globalchange  > 气候变化与战略
CSCD记录号: CSCD:5295194
论文题名:
近50年鄱阳湖水位变化特征研究
其他题名: VARIATION CHARACTERISTICS OF WATER LEVEL IN POYANG LAKE OVER 50YEARS
作者: 欧阳千林1; 刘卫林2
刊名: 长江流域资源与环境
ISSN: 1004-8227
出版年: 2014
卷: 23, 期:11, 页码:1203-1210
语种: 中文
中文关键词: 鄱阳湖 ; 水位 ; Mann-Kendall法 ; 最大熵谱
英文关键词: Poyang Lake ; water level ; Mann-Kendall method ; maximum entropy spectrum method
WOS学科分类: ENVIRONMENTAL SCIENCES
WOS研究方向: Environmental Sciences & Ecology
中文摘要: 基于鄱阳湖棠荫水文站近50a(1962~2012年)水位资料,采用Mann-Kendall法和最大熵谱法分析鄱阳湖湖区水位的演变趋势和周期性。研究表明:(1)年平均水位、年最高水位没有显著变化趋势,年最低水位具有显著下降趋势;(2)年平均水位、年最高水位的突变点为2005年,突变后期转为微弱下降趋势,年最低水位的突变点为2003和2005年,突变后期下降速度加快;(3)年平均水位以25~26a为第一主周期,6~7a为次主周期,11a、12a、16a年为第三主周期,年最高水位以19a为主周期,年最低水位以6a为第一主周期,16a为次主周期;(4)未来10a内鄱阳湖水资源量并无显著衰减趋势,洪水位并无上升趋势,年最低水位持续走低,进入枯水时间提前,枯水持续时间延长。
英文摘要: As the largest freshwater lake in China,the largest wetland in Asia and an important ecological zone in the world for migrating birds,the Poyang Lake plays important roles for ecology,human life and produce.The Poyang Lake has important function on sustaining bio-diversity,regulating flood,providing water for the midstream and downstream of the Yangtze River,and is strategic significant for regional and nationwide ecological safety.But it experienced significant changes in recent years under the pressure of global climate change and human disturbance,for example,the frequency of flood and drought increased,causing predicament for the habiting of fishes,migrating birds and finless porpoises,also for shipping,human fetching drinking water.The implement of Ecological Economic Zone Program of Poyang Lake,and the plan of Poyang Lake Eco-Hydraulic Project,brought new challenges and pressures for ecosystem of the Poyang Lake.Since the change of water level in the Poyang Lake had close relationships with birds migrating,ecological scene,and the development of fisheries,it was essential to study the change of water level for the health of the Poyang Lake ecosystem and the sustainable development of Poyang Lake Eco-economic Region,while existing researches mainly aimed to the runoff characteristics in Poyang Lake Basin,seldom focused on the water level.This paper investigated the trend and cyclical characteristic of water level in the Poyang Lake and obtained qualitative and quantitative analysis,employing the Mann-Kendall method and maximum entropy spectral method,basing on water level data in the past 51years(1962-2012)of Tangyin Hydrological Station,which located in an island surrounded by water in the center of the main body of the Poyang Lake.Almost 55%of inflow water of the Poyang Lake pass nearby this island.Both in high-water period and lowwater period,the water level data of Tangyin Hydrological Station had good representation for the Poyang Lake. The results show as follows.1)The annual average water level and the annual highest water level had no significant changing trend,and the annual lowest water level had significant downward trend.2)The mutation point of annual mean water level and the annual highest water level was the year of 2005,and the late mutations were transferred to weak downtrend;the mutations point of annual minimum water level was between the year of 2003and 2005,and the downward trend was more obvious during the late mutation.Moreover,there were significant decreasing trends especially since the year of 2010.3)The annual average water level was with 25-26ain the first cycle,6 -7ain the second main cycle,11a,12a,16ain the third main cycle;there were 19acycles in the annual highest water level;there were 6ain the first main cycle in the annual minimum water level,and 16ain the second main cycle.4)The next ten years,the flood will be without a rising trend,and the flood inundated area will not expand;the low water level will be lower,the dry time will come into being in advance,the disappear of dry time will delay,and the problem of water shortage in extended urban area and shipping will be more serious.
资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/148638
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作者单位: 1.鄱阳湖水文局, 星子, 江西 332800, 中国
2.南昌工程学院, 南昌, 江西 330099, 中国

Recommended Citation:
欧阳千林,刘卫林. 近50年鄱阳湖水位变化特征研究[J]. 长江流域资源与环境,2014-01-01,23(11):1203-1210
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