[1]付强,李铁男,李天霄,等.基于近似熵理论的三江平原月降水量空间复杂性分析[J].水土保持研究,2015,22(02):113-116,122.
　FU Qiang,LI Tienan,LI Tianxiao,et al.Analysis of Spatial Complexity of Monthly Precipitation in Sanjiang Plain Based on Approximate Entropy[J].Research of Soil and Water Conservation,2015,22(02):113-116,122.
点击复制

基于近似熵理论的三江平原月降水量空间复杂性分析

《水土保持研究》[ISSN:1005-3409/CN:61-1272/P] 卷: 22 期数: 2015年02期 页码: 113-116,122 栏目: 出版日期: 2015-04-28
Title:
Analysis of Spatial Complexity of Monthly Precipitation in Sanjiang Plain Based on Approximate Entropy
作者:
付强1,2, 李铁男1, 李天霄1, 孟凡香3
1. 东北农业大学 水利与建筑学院, 哈尔滨 150030;
2. 黑龙江省粮食产能提升协同创新中心, 哈尔滨 150030;
3. 黑龙江农垦勘测设计研究院, 哈尔滨 150030
Author(s):
FU Qiang1,2, LI Tienan1, LI Tianxiao1, MENG Fanxiang3
1. Collage of Water Conservancy & Architecture, Northeast Agricultural University, Harbin 150030, China;
2. Collaborative Innovation Centre of Grain Production Promotion in Heilongjiang Province, Harbin 150030, China;
3. Heilongjiang Nongken Survey Design Research Institute, Harbin 150090, China
关键词:
三江平原; 近似熵理论; 月降水量; 空间复杂性
Keywords:
Sanjiang Plain; approximate entropy theory; monthly precipitation; spatial complexity
分类号:
P333.1;S11+7
摘要:
以三江平原7个国家级气象站1959—2013年的月降水量数据为基础，采用近似熵理论、ArcGIS空间分析理论，分析了近50 a三江平原月降水量的空间复杂性。结果表明：三江平原月降水量表现出了较强的非线性特征，其中南部鸡西站月降水量的极差最大，达到了340.1 mm，北部富锦站月降水量的极差最小，仅为231.6 mm；月降水量空间复杂性东西方向整体呈现出了条状分布，且由西南向东北逐渐增加，这主要与三江平原西南部海拔低，湿地面积多，降水日数与降水强度小，且多为山区等因素有关。研究成果对于指导三江平原科学合理地利用降水资源具有一定的指导意义。
Abstract:
The approximate entropy theory and ArcGIS spatial analysis theory were used to analyze the spatial complexity of monthly precipitation data collected at seven national weather stations in the Sanjiang Plain from 1959 to 2013. The results showed that the monthly precipitation presented a strong nonlinear feature. The range of monthly precipitation in Jixi station was maximum, which reached to 340.1 mm, and it was minimum in Fujin station, which only reached to 231.6 mm. The spatial complexity of monthly precipitation presented a strip distribution at the east-west direction and increased gradually from the southwest to northeast. The low altitude, more wetland and mountain areas, small precipitation intensity and precipitation day were the main drivers of difference in the spatial complexity characteristics. The research results can provide guidance for scientific investigations and the reasonable use of rainfall resources in the Sanjiang Plain.

参考文献/References:

[1] 刘卫林.漳河观台站降雨径流时间序列的混沌特性分析[J].河海大学学报:自然科学版,2011,39(4):384-390.
[2] 于延胜,陈兴伟.福州市区降雨序列多时间尺度的混沌特征[J].福建师范大学学报:自然科学版,2008,24(5):96-100.
[3] Millan H, Rodriguez J, Ghanbarian-Alavijeh B, et al. Temporal complexity of daily precipitation records from different atmospheric environments:Chaotic and Levy stable parameters[J]. Atmospheric Research,2011,101(4):879-892.
[4] 武秋晨,刘东.等概率粗粒化LZC算法在降水变化复杂性研究中的应用[J].中国农村水利水电,2013(5):1-5,10.
[5] 刘东,张健,付强.基于连续小波变换与分形理论的三江平原井灌区地下水埋深序列复杂性研究[J].水土保持研究,2011,18(2):116-120.
[6] Fan Q, Wang Y, Zhu L. Complexity analysis of spatial-temporal precipitation system by PCA and SDLE[J]. Applied Mathematical Modelling,2013,37(6):4059-4066.
[7] 刘东,周明,孟军.近似熵在三江平原地下水埋深序列复杂性分析中的应用[J].自然资源学报,2012,27(1):115-121.
[8] 刘萌,刘东.基于样本熵的地下水埋深序列复杂性分析[J].水利水电技术,2012,43(12):5-8.
[9] 孙东永,黄强,王义民,等.滑动近似熵在径流序列突变性分析中的应用[J].水力发电学报,2014,33(4):1-6.
[10] 王启光,张增平.近似熵检测气候突变的研究[J].物理学报,2008,57(3):1976-1983.
[11] Pan X, Yan B, Yoh M, et al. Temporal variability of iron concentrations and fractions in wetland waters in Sanjiang Plain, Northeast China[J]. Journal of Environmental Sciences-China,2010,22(7):968-974.
[12] Zhou D, Gong H, Wang Y, et al. Driving forces for the marsh wetland degradation in the Honghe National Nature Reserve in Sanjiang Plain, Northeast China[J]. Environmental Modeling & Assessment,2009,14(1):101-111.
[13] 何文平,何涛,成海英,等.基于近似熵的突变检测新方法[J].物理学报,2011,60(4):820-828.
[14] 原立峰,张增信,刘星飞,等.鄱阳湖流域近49a降雨序列一致性检验与分析[J].安徽农业科学,2013,41(2):732-735.
[15] 姜秋香,付强,王子龙.空间变异理论在土壤特性分析中的应用研究进展[J].水土保持研究,2008,15(1):250-253.
[16] 腊贵晓,顾怀胜,刘国顺,等.喀斯特地区烟田土壤养分的空间变异特征[J].水土保持研究,2012,19(3):48-53.

相似文献/References:

[1]殷嘉迪,雷国平,乐容潮,等.三江平原农村居民点时空格局演变——以富锦市为例[J].水土保持研究,2017,24(06):300.
　YIN Jiadi,LEI Guoping,LE Rongchao,et al.Spatiotemporal Evolution of Rural Settlements in Sanjiang Plain—A Case Study in Fujin City[J].Research of Soil and Water Conservation,2017,24(02):300.
[2]刘东,张健,付强.基于连续小波变换与分形理论的三江平原井灌区地下水埋深序列复杂性研究[J].水土保持研究,2011,18(02):116.
　LIU Dong,ZHANG Jian,FU Qiang.Study on Complexity of Groundwater Depth Series in Well Irrigation Area of Sanjiang Plain Based on Continuous Wavelet Transform and Fractal Theory[J].Research of Soil and Water Conservation,2011,18(02):116.
[3]刘东,付强.基于小波变换的三江平原井灌区主汛期降水序列多时间尺度分析[J].水土保持研究,2008,15(06):42.
　LIU Dong,FU Qiang.Multi-Time Scales Analysis of Main Flood Season Precipitation Series Based on Wavelet Transform in Area of Well-Irrigation in Sanjiang Plain[J].Research of Soil and Water Conservation,2008,15(02):42.
[4]陈红光,李晨洋,李晓丹.基于风险分析的三江平原灌区多水源联合调度方案优化决策研究[J].水土保持研究,2013,20(04):273.
　CHEN Hong-guang,LI Chen-yang,LI Xiao-dan.Study on the Water Joint Operation Scheme Optimization in Sanjiang Plain Irrigation Area Based on Risk Analysis[J].Research of Soil and Water Conservation,2013,20(02):273.
[5]韩丽伟,付强,刘东,等.三江平原地下水承载能力综合评价模型的构建及其应用[J].水土保持研究,2010,17(02):182.
　HAN Li-wei,FU Qiang,LIU Dong,et al.Construction and Application of the Model on Groundwater Resources Carrying Capacity in Sanjiang Plain[J].Research of Soil and Water Conservation,2010,17(02):182.
[6]马吉巍,郭翔宇,付强,等.区域农业水土资源复杂适应系统配置研究——以三江平原为例[J].水土保持研究,2014,21(03):256.
　MA Ji-wei,GUO Xiang-yu,FU Qiang,et al.Study on Complex Adaptive Allocation of Regional Agricultural Water and Soil Resources—Taking Sanjiang Plain for Example[J].Research of Soil and Water Conservation,2014,21(02):256.
[7]申月静,雷国平,曲晓涵,等.基于加权Voronoi图扩展断裂点的农村居民点布局优化[J].水土保持研究,2017,24(04):284.
　SHEN Yuejing,LEI Guoping,QU Xiaohan,et al.Layout Optimization of Rural Settlements Based on the Extended Break-Point Model of Weighted Voronoi diagram[J].Research of Soil and Water Conservation,2017,24(02):284.
[8]杜嘉,张柏,宋开山,等.基于NOAA/AVHRR数据估算三江平原蒸散量研究初探[J].水土保持研究,2009,16(02):56.
　DU Jia,ZHANG Bai,SONG Kai-shan,et al.Estimated Evapotranspiration Based on NOAA/AVHRR Data in the Sanjiang Plain[J].Research of Soil and Water Conservation,2009,16(02):56.
[9]王振芬.三江平原湿地不同土地利用方式对土壤养分及酶活性的影响[J].水土保持研究,2019,26(02):43.
　WANG Zhenfen.Characteristics of Soil Nutrients and Enzyme Activity Under Different Types of Land Use in Wetland of Sanjiang Plain[J].Research of Soil and Water Conservation,2019,26(02):43.
[10]鲁菁,张玉虎,高峰,等.近40年三江平原极端降水时空变化特征分析[J].水土保持研究,2019,26(02):272.
　LU Jing,ZHANG Yuhu,GAO Feng,et al.Temporal and Spatial Variation Characteristics of Extreme Precipitation in the Sanjiang Plain in Recent 40 Years[J].Research of Soil and Water Conservation,2019,26(02):272.

备注/Memo

收稿日期:2014-10-02;改回日期:2014-11-10。
基金项目:国家自然科学基金（51179032，51479032）；水利部公益性行业科研专项经费项目（201301096）；教育部新世纪优秀人才支持计划；黑龙江省高校长江学者后备支持计划项目；黑龙江省杰出青年基金（JC201402）
作者简介:付强(1973-),男,辽宁锦州人,教授,博士生导师,主要从事农业水土资源系统分析、节水灌溉及农业系统工程建模与优化技术、冻融土壤水热作用机理等方面研究。E-mail:fuqiang0629@126.com

更新日期/Last Update: 1900-01-01