资源科学 ›› 2016, Vol. 38 ›› Issue (9): 1754-1767.doi: 10.18402/resci.2016.09.13
收稿日期:
2016-01-10
修回日期:
2016-06-05
出版日期:
2016-09-25
发布日期:
2016-09-22
作者简介:
作者简介:刘盈曦,女,云南昆明人,博士,讲师,主要研究方向为环境经济学。E-mail:
基金资助:
LIU Yingxi1(), PENG Guifen2, CHEN Xiangang3, YANG Yuming4
Received:
2016-01-10
Revised:
2016-06-05
Online:
2016-09-25
Published:
2016-09-22
摘要:
采用云南省香格里拉气象站55a(1958-2012)的逐年气温、降水量、绝对湿度、相对湿度和霜日数资料,引入多元最小二乘估计模型(多元OLS)、多元向量自回归模型(多元VAR)和结构方程模型,基于Morlet连续复小波(Cmor)变换的主周期数据,探索未来50a香格里拉气温等气候环境要素的定量预估模型、变化趋势及5个主要气候环境要素的相互关系。结果表明:未来50a内香格里拉的气温以0.44℃/10a的速率升高,50a后气温将升高2℃左右;降水以围绕平均值做周期振荡为主,并以14.7mm/10a的速率增多;绝对湿度以0.06 mg/L/10a的速率增大,并有明显的周期振荡;相对湿度以-0.96%/10a的速率减小,并有周期振荡;年霜日数以-2.8d/10a的速率减少,并有周期振荡。绝对湿度、相对湿度和霜日数的变化与气温和降水的变化显著相关,气温变化对湿度和霜日数的影响大于降水量的影响,气温的持续升高是除降水外其他气候要素变化的主要原因。
刘盈曦, 彭贵芬, 陈先刚, 杨宇明. 香格里拉未来50a主要气候环境要素变化预估——基于小波分析和多元 VAR 回归预估模型[J]. 资源科学, 2016, 38(9): 1754-1767.
LIU Yingxi,PENG Guifen,CHEN Xiangang,YANG Yuming. Climatic and environmental changes in Shangri-La in next 50 years according to wavelet analysis and multiple VAR regression prediction modeling[J]. Resources Science, 2016, 38(9): 1754-1767.
表3
多元OLS模型预估因子分析结果"
降水量 | 绝对湿度 | 相对湿度 | 霜日 | ||||
---|---|---|---|---|---|---|---|
3a主周期 | 3.945 0 (0.121) | 5a主周期 | 0.069 0***(0.006) | 28a主周期 | -0.325 0* (0.059) | 6a主周期 | 0.822 0***(0.001) |
6a主周期 | 0.381 0 (0.308) | 8a主周期 | 0.068 9***(0.001) | 31a主周期 | 1.119 0** (0.034) | 8a主周期 | 0.327 0 (0.146) |
7a主周期 | 0.655 0 (0.187) | 15a主周期 | 0.034 7* (0.059) | 32a主周期 | -0.852 0** (0.023) | 22a主周期 | 0.887 0 (0.129) |
13a主周期 | 0.669 0***(0.001) | 23a主周期 | 0.009 7 (0.215) | 23a主周期 | -0.764 0 (0.220) | ||
22a主周期 | 0.210 0 (0.225) | 31a主周期 | 0.002 5 (0.605) | 28a主周期 | -0.445 0 (0.375) | ||
31a主周期 | 0.543 0 (0.355) | 29a主周期 | 0.491 0 (0.274) | ||||
趋势项 | 0.934 0 (0.216) | 趋势项 | 0.005 6***(0.000) | 趋势项 | -0.087 5***(0.000) | 趋势项 | -0.341 0***(0.000) |
常数项 | 611.200 0***(0.000) | 常数项 | 6.756 0***(0.000) | 常数项 | 71.340 0***(0.000) | 常数项 | 159.400 0***(0.000) |
N | 55 | N | 55 | N | 55 | N | 55 |
R | 0.609 | R | 0.714 | R | 0.744 | R | 0.669 |
表4
未来50a气候要素变化预估结果"
预估年数 | 10a | 20a | 30a | 40a | 50a | 未来50a 变率/10a |
---|---|---|---|---|---|---|
预估年份 | 2013-2022 | 2023-2032 | 2033-2042 | 2043-2052 | 2053-2062 | |
年降水量/mm | 664.845 5 | 696.612 1 | 660.637 9 | 689.148 8 | 755.739 1 | 14.729 0 |
年平均绝对湿度/(mg/L) | 7.072 0 | 7.173 0 | 7.189 0 | 7.257 0 | 7.311 0 | 0.060 0 |
年平均相对湿度/% | 65.819 0 | 65.115 0 | 63.497 0 | 63.604 0 | 61.981 0 | -0.960 0 |
年霜日/d | 139.647 0 | 134.549 0 | 133.642 0 | 125.293 0 | 128.380 0 | -2.817 0 |
表6
香格里拉气候环境系统耦合关系结构方程模型回归结果"
被解释变量 | 解释变量 | 系数 | 标准差 | Z | P>|z| | 95%的置信区间 | R | ||
---|---|---|---|---|---|---|---|---|---|
结构方程 | 绝对湿度 | 降水 | 0.175** | 0.075 | 2.34 | 0.019 | 0.028 | 0.322 | 0.66 |
气温 | 0.631*** | 0.054 | 11.73 | 0.000 | 0.526 | 0.737 | |||
常数项 | 26.090*** | 2.926 | 8.92 | 0.000 | 20.355 | 31.826 | |||
相对湿度 | 降水 | 0.210*** | 0.069 | 3.05 | 0.002 | 0.075 | 0.345 | 0.76 | |
气温 | -0.738*** | 0.043 | -17.11 | 0.000 | -0.823 | -0.654 | |||
常数项 | 37.411*** | 2.068 | 18.09 | 0.000 | 33.357 | 41.464 | |||
霜日 | 绝对湿度 | -0.298** | 0.132 | -2.25 | 0.024 | -0.557 | -0.039 | 0.56 | |
降水 | -0.175* | 0.101 | -1.74 | 0.083 | -0.373 | 0.023 | |||
气温 | -0.267** | 0.116 | -2.30 | 0.022 | -0.494 | -0.039 | |||
常数项 | 25.231*** | 3.340 | 7.55 | 0.000 | 18.679 | 31.785 | |||
残差的协方差 | 相对湿度与绝对湿度 | 0.843*** | 0.039 | 21.57 | 0.000 | 0.766 | 0.919 |
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