气候与水文

近59 a锡林河流域潜在蒸散发及地表干湿状况变化趋势分析

展开
  • 1 内蒙古农业大学水利与土木建筑工程学院,内蒙古 呼和浩特 010018;
    2 陕西省水文水资源勘测局,陕西 西安 710068
张璐(1995–),女,硕士研究生,主要从事干旱半干旱区生态水文研究. E-mail:971568173@qq.com

收稿日期: 2019-06-18

  修回日期: 2019-11-04

  网络出版日期: 2020-11-18

基金资助

国家自然科学基金项目(51779116); 地区科学基金项目(51669018,51869015)资助

Trends of potential evapotranspiration and surface wet conditions in the Xilin River Basin in recent 59 years

Expand
  • 1 College of Water Resources and Civil Engineering,Inner Mongolia Agricultural University,Hohhot 010018,Inner Mongolia, China;
    2 Shaanxi Provincial Bureau of Hydrology and Water Resources Survey,Xi’an 710068,Shaanxi, China

Received date: 2019-06-18

  Revised date: 2019-11-04

  Online published: 2020-11-18

摘要

利用1960—2018年锡林河流域周边13个气象站的逐日气象资料,采用世界粮农组织(Food and Agriculture Organization of the United Nations,FAO)推荐的Penman-Monteith公式计算各气象站多年潜在蒸散发量及相对湿润度指数。通过利用主成分分析、相关分析和偏相关分析,探讨了锡林河流域潜在蒸散发、地表干湿状况多年变化规律;分析了影响潜在蒸散发的主要气象因子及各气象要素间的相互作用;着重讨论了锡林河流域潜在蒸散发的周期变化及其与相对湿润度指数、各气象要素的相互作用。结果表明:流域近59 a潜在蒸散发整体呈现增长趋势,且上升趋势显著,存在显著增加—减小交替的多尺度时频变化特征和多主周期变化规律;各气象要素中潜在蒸散发对温度的响应较大,平均风速次之;平均相对湿度受到潜在蒸散发的影响较大,降水次之。整个流域环境有不显著的变湿润趋势。

本文引用格式

张璐, 朱仲元, 张圣微, 王慧敏, 王飞, 席小康 . 近59 a锡林河流域潜在蒸散发及地表干湿状况变化趋势分析[J]. 干旱区地理, 2020 , 43(4) : 997 -1003 . DOI: 10.12118/j.issn.1000-6060.2020.04.14

Abstract

Using the daily meteorological data of the period from 1960 to 2018, which were obtained from 13 meteorological stations surrounding the Xilin River Basin,Inner Mongolia,China,the Penman-Monteith formula recommended by the Food and Agriculture Organization of the United Nations (FAO) was used to calculate the multiyear potential evapotranspiration and relative humidity index in each weather station. The potential evapotranspiration and surface wet and dry conditions of the Xilin River Basin were explored over the aforementioned period through principal component,correlation,and partial correlation analyses. The cyclical changes in the potential evapotranspiration in the Xilin River Basin and their correlations to the relative humidity index and various meteorological elements were discussed. The results indicated that the potential evapotranspiration in the basin in recent 59 a exhibited a significant overall increasing trend. Significant increasing and decreasing trends were found among the characteristics of the multiscale time-frequency changes and multiperiod changes,respectively. The response was larger,followed by average wind speed. The average relative humidity followed by precipitation were the most affected by the potential evapotranspiration. The entire basin environment exhibited an insignificant tendency to become humid.

参考文献

[1] 高妍,冯起,李宗省,等. 1957—2012年讨赖河流域潜在蒸发量变化[J]. 中国沙漠,2014,34(4):1125–1132.
[GAO Yan,FENG Qi,LI Zongsheng,et al.Changes in potential evaporation in the Tanlai River Basin from 1957 to 2012[J]. China Desert,2014,34(4):1125–1132.]
[2] 韩盟伟,赵广举,穆兴民,等. 黄土高原1959—2015年潜在蒸发量的时空变化[J]. 干旱区地理,2017,40(5):997–1004.
[HAN Mengwei,ZHAO Guangju,MU Xingmin,et al.Temporal and spatial changes of potential evaporation in the Loess Plateau from 1959 to 2015[J]. Arid Land Geography,2017,40(5):997–1004.]
[3] 杨泽粟. 黄土高原植被生理过程和蒸散量计算方法及变化特征研究[D]. 兰州:兰州大学,2016.
[YANG Zesu.Study on physiological processes and evapotranspiration calculation methods and change characteristics of vegetation on the Loess Plateau[D]. Lanzhou:Lanzhou University,2016.]
[4] YANG Dawen,SUN Fubao,LIU Zhiyu,et al. Interpreting the complementary relationship in non-humid environments based on the Budyko and Penman hypotheses[J]. Geophysical Research Letters,2006,33(18):doi:10.1029/2006GL027657.
[5] 邵月红,刘永和,吴俊梅. 蒸散量双线性曲面回归模型的改进及验证[J]. 农业工程学报,2017,33(2):94–101.
[SHAO Yuehong,LIU Yonghe,WU Junmei.Improvement and validation of evapotranspiration bilinear surface regression model[J]. Transactions of the Chinese Society of Agricultural Engineering,2017,33(2):94–101.]
[6] GAO Y T,ZHAO C Y,ASHIQ M W,et al.Actual evapotranspiration of subalpine meadows in the Qilian Mountains,Northwest China[J]. Journal of Arid Land,2019,11(3):371–384.
[7] 宋小园,朱仲元,张圣微,等. 锡林河流域气候变化特征诊断分析[J]. 干旱区资源与环境,2016,30(4):151–158.
[SONG Xiaoyuan,ZHU Zhongyuan,ZHANG Shengwei,et al.Diagnosis and analysis of climate change characteristics in Xilin River Basin[J]. Journal of Arid Land Resources and Environment,2016,30(4):151–158.]
[8] 宋小园. 气候变化和人类活动影响下锡林河流域水文过程响应研究[D]. 呼和浩特:内蒙古农业大学,2016.
[SONG Xiaoyuan.Hydrological process response of Xilin River Basin under the influence of climate change and human activities[D]. Hohhot:Inner Mongolia Agricultural University,2016.]
[9] 郝祥云,朱仲元,宋小园,等. 近50 a锡林河流域极端天气事件及其与气候变化的联系[J]. 干旱区资源与环境,2017,31(7):114–120.
[HAO Xiangyun,ZHU Zhongyuan,SONG Xiaoyuan,et al.Extreme weather events in the Xilin River Basin and their relationship with climate change in the past 50 years[J]. Arid Land Resources and Environment,2017,31(7):114–120.]
[10] 王飞,朱仲元,张鹏,等. SRM融雪径流模型在锡林河流域的应用[J]. 干旱区研究,2019,36(3):575–581.
[WANG Fei,ZHU Zhongyuan,ZHANG Peng,et al.Application of SRM snowmelt runoff model in Xilin River Basin[J]. Arid Zone Research,2019,36(3):575–581.]
[11] 宋小园,朱仲元,焦玮,等. 数字滤波法在锡林河基流分割中的比较与应用[J]. 干旱区地理,2016,39(6):1319–1326.
[SONG Xiaoyuan,ZHU Zhongyuan,JIAO Wei,et al.Comparison and application of digital filtering methods in basement segmentation of Xilin River[J]. Arid Land Geography,2016,39(6):1319–1326.]
[12] 靳立亚,李静,王新,等. 近50 a来中国西北地区干湿状况时空分布[J]. 地理学报,2004,59(6):847–854.
[JIN Liya,LI Jing,WANG Xin,et al.Spatiotemporal distribution of dry and wet conditions in Northwest China in the past 50 years[J]. Acta Geographica Sinica,2004,59(6):847–854.]
[13] 张新时. 植被的PE(可能蒸散)指标与植被—气候分类(一)—几种主要方法与PEP程序介绍[J]. 植物生态学与地植物学学报,1989,13(1):1–9.
[ZHANG Xinshi.PE (Possible Evapotranspiration) indicators and vegetation-climatic classification of vegetation (I):Introduction of several main methods and PEP programs[J]. Journal of Plant Ecology and Geobotany,1989,13(1):1–9.]
[14] 王莺,李耀辉,姚玉璧,等. 石羊河流域地表干湿变化的时空分布特征[J]. 资源科学,2013,35(10):2112–2120.
[WANG Ying,LI Yaohui,YAO Yudi,et al.Spatiotemporal distribution characteristics of surface wet and dry changes in the Shiyang River Basin[J]. Resources Science,2013,35(10):2112–2120.]
[15] 王文圣,丁晶,向红莲. 小波分析在水文学中的应用研究及展望[J]. 水科学进展,2002,13(4):515–520.
[WANG Wensheng,DING Jing,XIANG Honglian.Application and prospect of wavelet analysis in hydrology[J]. Progress in Water Science,2002,13(4):515–520.]
[16] HE S G,WANG G A,Cook D F.Multivariate measurement system analysis in multisite testing:An online technique using principal component analysis[J]. Expert Systems With Applications,2011,38(12):14602–14608.
[17] GB/T20481–2017. 气象干旱等级[S]. 北京:中华人民共和国国家质量监督检验检疫总局,2017.
[GB/T20481–2017. Meteorological drought grade[S]. Beijing:General Administration of Quality Supervision,Inspection and Quarantine of the People's Republic of China,2017.]
[18] 杨建平,丁永建,陈仁升,等. 近50年来中国干湿气候界线的10年际波动[J]. 地理学报,2002,57(6):655–661.
[YANG Jianping,DING Yongjian,CHEN Rensheng,et al.Interdecadal fluctuations of the wet and dry climate boundary in China in the past 50 years[J]. Acta Geographica Sinica,2002,57(6):655–661.]
[19] 王慧敏,朱仲元. 锡林河流域1981—2016年干湿变化及其与温度的关系[J]. 水土保持研究,2019,26(1):178–191.
[WANG Huimin,ZHU Zhongyuan.Dry and wet changes in the Xilin River Basin from 1981 to 2016 and their relationship with temperature[J]. Research of Soil and Water Conservation,2019,26(1):178–191.]
[20] 李玮,刘廷玺,格日乐吐,等. 半干旱草原型流域不同时间尺度降水特征分析[J]. 干旱区地理,2017,40(2):304–312.
[LI Wei,LIU Tingxi,GE Riletu,et al.Analysis of precipitation characteristics at different time scales in semi-arid steppe watershed[J]. Arid Land Geography,2017,40(2):304–312.]
[21] 王海梅. 锡林郭勒地区气候变化规律与植被覆盖变化驱动机制研究[D]. 呼和浩特:内蒙古农业大学,2009.
[WANG Haimei.Study on climate change law and driving mechanism of vegetation cover change in Xilinguole area[D]. Hohhot:Inner Mongolia Agricultural University,2009.]
文章导航

/