubs. As the growth period increases from lO to 17 months, the incremental increase in RAR is 48.32% ~ 21o.25% for Caragana korshinskii Kom and 0.56% ~ 166.85% for ZygophyUum xanthoxylon (Bunge) Maxim. This proportional increase is notably larger than that for RLD and RD. The increment in RAR is marginally greater for C. korshinskff than it is for Z. xanthoxylon. Correspondingly, the cohesion force incremental rates of remolded rooted soil for C. korshinskii and Z. xanthoxylon are 12.41% ~ 25.22% and 3.45% ~ 17.33% respectively. Meanwhile, as root content increases, the contribution by roots to cohesion force increases markedly until a threshold condition is reached. 展开更多
关键词 Cold region Semiarid region Soil reinforcement Hillslope stability Root system architectural indices Plateau
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