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首页|期刊导航|中国岩溶|GM(1,1)分解模型与ARIMA模型在岩溶地下水模拟中的对比研究——以柳林泉流量模拟为例

GM(1,1)分解模型与ARIMA模型在岩溶地下水模拟中的对比研究——以柳林泉流量模拟为例

李华敏 吴敬 赵娇娟 郝永红 王亚捷 曹碧波

中国岩溶2011,Vol.30Issue(3):260-269,10.
中国岩溶2011,Vol.30Issue(3):260-269,10.

GM(1,1)分解模型与ARIMA模型在岩溶地下水模拟中的对比研究——以柳林泉流量模拟为例

Comparative study on karst ground water simulation between GM(1,1) decomposition model and ARIMA model :A case study on discharge simulation of the Liulin Spring

李华敏 1吴敬 2赵娇娟 1郝永红 3王亚捷 3曹碧波1

作者信息

  • 1. 天津师范大学城市与环境科学学院,天津300387
  • 2. 天津财经大学理工学院统计系,天津300222
  • 3. 天津师范大学天津市水环境与水资源重点实验室,天津300387
  • 折叠

摘要

Abstract

The discharge of the Liulin spring is simulated with GM(1,1) decomposition model and ARIMA model respectively. According to the hydrological characteristics, the Liulin spring flow series could be divided into two periods. First, from 1957 to 1973 the spring flow was under natural state; second, from 1974 to 2009 the spring flow was impacted by both climate change and human activities. Using the data of first period, the spring flow under the natural state is fitted with GM(1,1) decomposition model and ARIMA model, and then the models are extrapolated to obtain the second periods' spring flow under the natural state. According the water balance principle, the spring flow decrement contributed by human activities is acquired by subtracting the observed discharge from simulated spring flow of the second period under the natural state. Thus, it is differentiated the effects of human activities from climate change. The simulated Liulin Springs' attenuation from 1970s to early 21st century is 2. 26 m3/s by GM (1,1) decomposition model and 2. 36 m3/s by ARIMA model with the relative error being 0. 44% and 2. 20% respectively, showing both GM (1,1) decomposition model and ARIMA model are suitable for spring flow simulation. Comparing the effects of human activities and climate change to the depletion of the Liulin Spring's discharge, the authors find that the contribution of human activities is 8 to 9 times higher than that of the climate change. The empirical studies have shown that the GM (1,1) model is of high precision in simulating the exponential series. It can also improve accuracy by periodic amendment, when simulate the spring flow with periodic fluctuations. ARIMA model could reflect time-lag between precipitation and spring discharge and accurately simulate their quantitative relation.

关键词

GM(1,1)分解模型/ARIMA模型/分时段分析/岩溶泉流量

Key words

GM (1,1) decomposition model/ ARIMA model/ piecewise analysis/ karst spring discharge

分类

天文与地球科学

引用本文复制引用

李华敏,吴敬,赵娇娟,郝永红,王亚捷,曹碧波..GM(1,1)分解模型与ARIMA模型在岩溶地下水模拟中的对比研究——以柳林泉流量模拟为例[J].中国岩溶,2011,30(3):260-269,10.

基金项目

国家自然科学基金(40972165,40572150)、天津市科技发展战略研究计划项目09JCYBJC27500、天津市水资源与水环境重点实验室开放基金52XS1015 (40972165,40572150)

中国岩溶

OACSCDCSTPCD

1001-4810

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