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101.
A 2000-yr reconstruction of air temperature in the Great Basin of the United States with specific reference to the Medieval Climatic Anomaly 总被引:1,自引:0,他引:1
Scott A. Reinemann David F. Porinchu Glen M. MacDonald Bryan G. Mark James Q. DeGrand 《Quaternary Research》2014
A sediment core representing the past two millennia was recovered from Stella Lake in the Snake Range of the central Great Basin in Nevada. The core was analyzed for sub-fossil chironomids and sediment organic content. A quantitative reconstruction of mean July air temperature (MJAT) was developed using a regional training set and a chironomid-based WA-PLS inference model (r2jack = 0.55, RMSEP = 0.9°C). The chironomid-based MJAT reconstruction suggests that the interval between AD 900 and AD 1300, corresponding to the Medieval Climate Anomaly (MCA), was characterized by MJAT elevated 1.0°C above the subsequent Little Ice Age (LIA), but likely not as warm as recent conditions. Comparison of the Stella Lake temperature reconstruction to previously published paleoclimate records from this region indicates that the temperature fluctuations inferred to have occurred at Stella Lake between AD 900 and AD 1300 correspond to regional records documenting hydroclimate variability during the MCA interval. The Stella Lake record provides evidence that elevated summer temperature contributed to the increased aridity that characterized the western United States during the MCA. 相似文献
102.
Comprehensive Development and Utilization of Saline Lake Groups in Dingbian,Shanxi Province of China
正The Dingbian Saline Lake groups are in Dingbian County,northwest of Shaanxi province,and located on the border area of the Loess Plateau and Maowusu Desert in Northern Shanxi.It's altitude is more than 1300m.The 相似文献
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在中央提出推进新型城镇化和实施农村土地制度改革试点的新形势下,如何适应客观实际、率先探索出大都市郊区土地综合改革新路并为全国其他地区改革提供参考借鉴,具有十分重要的现实意义。本文以上海市浦东新区为例,深入分析梳理大都市郊区农村土地开发利用和改革创新所面临的问题与主要瓶颈,在此基础上就如何深化农村土地制度综合改革的总体思路和具体措施提出有针对性和可操作性的对策建议。 相似文献
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空间异质性定量研究方法 总被引:8,自引:2,他引:6
岳天祥 《地球信息科学学报》1999,1(2):75-79
空间异质性是景观生态学定量化研究的核心,其定量研究方法包括景观综合图、数学模型和地学信息图谱.本文概括总结了景观综合图的内容和定量化指标,分析了这种定量化方法的优势和局限;对数学模型的复杂性、优点和与景观综合图的互补性作了简要分析,指出了数学模型研究需要进一步探讨和重视的问题;通过对地学信息图谱三个阶段(景观制图实验,图谱概念的提出和地学信息图谱理论的形成)的回顾和对其特点的分析,我们认为地学信息图谱综合了景观综合图和抽象的数学模型可以提供的互补信息,吸收了两者的优点,是空间异质性的综合定量研究方法. 相似文献
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基于高光谱遥感数据,通过RST算法提取2020年7月12日唐山5.1级地震前不同参数异常信息,发现震前CH4、CO、H2O、O3均出现了高值异常,且异常均位于震中附近,异常幅度高于2倍均方差,CH4、CO、H2O异常机理不同于O3。通过统计2018—2020年CH4、CO、H2O三种气体出现频次,发现同步异常具有可靠性,认为高光谱多参数异常出现的同步性,可提高异常性质判定的信度。通过对不同参数进行连续跟踪观测,提取多参数同步异常信息,对地震短临预报具有一定参考意义。 相似文献
110.
Although there has been significant progress in the seismic imaging of mantle heterogeneity,the outstanding issue that remains to be resolved is the unknown distribution of mantle temperature anomalies in the distant geological past that give rise to the present-day anomalies inferred by global tomography models.To address this question,we present 3-D convection models in compressible and self-gravitating mantle initialised by different hypothetical temperature patterns.A notable feature of our forward convection modelling is the use of self-consistent coupling of the motion of surface tectonic plates to the underlying mantle flow,without imposing prescribed surface velocities(i.e.,plate-like boundary condition).As an approximation for the surface mechanical conditions before plate tectonics began to operate we employ the no-slip(rigid) boundary condition.A rigid boundary condition demonstrates that the initial thermally-dominated structure is preserved,and its geographical location is fixed during the evolution of mantle flow.Considering the impact of different assumed surface boundary conditions(rigid and plate-like) on the evolution of thermal heterogeneity in the mantle we suggest that the intrinsic buoyancy of seven superplumes is most-likely resolved in the tomographic images of present-day mantle thermal structure.Our convection simulations with a plate-like boundary condition reveal that the evolution of an initial cold anomaly beneath the Java-Indonesian trench system yields a long-term,stable pattern of thermal heterogeneity in the lowermost mantle that resembles the presentday Large Low Shear Velocity Provinces(LLSVPs),especially below the Pacific.The evolution of subduction zones may be,however,influenced by the mantle-wide flow driven by deeply-rooted and longlived superplumes since Archean times.These convection models also detect the intrinsic buoyancy of the Perm Anomaly that has been identified as a unique slow feature distinct from the two principal LLSVPs.We find there is no need for dense chemical ’piles’ in the lower mantle to generate a stable distribution of temperature anomalies that are correlated to the LLSVPs and the Perm Anomaly.Our tomography-based convection simulations also demonstrate that intraplate volcanism in the south-east Pacific may be interpreted in terms of shallow small-scale convection triggered by a superplume beneath the East Pacific Rise. 相似文献