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排序方式: 共有491条查询结果,搜索用时 15 毫秒
91.
92.
李洁园 《测绘与空间地理信息》2011,34(1):192-194,201
以广州增城市为例,介绍了应用第二次土地调查成果联合开展农村宅基地权属调查及规范农民建房摸底调查的一种全新工作方法,通过实践应用,得出联合调查这一新方法可以极大地加快工作进度,提高成果质量,节约政府财政成本,减少扰民. 相似文献
93.
土地作为一种不可再生资源,科学利用和有效管理土地资源对我国有着比较重要的意义.20世纪80年代,3S技术已经逐步地在土地管理工作中有了比较广泛的应用.特别是最近两年,经过二次土地调查之后,3S技术在建设用地前期勘测定界、土地资源动态监测、土地整理、土地规划、地籍测绘等工作中得到了更加广泛的应用.但也应当看到,3S技术在... 相似文献
94.
Relation of the Second Type Thermal Helicity to Precipitation of Landfalling Typhoons: A Case Study of Typhoon Talim 下载免费PDF全文
This study utilized the MM5 mesoscale model to simulate the landfalling process of Typhoon Talim. The simulated typhoon track,
weather patterns, and rainfall process are consistent with the observation. Using the simulation results, the relation of
the second type thermal helicity (H
2) to rainfall caused by the landfalling typhoon Talim was analyzed. The results show that H
2 could well indicate the heavy inland rainfall but it did not perform as well as the helicity in predicting rainfall during
the beginning stage of the typhoon landfall. In particular, H
2 was highly correlated with rainfall of Talim at 1-h lead time. For 1–5-h lead time, it also had a higher correlation with
rainfall than the helicity did, and thus showing a better potential in forecasting rainfall intensification. Further analyses
have shown that when Talim was in the beginning stage of landfall, 1) the 850–200-hPa vertical wind shear around the Talim
center was quite small (about 5 m s−1); 2) the highest rainfall was to the right of the Talim track and in the area with a 300-km radius around the Talim center,
exhibiting no obvious relation to low-level temperature advection, low-level air convergence, and upper-level divergence;
3) the low-level relative vorticity reflected the rainfall change quite well, which was the main reason why helicity had a
better performance than H
2 in this period. However, after Talim moved inland further, 1) it weakened gradually and was increasingly affected by the
northern trough; 2) the vertical wind shear was enhanced as well; 3) the left side of the down vertical wind shear lay in
the Lushan and Dabieshan mountain area, which could have contributed to triggering a secondary vertical circulation, helping
to produce the heavy rainfall over there; hence, H
2 showed a better capacity to reflect the rainfall change during this stage. 相似文献
95.
This study investigated the second indirect climatic effect of anthropogenic aerosols,including sulfate,organic carbon(OC) ,and black carbon(BC) ,over East Asia.The seasonal variation of the climatic response to the second indirect effect was also characterized.The simulation period for this study was 2006.Due to a decrease in autoconversion rate from cloud water to rain as a result of aerosols,the cloud liquid water path(LWP) ,and radiative flux(RF) at the top of the atmosphere(TOA) changed dramatically,increasing by 14.3 g m-2 and decreasing by-4.1 W m-2 in terms of domain and annual average.Both LWP and RF changed most in autumn. There were strong decreases in ground temperature in Southwest China,the middle reaches of the Yangtze River in spring and autumn,while maximum cooling of up to-1.5 K occurred in the Chongqing district.The regional and annual mean change in ground temperature reached-0.2 K over eastern China.In all seasons except summer,precipitation generally decreased in most areas north of the Yangtze River,whereas precipitation changed little in South China.Precipitation changed most in summer,with alternating bands of increasing(~40 mm) and decreasing(~40 mm) precipitation appearing in eastern China.Precipitation decreased by 1.5-40 mm over large areas of Northeast China and the Huabei Plain.The domain and annual mean change in precipitation was approximately-0.3 mm over eastern China.The maximum reduction in precipitation occurred in summer,with mean absolute and relative changes of-1.2 mm and-3.8%over eastern China.This study revealed considerable climate responses to the second indirect effect of aerosols over specific regions of China. 相似文献
96.
莺歌海盆地莺歌海组二段泥岩盖层封闭性综合评价 总被引:2,自引:0,他引:2
通过实测莺歌海盆地莺歌海组二段泥岩盖层的排替压力,建立了盖层排替压力与声波时差的线性关系,进而提出了利用声波时差及地震速度资料求取排替压力的方法.接着,利用测井声波时差和地震速度资料,按等效深度法确定莺歌海组二段下部泥岩盖层的超压分布.综合考虑盖层累计厚度、排替压力、剩余压力、气藏内部压力、断裂对盖层破坏程度和天然气本... 相似文献
97.
利用淮南市朱集东矿井新生界松散层供水水文地质勘探成果和抽水试验资料,查明了区内新生界松散层供水含水层的供水水文地质条件,认为第一含水层埋藏浅,易受污染,水量随季节变化大,不宜作为生活饮用水供水水源,第三含水层水质较差,亦不作为生活饮用水供水水源,确定了第二含水层为矿区主要供水层位。采用解析法对第二含水层的水量进行了计算,并设计了布井方案,计算了井群水量;水位预报结果表明,开采50a后,3#、4#井中的水位最大降深为35.229m,小于其顶板埋深,说明拟建井群布置是合适的。评价结果为矿井供水设计提供了依据。 相似文献
98.
渤海海域沙一、二时期湖相碳酸盐岩分布广泛。根据其沉积特征可划分为台地型、斜坡型、水下隆起型和混合沉积型4大类及相应的亚相、微相,其中位于湖平面之下浪基面之上的各类浅水湖泊碎屑滩(生物滩、陆屑滩)储层最为发育。该时期渤海海域为温暖潮湿的北亚热带气候、封闭的微咸水-半咸水的环境。古地貌特征为影响碳酸盐岩发育和富集分布规律的主控因素,周边陆源碎屑供给能力则影响碳酸盐岩的发育程度。 相似文献
99.
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