你管政府增加农民负担吗?兴化周庄镇大桥路68号政府正收老百姓每户600-2000不等的吃水费。请做主

Abstract&In order to further understanding long-term variation of low-level wind field over the mountains region of the Qinghai-Xizang Plateau,based on the observational data of boundary layer tower and wind profile radar in Dali region of the southeastern margin of the Qinghai-Xizang Plateau from 2008 to 2012,the vertical structure and variation characteristics of wind field were analyzed.The results show as follow:Firstly,wind speed and wind direction frequency in the low-level atmosphere varied with height.Wind force scale was 2 level and prevailing winds were east winds between 2 m and 400 m height.It indicated that wind speed and wind direction measured with boundary layer tower and wind profile radar was continuous.Secondly,vertical wind speed changed with season,which its value was greater in winter than that in summer.The diurnal variations of wind speed at different height were different,that is to say,the diurnal variations of wind speed displayed one peak below 20 m and two speaks between 100 m and 1500 m height,and were not evident above 2000 m height.The monthly variations of wind speed showed one speak below 20 m and above 1500 m height,and showed two speaks between 100 m and 1000 m height.Finally,the zonal winds below 600 m height appeared a daily cycle of east wind and west wind.The meridional winds were south winds all the day between 2 m and 20 m height,and were south winds from afternoon to sunset and north winds form night to next morning above 100 m height.
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In order to further understanding long-term variation of low-level wind field over the mountains region of the Qinghai-Xizang Plateau,based on the observational data of boundary layer tower and wind profile radar in Dali region of the southeastern margin of the Qinghai-Xizang Plateau from 2008 to 2012,the vertical structure and variation characteristics of wind field were analyzed.The results show as follow:Firstly,wind speed and wind direction frequency in the low-level atmosphere varied with height.Wind force scale was 2 level and prevailing winds were east winds between 2 m and 400 m height.It indicated that wind speed and wind direction measured with boundary layer tower and wind profile radar was continuous.Secondly,vertical wind speed changed with season,which its value was greater in winter than that in summer.The diurnal variations of wind speed at different height were different,that is to say,the diurnal variations of wind speed displayed one peak below 20 m and two speaks between 100 m and 1500 m height,and were not evident above 2000 m height.The monthly variations of wind speed showed one speak below 20 m and above 1500 m height,and showed two speaks between 100 m and 1000 m height.Finally,the zonal winds below 600 m height appeared a daily cycle of east wind and west wind.The meridional winds were south winds all the day between 2 m and 20 m height,and were south winds from afternoon to sunset and north winds form night to next morning above 100 m height.
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DONG Baoju,
SUN Jihua etc
.Vertical Structure and Variation Characteristics of Wind Field in Low-Level Atmosphere in the Southeastern Margin of Qinghai-Xizang Plateau[J]& PLATEAU METEOROLOGY, ): 597-607
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尚大成,王澄海.2006.高原地表过程中冻融过程在东亚夏季风中的作用[J].干旱气象,24(3):19-22.Shang Dacheng,Wang Chenghai.The effect of the frozen-thaw process in Tibetan Plateau on summer monsoon over eastern Asia[J].J Arid Meteor,24(3):19-22.
Hennessy K J,Gregory J M,Mitchell J F B.1997.Changes in daily precipitation under enhanced greenhouse conditions[J].Climate Dyn,13(9):667-680.
郭其蕴.1994.东亚冬季风的变化与中国气温异常的关系[J].应用气象学报,5(2):218-225.Guo Qiyun.1994.The relationship between the change of the east Asian winter monsoon and temperature in China[J].J Appl Meteor,5(2):218-225.
尚伦宇,吕世华,张宇,等.2010.青藏高原东部土壤冻融过程中地表粗糙度的确定[J].高原气象,29(1):17-22.Shang Lunyu,Lv Shihua,Zhang Yu,et al.2010.Determination of surface roughness length during soil freezing and thawing season over eastern Qinghai-Xizang Plateau[J].Plateau Meteor,29 (1):17-22.
孙淑芬.2005.陆面过程的物理、生化机理和参数化模型[M].北京:气象出版社.Sun Shufen.Physical,biochemical mechanism and parametric model of land surface process[M].Beijing:China Meteorological Press.
唐红玉,李锡福,李栋梁.2014.青藏高原春季积雪多、少年中低层环流对比分析[J].高原气象,33(5):.Tang Hongyu,Li Xifu,Li Dongliang.2014.Contrast of circulation pattern related to more and less spring snow cover over Qinghai-Xizang Plateau[J].Plateau Meteor,33(5):.DOI:10.7522/j.issn.13.00125.
Bezdek J C,Ehrlidh R,Full W.1984.FCM:The Fuzzy C-means clustering algorithm[J].Computers and Geosciences,10(2-3):191-203.
叶笃正,高由禧.1979.青藏高原气象学[M].北京:科学出版社,10-48,153-171.Ye Duzheng,Gao Youxi.1979.Tibetan Plateau meteorology[M].Beijing:Chinese Science Press,10-48,153-171.
Edward English.2005.Development of knowledge for predictive mapping using a Fuzzy C-means classification[C]//Proceedings of the Eleventh International Fuzzy Systems.Association World Congress,7:TP18.
Kalnay E,Kanamitsu M,Kistler R,et al.1996.The NCEP/NCAR 40-Year Reanalysis Project[J].Bull Amer Meteor Soc,77(3):437-471.
2.0.CO;2 target="_blank">
黄嘉佑,刘舸,赵昕奕.2004.副高极涡因子对我国夏季降水的影响[J].大气科学,28(4):517-526.Huang Jiayou,Liu Ge,Zhao Xinyi.2004.The influence of Subtropical High indexes and polar vortex indexes on the summertime precipitation in China[J].Chinese J Atmos Sci,28(4):517-526.
王澄海,董文杰,韦志刚.2003.青藏高原季节冻融过程与东亚大气环流关系的研究[J].地球物理学报,46(3):309-316.Wang Chenghai,Dong Wenjie,Wei Zhigang.2003.Study on relationship between the frozen-thaw process in Qinghai-Xizang Plateau and circulation in east Asia[J].Chinese Journal of Geophysics,46(3):309-316.
中国气象局.2003.地面气象观测规范[Z].北京:气象出版社,131-132.China Meteorological Administration.2013.Specifications for surface meteorological observation[Z].Beijing:China Meteorological Press,131-132.
王澄海,尚大成.2007.藏北高原土壤温、湿度变化在高原干湿季转换中的作用[J].高原气象,26(4):677-685.Wang Chenghai,Shang Dacheng.2007.Effect of the variation of the soil temperature and moisture in the transition from dry-season to wet-season over northern Tibetan Plateau[J].Plateau Meteor,26(4):677-685.
Gilichinsky D A,Barry R G,Bykhovets S S,et al.1998.A century of temperature observations of soil climate:Methods of analysis and long-term trends[C]//Lewkowicz A G,Allard M,eds.Yellowknife,Canada:Proceedings of the Seventh International Conference on Permafrost,313-317.
Katz R W,Brown B G.1992.Extreme events in a changing climate:Variability is more important than averages[J].Climatic Change,21(3):289-302.
王澄海,师锐.2007.青藏高原西部陆面过程特征的模拟分析[J].冰川冻土,29(1):73-81.Wang Chenghai,Shi Rui.2007.Simulation of the land surface process in the western Tibetan Plateau in summer[J].J Glaciology Geocryology,29 (1):73-81.
康丽华,陈文,魏科.2006.我国冬季气温年代际变化及其与大气环流异常变化的关系[J].气候与环境研究,11 (3):330-339.Kang Lihua,Chen Wen,Wei Ke.2006.The interdecadal variation of winter temperature in China and its relation to the anomalies in atmospheric general circulation[J].Climatic Environ Res,11(3):330-339.DOI:10.3969/j.issn.06.03.009.
周立波,邹捍,马舒坡,等.2007.南亚夏季风对珠穆朗玛峰北坡地面风场的影响[J].高原气象,26(6):.Zhou Libo,Zou Han,Ma Shupo,et al.2007.Impacts of the south Asian summer monsoon on variations of surface wind on the northern slope of Mt.Qomolangma[J].Plateau Meteor,26(6):.
Li Z,Yan Z.2009.Homogenized China daily mean/maximum/minimum temperature series [J].Atmos Oceanic Sci Lett,2(4):237-243.
王澄海,师锐,左洪超.2008.青藏高原西部冻融期陆面过程的模拟分析[J].高原气象,27(2):239-248.Wang Chenghai,Shi Rui,Zuo Hongchao.2008.Analysis on simulation of characteristic of land surface in western Qinghai-Xizang Plateau during frozen and thawing[J].Plateau Meteor,27(2):239-248.
李崇银,王力群,顾薇.2011.冬季蒙古高压与北太平洋海温异常的年际尺度关系[J].大气科学,35(2):193-200.Li Chongyin,Wang Liqun,Gu Wei.2011.Interannual time-scale relationship between Mongolia high and SST anomaly in the North Pacific in winter[J].Chinese J Atmos Sci,35(2):193-200.
Lamaud E,Irvine M.2006.Temperature-humidity dissimilarity and heat-to-water-vapour transport efficiency above and within a pine forest canopy: The role of the Bowen ratio[J].Bound-Layer Meteor,120(1):87-109.DOI:10.-005-9032-6.
雷杨娜,孙娴,乐章燕.2014.中国东部地区冬季气温与北极涛动的关系[J].气象与环境学报,30(4):42-48.Lei Yangna,Sun Xian,Le Zhangyan.2014.Relationship between winter air temperature in Eastern China and Arctic Oscillation[J].J Meteor Environ,30(4):42-48.DOI:10.3969/j.issn.l673-503 X..
王少影,张宇,吕世华,等.2012.玛曲高寒草甸地表辐射与能量收支的季节变化[J].高原气象,31(3):605-614.Wang Shaoyin,Zhang Yu,L Shihua,et al.2012.Seasonal variation characteristics of radiation and energy budgets in alpine meadow ecosystem in Maqu grassland[J].Plateau Meteor,31(3):605-614.
Larsen X G,Kelly M,Sempreviva A M.2014.On the temperature and humidity dissimilarity in the marine surface layer[J].Bound-Layer Meteor,151(2):273-291.DOI:10.-013-9896-9.
李瑞青,吕世华,韩博,等.2012.青藏高原东部三种再分析资料与地面气温观测资料的对比分析[J].高原气象,31(6):.Li Ruiqing,Lu Shihua,Han Bo,et al.2012.Preliminary comparison and analyses of air temperature at 2m height between three reanalysis data-sets and observation in the east of Qinghai-Xizang Plateau[J].Plateau Meteor,31(6):.
李崇银,王力群,顾薇.2011.冬季蒙古高压与北太平洋海温异常的年际尺度关系[J].大气科学,35(2):193-200.Li Chongyin,Wang Liqun,Gu Wei.2011.Interannual time-scale relationship between Mongolia high and SST anomaly in the North Pacific in winter[J].Chinese J Atmos Sci,35 (2):193-200.DOI:10.3878/j.issn.11.02.01.
Li D,Bou-Zeid E.2011.Coherent structures and the dissimilarity of turbulent transport of momentum and scalars in the unstable atmospheric surface layer[J].Bound-Layer Meteor,140(2):243-262.DOI:10.-011-9613-5.
刘晴晴,王盘兴,徐祥德,等.2011.蒙古高压一组环流指数及与中国同期气候异常关系分析[J].热带气象学报,27(6):889-898.Liu Qingqing,Wang Panxing,Xu Xiangde,et al.2011.A group of circulation indices of Mongolia high and analysis of its relationship with simultaneous anomaly in the climate of China[J].J Trop Meteor,27(6):889-898.
Haeberli W,Hoclzle M,Keller F,et al.1993.Monitoring the long-term revolution of mountain permafrost in the Swiss Apls[C]//Proceedings of Six International Conference on Permafrost,July 5-9,Beijing,1993.Guangzhou:South China University of Technology Press,1:214-219.
王国亚,毛炜峄,贺斌,等.2012.新疆阿勒泰地区积雪变化特征及其对冻土的影响[J].冰川冻土,34(6):.Wang Guoya,Mao Weiyi,He Bin,et al.2012.Changes in snow covers during
and its effects on frozen ground in Altay region,Xinjiang[J].J Glaciology Geocryology,34(6):.
麻巨慧,王盘兴,李丽平,等.南方雪灾&与同期蒙古高压中期活动的关系[J].大气科学学报,32(5):652-660.Ma Juhui,Wang Panxing,Li Liping,et al.2009.Contemporaneous relationship between&0801 snow storm over Southern China&and medium-term activities of Mongolian high[J].Trans Atmos Sci,32(5):652-660.
周明煜,徐祥德,卞林根,等.2000.青藏高原大气边界层观测分析与动力学研究[M].北京:气象出版社,57-78.Zhou Mingyu,Xu Xiangde,Bian Lingen,et al.2000.Observational analysis and dynamic study of atmospheric boundary layer on Tibetan Plateau[M].Beijing:China Meteorological Press,57-78.
Monin A S,Obukhov A M.1954.Basic laws of turbulent mixing in the ground layer of the atmosphere[J].Trans Geophys Inst Akad Nauk USSR,24(151):163-187.
朱凌云,张美根,马舒坡,等.2007.珠峰绒布河谷大气边界层结构的数值模拟[J].高原气象,):.Zhu Lingyun,Zhang Meigen,Ma Shupo,et al.2007.Numerical simulation of atmospheric boundary layer structure over Rongbuk valley of Mt.Qomolangma[J].Plateau Meteor,26(6):.
Nordbo A,Jarvi L,Haapanala S,et al.2013.Intra-city variation in urban morphology and turbulence structure in Helsinki,Finland[J].Bound-Layer Meteor,146(3):469-496.DOI:10.-012-9773-y.
马晓波.1995.50年来蒙古国与北半球的气温变化[J].高原气象,14(3):348-358.Ma Xiaobo.1995.Air temperature variations in Mongolia and Northern Hemisphere for recent 50 years[J].Plateau Meteor,14(3):348-358.
邹捍,李鹏,朱金焕,等.2007a.HEST2007珠峰北坡风廓线观测研究[J].高原气象,26(6):.Zou Han,Li Peng,Zhu Jinhuan,et al.2007a.Observational study on the wind from wind-profiler during HEST2007[J].Plateau Meteor,26(6):.
邹捍,周立波,马舒坡,等.2007b.珠穆朗玛峰北坡局地环流日变化的观测研究[J].高原气象,26(6):.Zou Han,Zhou Libo,Ma Shupo,et al.2007b.Observation of diurnal circulation on the northern slope of Mt.Qomolangma[J].Plateau Meteor,26(6):.
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是谁给予兴化市周庄镇人民政府的权利
是谁给予兴化市周庄镇人民政府的权利
周庄镇人民政府实施镇区二次改水工程,本来是一件造福人民的民心工程,可是却变味了,门市改水1200元,住房600元费用,但是我们以前都交了初装费,现在还要收初装费,如果下次再改水,是不是我们还要交?周庄镇人民政府依据法律哪一条哪一款,凭什么收取费用。
周庄镇人民政府一没有召开听会,二没有物价部门核实,擅自收取如此高额费用,公理何在?在党的十八大召开之前,周庄镇人民政府如此之举,有碍和谐。
党和政府给的
青春流逝,真情犹在,活跃同城QQ群,今天你加了吗?
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新人进群请上传本人照片,主动进群报道。非诚勿扰.
如此政府应该问责
市政府应该查一查
楼主应该拨打:《小范帮你忙》给曝光一下,这些个当官的就不会收费了····
我们那儿改水是没人交的400元,现在的水烧开后一点沉淀物都没有!
中国人口多底子薄,党和政府能养活中国13亿人口已经很不容易了.现在国家有困难,咱们老百姓更应该舍小家保大家,支持党和政府的正确领导.在党和政府的正确领导下,中国国力日益强盛,老百姓生活欣欣向荣,但是国际反华势力是看不得中国发展.他们雇佣大批网特质疑社会主义建设,煽动人民群众对党和政府的不满情绪,破坏党和国家领导人在人民群众中的光辉形象,咱们老百姓不能被它们蒙蔽煽动,做出危害社会秩序,破坏和谐社会的错事.那些贪图蝇头小利,丧失国格人格的汉奸网特,是注定没有好下场的.
  中国人口多底子薄,历史上被帝国主义,蒋家王朝洗劫掠夺,是党和政府把中国人民从旧社会解救出来,中国老百姓是感恩的.党和政府在短短几十年就解决了十几亿中国人的吃饭问题,把一穷二白的中国建设成为世界第二经济强国,党和政府高瞻远瞩的执政能力是不容质疑的.
  当前国家形势一片大好,财政收入即将达到20万亿!祖国一片繁荣昌盛。养老金正在农村普及!而我们的福利会越来越好的呀!
  大家应该理性发言,我们国家本来就人口多、底子薄,经过短短30年改革开放能够取得今天的成就已经很了不起了。现在我们的的领导,出访国外都受到最高规格接待,犹如众星捧月,看到这些,作为一个中国人的你不自豪吗?现在国家正处于向前大发展的关键时期,难免会出现一些社会问题,境外的反华势力故意渲染、放大这些问题,误导国民辱骂、诋毁国家,大家应该擦亮眼睛,自觉维护社会稳定。时时刻刻别忘了自己是一名中国人,记住:子不嫌母丑,狗不嫌家贫!!!时时刻刻别忘了自己是一名马列主义接班人!
  每天面对这些网上暴民的漫骂和攻击。真的让我很痛心!我无时无刻不控制自己的情绪,耐心的和你们讲着道理。可换来的缺是一次又一次的漫骂。我的心在滴血,一颗真挚的心就这样被践踏。
  我坚信我是站在正义一边,我是个受过高等教育的人,我觉得满口污言秽语是很可耻的。
  我们的祖国正在发展阶段,法律法规也在不断的完善。我们应该给予更多的支持,而不是各种漫骂和攻击。一旦看见国内出了什么事情,这些暴民兴奋的拍手叫好。你们到底还是中国人么?
  即使你不爱国,也请不要漫骂好么?一个人的力量是渺小的,而发生一些问题,靠攻击漫骂也是没有用的。相信法律的公正,真的遇到问题,通过正当的途径来解决,这才是正路。闹不解决任何问题。
  祖国要强大,靠的是我们团结。我很不明白,为什么声嘶力竭劝你们向善,反到遭到漫骂。你们真的是暴民么?你们的心真的是肉长的么?只有祖国强大了,我们在外面才更加自信。一个连自己国家都不爱的人,谈什么未来。
  不要受美狗日杂的挑唆。做个文明的人不好么?怎么我一字一句的诉说道理。就没人愿意去听呢。我一直高素质严要求自己。文明发言。我也希望你们也做到。看我的字字句句,哪句不在理上。你们每天的漫骂,反到成了我的不是。你们好好想想吧。看着你们堕落,我真的很痛心。
当然是江苏省兴化市人民政府给的
嘎里个兄弟们!进来望啊子啥~
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