Establishing the skill of climate field reconstruction techniques for precipitation with pseudoproxy experiments     

Gómez-Navarro  Juan José  Werner  Johannes  Wagner  Sebastian  Luterbacher  Jürg  Zorita  Eduardo 《Climate Dynamics》2015,45(5-6):1395-1413

Climate Dynamics - This study aims at assessing the skill of several climate field reconstruction techniques (CFR) to reconstruct past precipitation over continental Europe and the Mediterranean at...  相似文献   

一次龙卷生成中风暴单体合并和涡旋特征的雷达观测研究   总被引：4，自引：0，他引：4  

朱江山  刘娟  边智  符长静 《气象》2015,41(2):182-191

本文利用阜阳市多普勒天气雷达CINRAD/SA资料,分析了2008年7月23日发生在安徽省颍上县的龙卷天气过程。结果表明：本次过程中,风暴单体的连续合并对风暴单体迅速增强为超级单体风暴有重要作用。风暴单体的合并和邻近风暴单体之间的相互作用与龙卷的发生在时间和位置上有较明显的相关,说明风暴单体间的合并和相互作用可能对龙卷存在激发作用,这对龙卷预警具有一定的参考价值。在缺省适配参数条件下,雷达系统CINRAD/SA的中气旋(M)产品和龙卷涡旋特征(TVS)产品对龙卷预警有较好的指示作用。如果风暴被同时识别出M和TVS产品,并观测到风暴单体中存在有界弱回波区,则出现龙卷的几率更高。  相似文献   

新北油田北部馆陶组上段沉积演化          下载免费PDF全文

邹娟  戴俊生  冀国盛  吉文辉  田博 《沉积与特提斯地质》2015,(2):16-21

新北油田北部凹陷众多,成藏条件比较复杂,尤其是馆陶组上段。通过对岩心录井、测井曲线特征等分析,结合前人研究,对新北油田北部馆陶组上段沉积地层进行了重新划分,将前3个砂层组划分为12个小层,研究其地层发育特征。并以单井沉积相分析为基础,对新北油田北部馆陶组上段沉积相进行重新分析,认为该段为三角洲平原亚相,物源来自北东方向,主要发育分流河道、分流间湾、天然堤、决口扇等微相。在馆陶组上段沉积时期,沉积环境整体较稳定,沉积相展布变化不大,仅第二砂层组沉积时期,水体相对较动荡,砂体量、分流河道走向多变。  相似文献   

黑河流域近两千年人—水—生态演变研究进展   总被引：2，自引：0，他引：2  

陆志翔  肖洪浪  Wei Yongping  邹松兵  任娟  张志强 《地球科学进展》2015,30(3):396-406

理解流域历史时期的人—水—生态演变过程和规律,对其当前和未来的管理规划极为重要。通过梳理近几十年来有关学者对西北干旱区典型内陆河流域——黑河流域过去2 000年的水环境、人类活动、生态环境演变及其耦合研究等方面的成果,发现单个方面的研究均已较为普遍和成熟,并且积累了大量的素材和数据,但是缺乏以流域为单元,从长时间尺度综合考虑人—水—生态相互作用,定量分析人—水—生态协同演化过程的研究成果。今后的研究,一是应当着重于数据挖掘方法的探索,对已有成果进一步挖掘并进行对比和校正,构建一套长时间序列的可靠的人类活动、水文和生态数据集;二是应当着重于动力学模型的构建,增加生态—水文系统与人类活动的互馈机制描述,刻画人—水—生态的协同演化过程,从而达到通过揭示流域过去2 000年的人—水—生态协同演化过程,为流域当前和未来的管理提供历史镜鉴,为国内外的其他类似流域提供参考。社会水文学的提出无疑将极大地促进流域人—水—生态演变研究的发展。  相似文献   

博茨瓦纳三级成矿区带划分          下载免费PDF全文

修群业  刘晋  韩军  范光  李娟 《地质找矿论丛》2015,30(S1):60-65

博茨瓦纳以盛产金刚石闻名于世,但其基础地质和矿产地质研究的程度并不高。文章依据地质构造单元、主要矿种和主要成矿类型的成矿单元划分原则,将博茨瓦纳划分为太古宙津巴布韦克拉通铜-镍-钴-金多金属成矿带、太古宙卡普瓦尔克拉通铁-锰-金多金属成矿带、古元古代林波波铜-镍成矿带、太古宙刚果克拉通(铜)成矿带、新元古代达马拉铜-锡成矿区、卡拉哈里盆地煤-金刚石-铀成矿区等6个Ⅲ级成矿区带,并对这些成矿区带的主要特征进行了阐述。  相似文献   

Changes in the storage and sink of carbon dioxide in subsurface atmospheres controlled by climate-driven processes: the case of the Ojo Guareña karst system     

Angel Fernandez-Cortes  Soledad Cuezva  Elena Garcia-Anton  Miriam Alvarez-Gallego  Concepcion Pla  David Benavente  Juan Carlos Cañaveras  Jose Maria Calaforra  David Paterson Mattey  Sergio Sanchez-Moral 《Environmental Earth Sciences》2015,74(12):7715-7730

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北冰洋叶绿素a及初级生产力遥感反演研究进展     

庞小平  胡晓坤  季青  李娟  张晨雷  梁泽毓  陈亦卓 《极地研究》2022,34(1):1-10

海洋表层叶绿素a浓度和浮游植物初级生产力是海洋生态系统的基础参数,可有效评估海洋生态系统的初级生物量及其变化.阐明北冰洋浮游植物生物量和初级生产力的时空变化,对预测北极环境快速变化背景下的海洋生态系统潜在变化、科学指导北冰洋的生态管理具有重要意义.本文总结了基于卫星数据的海表叶绿素a浓度和初级生产力的研究方法,整理归纳...  相似文献   

The influence of mountainous relief on the vertical gradient of precipitation and pluvial zoning in the central slope of the Gulf of Mexico     

Victor Soto  Juan Cervantes 《Singapore journal of tropical geography》2023,44(1):112-129

Although variation of air temperature with respect to terrain altitude is widely understood, less is known about the altitudinal behaviour of precipitation. The eastern slope of Mexico is the most contrasting physiographic province of the country due to its relief. This area is also one of the most important regions of Mexico and of the intertropical region of America because of its biodiversity. Due to the vital and ecosystemic value of precipitation, this work seeks to analyse the altitudinal distribution of precipitation as a function of the relief. Our main methodology consisted of analysing the climatological normal of 86 weather stations to determine accumulated precipitation during rainy, dry and annual periods. Precipitation was correlated with the altitude of the relief, which allowed the study area to be divided into groups relative to the degree of accumulated rainfall throughout the year, as well as by the gradient of variation according to the elevation of the terrain. The results indicated that during the year, precipitation was favoured by the humidity of the Gulf of Mexico and decreased at a rate of -3.7 mm/m in coastal areas. Subsequently, precipitation increased with the altitude of the relief at a rate of 0.7 mm/m, between ~700 and ~ 1500 masl, which is where the greatest accumulation of rainfall was concentrated. Thereafter, it decreased by -0.9 mm/m until it reached the highest volcanic watershed. Crossing this watershed, the foehn effect caused rainfall rates to be much lower than on the windward slope, where the central plateau of the country begins.  相似文献   

A possible 5 km wide impact structure with associated 22 km wide exterior collapse terrain in the Alhabia–Tabernas Basin,southeastern Spain     

Sebastián Tomás Sánchez Gómez  Jens Ormö  Carl Alwmark  Sanna Holm-Alwmark  Gabriel Zachén  Robert Lilljequist  Juan Antonio Sánchez Garrido 《Meteoritics & planetary science》2023,58(10):1512-1539

The Tabernas–Alhabia Basin is a structural depression situated in the province of Almería, southeastern Spain. The basin is filled with Neogene, Pliocene, and Pleistocene sediments resting discordantly on a Paleozoic metamorphic basement. During the marine Tortonian sedimentation, a bed of breccia (Gordo megabed) was formed. It consists of rotated sedimentary megablocks commonly capped and/or surrounded by a polymict breccia composed mainly of up to dm-sized clasts of the crystalline (schist) basement. Previous work has suggested the bed to be a seismite corresponding to events induced by earthquakes. Here, we link the formation of the Gordo megabed with an ∼5 km wide, rimmed depression with exposed breccias on the northern flank of the Sierra de Gádor mountain. This semicircular structure, developed in mainly schists and dolostone of the basement, is delimited to the W, S, and E by an up to 350 m high escarpment with overturned stratigraphy. Toward the north, this crater-like structure opens toward the Gordo megabed of the Tabernas Basin. In the southern sector, the overturned strata transform outward for into a blocky allochthonous breccia with decreasing thickness and clast size. In the interior of the structure, there are occurrences of graded breccia and arenite superposed on a blocky, autochthonous breccia. Based on the presence of mineralogical shock metamorphic evidence, potential shatter cones, and a high Ir anomaly (∼500 ppb) as well as the position of the structure near the town of Alhama de Almería, we propose to call it the Alhama de Almería impact structure.  相似文献   

Terrain data compression using wavelet-tiled pyramids for online 3D terrain visualization     

Ricardo Olanda  Mariano Pérez  Juan Manuel Orduña  Silvia Rueda 《International journal of geographical information science》2014,28(2):407-425

Last years have witnessed the widespread use of online terrain visualization applications. However, the significant improvements achieved in sensing technologies have allowed an increasing size of the terrain databases. These increasing sizes represent a serious drawback when terrain data must be transmitted and rendered at interactive rates. In this paper, we propose a novel wavelet-tiled pyramid for compressing terrain data that replaces the traditional multiresolution pyramid usually used in wavelet compression schemes. The new wavelet-tiled pyramid modifies the wavelet analysis and synthesis processes, allowing an efficient transmission and reconstruction of terrain data in those applications based on multiresolution tiled pyramids. A comparative performance evaluation with the currently existing techniques shows that the proposed scheme obtains a better compression ratio of the terrain data, reducing the storage space and transmission bandwidth required, and achieving a better visual quality of the virtual terrain reconstructed after data decompression.  相似文献