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951.
对2014年11月20日—12月31日中国气象局大气探测综合试验基地Ka波段毫米波云雷达、Vaisala CL51激光云高仪、L波段高空探测系统观测的云底高度进行对比分析。结果表明:在低能见度条件下,毫米波云雷达对云的探测能力明显优于激光云高仪,随着能见度的增加,两设备云探测能力差距在减小;毫米波云雷达与激光云高仪同时观测到有云时,二者观测的云底高度相关系数为0.92;毫米波云雷达与探空观测云底、云顶高度的相关系数分别为0.93和0.78;云雷达观测的云底高度均略低于激光云高仪和探空,云雷达观测的云顶高度略高于探空。 相似文献
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Mucins are important components of mucus,which form a natural,physical,biochemical and semipermeable mucosal layer on the epidermis of fish gills,skin,and the gastrointestinal tract. As the first step towards characterizing the function of Muc2,we cloned a partial Megalobrama amblycephala Muc2 cDNA of 2 175 bp,and analyzed its tissue-specific expression pattern by quantitative real-time PCR(qPCR). The obtained sequence comprised 41 bp 5′-untranslated region(5′-UTR),2 134 bp open reading frame encoding a protein of 711 amino acids. BLAST searching and phylogenetic analysis showed that the predicted protein contained several common secreted mucin-module domains(VWD-C8-TIL-VWD-C8) and had high homology with mucins from other vertebrates. Among four candidate reference genes(β- Actin,RPI13α,RPII,18S) for the qPCR,R PII was chosen as an appropriate reference gene because of its lowest variation in different tissues. M. amblycephala Muc2 was mainly expressed in the intestine,in the order(highest to lowest) middle-intestine fore-intestine hind-intestine. Muc2 was expressed relatively poorly in other organs(brain,liver,kidney,spleen,skin and gill). Furthermore,after 20-days of starvation,M. amblycephala Muc2 expressions after refeeding for 0h,3 h,16 h,3 d,and 10 d were significantly decreased in the three intestinal segments(P 0.05) at 16 h,and were then upregulated to near the initial level at 10 d. 相似文献
954.
An improved wind retrieval algorithm for the HY-2A scatterometer 总被引:2,自引:0,他引:2
955.
We studied the sedimentary characteristics of a Paleocene-Eocene salt lake in the Jiangling Depression through field core observation,thin section identification,scanning electron microscopy,and X-ray diffraction analysis.On the basis of sedimentary characteristics we have summarized the petrological and mineralogical characteristics of the salt lake and proposed 9 types of grade IV salt rhythms.The deposition shows a desalting to salting order of halite-argillaceous-mudstone-mud dolostonemud anhydrock-glauberite-halite.The relationship among grade IV rhythms,water salinity and climate fluctuations was analyzed.Based on the analysis of the relationship between boron content and mudstone color and by combining the mineralogy and sedimentary environment characteristics,we propose that the early and late Paleocene Shashi Formation in the Jiangling Depression was a paleolacustrine depositional environment with a high salt content,which is a representation of the shallow water salt lake depositional model.The middle Paleocene Shashi Formation and the early Eocene Xingouzui Formation were salt and brackish sedimentary environments with low salt content in a deep paleolake,which represents a deep salt lake depositional model. 相似文献
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957.
活动断裂地震危险性的研究现状和展望 总被引:4,自引:2,他引:2
本文综述了活动断裂地震危险性研究的历史、发展现状、存在的问题及发展方向。在活动断裂地震危险性研究中,重点论述了在概率分析研究阶段地震复发模式、概率模型、断裂间相互作用以及最大震级的评估等问题,指出未来活动断裂地震危险性分析研究的主要发展方向是多学科资料和研究手段、动力环境分析和力学模型的引入。 相似文献
958.
Fission Track Geochronology of Xiaonanchuan Pluton and the Morphotectonic Evolution of Eastern Kunlun since Late Miocene 总被引:1,自引:0,他引:1
Apatite fission track (AFT) thermochronology of seven samples from the Xiaonanchuan (小南川) pluton in the Kunlun (昆仑) pass area was carried out, for the purpose of determining the timing of cooling and the relation between the exhumation and the morphotectonic processes. The AFT ages yield low denudation rates of 0. 020--0. 035 mm/a during the late Miocene, which correspond to a stable geomorphic and weak tectonic uplifting environment. The low denudation rates can be considered as the approximate tectonic uplifting rates. The AFT geochronology shows puroxysmully rapid cooling since the Pliocene and an apparent material unroofing of more than 3 km in the Xiaonanchuan area. This was not the result of simple denudation. The rapid cooling was coupled with the intensive orogeny since the Pliocene, which was driven by tectonic uplifting. The accelerated relief building was accompanied by a series of faulting, which caused the basin and the valley formation and sinking. The space pattern of the AFT ages also shows differential uplifting, which decreases northwardly. This trend is supported by the regional AFT data, which indicate that the exhumation decreases northwardly in eastern Kunlun. This trend also exists in cast-west orientation from the western Kunlun range to the eastern. The uplif- ting trend is also supported by gcomorphic characteristics including the elevation and the relief differences well as the distribution of the Late Cenozoic volcanism. 相似文献
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960.