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91.
Traditional rural homegarden agroforestry systems in the Chengdu Plain of China are often referred to as “Linpan” in Chinese, which integrates the landscape of ecological functions and human production activities. In recent years, due to the influences of urbanization and the aging population, the Linpan landscape has changed dramatically. Clarifying the factors which influence Linpan landscape evolution is a critical way to improve rural landscape renovation. Through oral history interviews, the deep-seated factors driving the evolution of the Linpan landscape form from 1949 to 2020 are explored using the grounded theory. The results show that in the process of Linpan landscape evolution, beneficiary groups, the material basis, and cultural characteristics are the prerequisites for changing the Linpan settlement landscape. The demand of production and life and government-led behavior are the two main influencing factors, and landscape change is the final result. The demand of production and life from the residents is the primary internal driving force of landscape change, while government-led behavior is the main external driving force of settlement development and evolution. The nature of the main driving forces behind the evolution of the Linpan landscape in the Chengdu Plain can be divided into three stages. (1) From 1949 to 1980, it was characterized as a balancing of government forces and social forces. (2) From 1981 to 1993, it was characterized by social forces suppressing government forces. (3) From 1994 to 2020, it was characterized as a stalemate between the government and social forces. From the perspective of the evolution of the Linpan settlement landscape, the traditional Linpan form and settlement layout have been unable to meet the new requirements of the rural social and economic transition period. They are facing the challenges of rural reconstruction and rural revitalization. In the future, village and town planning and the design of new settlements need to comprehensively consider the demands of different interest groups. 相似文献
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基于多尺度分析的思想,以离散小波变换为工具,利用小波对惯性元件输出的信息进行并行阈值消噪以削弱惯性元件误差对SINS及组合系统性能的影响;然后,对GPS输出的信息进行并行多尺度预处理,并结合传统的Kalman滤波方法,对系统进行综合滤波;将上述方法引入到GPS/SINS组合导航系统中,利用实测数据进行验证,并给出了基于不同方法的大量实验曲线。实验结果表明,该方法可以有效削弱惯性元件以及GPS误差对系统的影响,提高了GPS/SINS组合导航系的精度和可靠性。 相似文献
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风廓线雷达资料在台风苏拉登陆过程中的应用初探 总被引:2,自引:0,他引:2
为了研究风廓线雷达在台风天气过程预报中的作用,对2012年8月2—4日在福建秦屿镇登陆的台风苏拉天气过程统计分析,结果表明:风廓线雷达在台风苏拉登陆期间4 km以上高空有效数据获取率明显提高,确定风廓线雷达的有效探测高度为4.8 km;通过信噪比和垂直速度数据统计分析出台风登陆前后带来间歇性的降雨,而台风眼登陆主要表现为无降水天气,仅有少量的降雨,这一结论进一步在小时降雨量统计中得到验证;通过水平风速数据统计分析出台风登陆前后在有效探测高度内水平风速在25 m·s-1左右,而台风眼登陆水平风速在0~3 m·s-1; 统计结果与台风登陆物理过程相吻合。 相似文献
95.
Xueyuan Kuang Yaocun Zhang Ying Huang Danqing Huang 《Theoretical and Applied Climatology》2014,117(1-2):103-112
NCEP/NCAR reanalysis daily data from 1951 to 2008 are used in this study to reveal the spatial-asymmetric features in the seasonal variation of the upper-tropospheric jet stream (UTJS) and its thermal dynamic forcing mechanism. The jet occurrence percentage distribution of the UTJS demonstrates a spiral-like pattern in winter, but it is quasi-annular in summer. The jet occurrence percentage in the Eastern Hemisphere is larger than that in the Western Hemisphere, and its maximum area is located further south. The polar front jet stream (PJS) and subtropical jet stream (SJS) can be distinguished over the Northern Africa and Asian regions, whereas only one jet stream can be observed over the Western Pacific and Atlantic Ocean. Furthermore, a single peak pattern is found in the seasonal variation of the SJS occurrence frequency with the highest jet occurrence appearing in winter and the lowest in summer, while a double peak pattern is observed in the seasonal variation of the PJS occurrence, i.e., the jet occurrence reaches its peaks in autumn and spring for the PJS. Based on the thermal wind theory, air temperature gradient and atmospheric baroclinicity are calculated and compared with the jet occurrence variation to explore the thermal dynamic forcing mechanism for the UTJS variation. In addition, synoptic-scale transports of eddy heat and momentum are also calculated. The results indicate that the SJS variation is primarily determined by the air temperature gradient and atmospheric baroclinicity, while the PJS variation is under great influence of the transport of eddy heat and momentum over Northern Africa and East Asia. The UTJS variation over the area from 140E to 70W cannot be well individually explained by the air temperature gradient and atmospheric baroclinicity. Further analysis indicates that UTJS variation over this area is largely under control of combined effect of the transport of eddy heat and momentum as well as the atmospheric baroclinicity. 相似文献
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Yuning Hong Jinju Geng Song Qiao Lili Ding Xueyuan Gu Xiaorong Wang Dietmar Glindemann Hongqiang Ren 《Marine Chemistry》2010,118(1-2):67-74
Phosphine is a natural gaseous compound in the phosphorus biogeochemical cycle. This paper studies the spatial and temporal distributions of matrix-bound phosphine (MBP) and gaseous phosphine in the offshore area of the Southwest Yellow Sea, East Asia. The results show that MBP concentrations in marine surface sediments range from 0.69 ± 0.06 ng/kg (dry) to 179 ± 29 ng/kg (dry). Higher seasonal MBP concentrations in sediments are found in fall than in spring or winter in most sites. High MBP contents are observed in two fish-breeding areas. MBP concentrations decrease with distance to the coast, except in the southeast of the sampling area. MBP levels in marine sediments are found to be higher than those at several other places: freshwater sediments and soil, except eutrophic lakes. Gaseous phosphine contents in fall range from 0.14 ± 0.00 ng/m3 to 9.83 ± 0.97 ng/m3. No correlation is observed between MBP and gaseous phosphine. 相似文献
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西天山阿吾拉勒地区A型流纹斑岩的初步研究 总被引:1,自引:0,他引:1
新疆阿吾拉勒山是中亚造山带的重要组成部分。通过对区内火山岩的主量元素和微量元素地球化学研究,在群吉萨伊-塔尔得套一带下二叠统乌朗组中厘定出了一套铝质A型流纹斑岩。群吉萨伊和塔尔得套的流纹斑岩具有富硅(SiO2≥69.9%)和富碱(Na2O+K2O≥7.06%)的特征。其中,塔尔得套流纹斑岩的总碱含量低于群吉萨伊流纹斑岩,但其K2O含量则明显高于后者,属于高钾火山岩。二者均具有明显的Ba、Sr、Eu和Ti亏损,稀土总量在90.7×10-6~264×10-6之间。主量元素和微量元素特征显示,群吉萨伊和塔尔得套的A型流纹斑岩的源区均与硬质砂岩相似,属于A2型花岗岩,同时具有较高的锆饱和温度(TZr约900°C),其成因可能与后俯冲阶段的岩石圈拆沉过程有关。 相似文献