肇庆市"千里旅游走廊"开发的理论解释与策略研究   总被引：1，自引：1，他引：0  

肖光明 《热带地理》2004,24(4):381-386

运用点轴渐进式扩散理论、旅游地生命周期理论、阴影区理论对首批中国优秀旅游城市肇庆开发"千里旅游走廊"的行动进行了探讨,认为这是肇庆区域旅游发展的必然要求和有效手段,具有战略意义;分析了其旅游空间总体布局和旅游资源的主要特色,并提出若干开发策略.  相似文献   

河西走廊东部沙尘暴预报方法研究   总被引：18，自引：8，他引：10  

李岩瑛  李耀辉  罗晓玲  王汝忠  郭良才 《中国沙漠》2004,24(5):607-610

利用我国沙尘暴多发区, 甘肃省河西走廊东部民勤、凉州区等五站近50a的气象资料, 详细分析了河西东部沙尘暴频繁发生的气象因素, 应用近20a的天气资料, 结合近50a的典型个例做出沙尘暴的长期、中期、短期和短时预报预警系统。研究结果表明: 长期预报取决于冬春季气温、降水量和大风日数; 中期依靠使用国内外数值预报产品; 短期与大气环流条件、分型指标有关; 短时临近预报与高空大风形势、地面上游有无大风沙尘暴天气有关。  相似文献   

河西走廊地质历史中宋辽干冷期灾变事件及其影响          下载免费PDF全文

赫明林  曹兴山  曹炳媛 《甘肃地质》2006,15(1):10-18

宋辽寒冷干旱期的急剧降温,使河西地区降水量迅速减少,气候变得更为干旱。植被枯萎,风暴、沙暴、尘暴、火灾、旱灾、饥荒等灾害事件频繁发生,从而引发了一系列生态环境问题和战争动乱,对中国政治、社会、经济、文化产生重大影响。依据历史资料和考古研究成果及地质记录中“事件标志层”层位、年代,确定宋辽寒冷干旱期发生于公元1000~1050年,发展于公元1050~1100年,强盛于公元1100~1320年,消亡于公元1320~1335年。  相似文献   

河西走廊风速变化及风能资源研究   总被引：24，自引：9，他引：15  

王毅荣  张存杰 《高原气象》2006,25(6):1196-1202

利用河西走廊地区25年风速气候资料和风塔周年资料,研究了该区域近地面风速及风能的演变和分布。结果表明:河西走廊绿洲内风速下降十分明显,而其它高山站风速比较稳定,没有明显的减少趋势;风速变化具有周期振荡特点;垂直风速差由近地面向上减小,高层风速极大(小)值滞后于低层;风速随高度按自然对数规律增大,风能距地面8 m层内随高度变化迅速;该地区4~12 m/s风居多,是风能的主要贡献者;2~4月风速最大,1,5月最小;该地区风能丰富,10~70 m层内年风能储量在2200 khW/m2以上。  相似文献   

夏季通风气象指数预报     

赵娜  张德山  邓长菊  马小会  穆启占 《气象科技》2008,36(6):779-781

随着人们生活水平的提高,对室内污染越来越关注,应"中国室内环境监测委员会"提出的需求,通风气象指数于2006年6月首次向北京公众发布,文章就首先研发并投入业务使用的夏季通风指数给出了详细论述.通过对2005年夏季(6～8月)的各气象要素(气压、温、湿、风、能见度、天空状况等)资料共1790个数据做检验分析,最终选取体感温度为主要预报因子并综合考虑夏季特殊天气条件和风力以及污染的影响,得出夏季通风指数在一天中7个时段的预报公式,并划分出相应的指数等级.  相似文献   

隧道无轨运输独头掘进超9600 m施工通风技术          下载免费PDF全文

杨家松 《探矿工程》2008,35(10):66-70

锦屏电站辅助洞为A、B线的上下行单线隧道,线间距35 m,单线长175 km,由于隧道埋深大且无任何条件修建斜竖井做到长隧短打,只能从近东西向相向掘进,同时又由于工程的西端场地极其狭窄,不能满足有轨运输施工条件。通过技术论证,大胆创新,引入公路运营通风的理念,将射流通风运用于本工程的施工通风,从理论研究结合现场通风测试验证,成功地解决了巷道式射流风机选型、布置及通风管理等关键技术。通过双孔独头掘进9600 m的施工通风效果检测表明,洞内空气质量的各项指标均达到国家环卫标准,实现内燃作业、无轨运输,取得了  相似文献   

大陆岩石圈对扩张机制的响应——辽蒙地质走廊中—新生代火山活动的时空分布     

邵济安  ;季建清  ;路凤香  ;张履桥 《中国区域地质》2008,(9):1431-1440

选择以辽西为中心,近东西向延伸800km的辽蒙地质走廊为研究区,通过年代学研究,确认130Ma以来的中、新生代火山活动对称分布的时空格局具有“中间老、两侧新”的特点,而且随着时间的推移,软流圈来源的岩浆向东西两侧侧向流动,岩浆来源不断加深。在此基础上提出“软流圈底辟体上涌和水平侧向流动”的模式。  相似文献   

基于气象研究的城市通风廊道构建初探——以南京江北新区为例   总被引：1，自引：0，他引：1  

党冰  房小怡  吕红亮  程宸  杜吴鹏  刘勇洪  张硕  杨帆 《气象》2017,43(9):1130-1137

利用南京江北新区的气象观测数据、NCEP全球再分析资料和卫星遥感数据,采用统计分析、数值模拟以及地表温度反演技术,综合分析了江北新区的背景风场特征和城市热岛分布状况;并结合江北新区土地利用现状及未来规划资料,构建了其核心规划区域的通风廊道系统。结果表明:(1)江北新区主导风向为偏东风,局地存在山谷风和水陆风,风速主要集中在2~4 m·s~(-1)风速段,且近10年呈下降趋势;(2)在空间分布上,城镇、工业园区风速较小,同时是强热岛区域且有热岛连片发展趋势;长江、老山和林地等冷岛区风速较大,空气较为清新,可利用其与城镇进行空气交换;(3)结合当地气候条件、地形特征、用地类型及未来规划,以山体地势为脊骨,以顺势输引主导风向为基本,以沟通冷源和弱风区为目的,构建了东北—西南走向的1条主通风廊道和3条次通风廊道,以及东南—西北、东—西走向的8条局部通风廊道;并对通风廊道的走向、宽度、布局等提出控制指标和构建策略。  相似文献   

“A Place of Pain and Gain”: Exploring the Dynamics of Resistance in the Creation of Sengwe Tshipise Wilderness Corridor,Southeast Zimbabwe     

Chaka Chirozva  Rosemary Black  Vaughan Higgins 《社会与自然资源》2017,30(8):964-979

This article examines the relationship between place attachment and resistance during participatory planning of the Sengwe Tshipise Wilderness Corridor, located in southeast Zimbabwe, a region that falls within the Great Limpopo Transfrontier Conservation Area. Field research was conducted from July to December 2013 using 69 semistructured interviews, seven focus-group discussions, and analysis of secondary data. By following the dominant narratives articulated by villagers affected by this Corridor, we illustrate the multiple ways in which place attachment becomes part of everyday politics of resistance. Results show that a strong place-based identity is at the center of narratives deployed by villagers displaced by war, conservation, and veterinary fencing restrictions. Through deploying this place-based identity, communities collectively influenced both the spatial extent of the corridor and institutional governance arrangements. This article contributes to debates on the role of community agency in the implementation of transfrontier conservation areas.  相似文献   

Tidal Mixing in the Kuril Straits and Its Impact on Ventilation in the North Pacific Ocean     

Tomohiro Nakamura  Takahiro Toyoda  Yoichi Ishikawa  Toshiyuki Awaji 《Journal of Oceanography》2004,60(2):411-423

A numerical study using a 3-D nonhydrostatic model has been applied to baroclinic processes generated by the K ₁ tidal flow in and around the Kuril Straits. The result shows that large-amplitude unsteady lee waves are generated and cause intense diapycnal mixing all along the Kuril Island Chain to levels of a maximum diapycnal diffusivity exceeding 10³ cm²s⁻¹. Significant water transformation by the vigorous mixing in shallow regions produces the distinct density and potential vorticity (PV) fronts along the Island Chain. The pinched-off eddies that arise and move away from the fronts have the ability to transport a large amount of mixed water (∼14 Sv) to the offshore regions, roughly half being directed to the North Pacific. These features are consistent with recent satellite imagery and in-situ observations, suggesting that diapycnal mixing within the vicinity of the Kuril Islands has a greater impact than was previously supposed on the Okhotsk Sea and the North Pacific. To examine this influence of tidal processes at the Kurils on circulations in the neighboring two basins, another numerical experiment was conducted using an ocean general circulation model with inclusion of tidal mixing along the islands, which gives a better representation of the Okhotsk Sea Mode Water than in the case without the tidal mixing. This is mainly attributed to the added effect of a significant upward salt flux into the surface layer due to tidal mixing in the Kuril Straits, which is subsequently transported to the interior region of the Okhotsk Sea. With a saline flux into the surface layer, cooling in winter in the northern part of the Okhotsk Sea can produce heavier water and thus enhance subduction, which is capable of reproducing a realistic Okhotsk Sea Mode Water. The associated low PV flux from the Kuril Straits to the open North Pacific excites the 2nd baroclinic-mode Kelvin and Rossby waves in addition to the 1st mode. Interestingly, the meridional overturning in the North Pacific is strengthened as a result of the dynamical adjustment caused by these waves, leading to a more realistic reproduction of the North Pacific Intermediate Water (NPIW) than in the case without tidal mixing. Accordingly, the joint effect of tidally-induced transport and transformation dominating in the Kuril Straits and subsequent eddy-transport is considered to play an important role in the ventilation of both the Okhotsk Sea and the North Pacific Ocean. This revised version was published online in July 2006 with corrections to the Cover Date.  相似文献