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渭河流域蒸散发时空反演及其对人类活动的响应

王丽霞 夏鹏宇 杨潇 潘飞燕 罗旭

水利水电技术(中英文)2023,Vol.54Issue(12):120-132,13.
水利水电技术(中英文)2023,Vol.54Issue(12):120-132,13.DOI:10.13928/j.cnki.wrahe.2023.12.010

渭河流域蒸散发时空反演及其对人类活动的响应

Spatial-temporal inversion of evapotranspiration in the Weihe River Basin and its response to human activities

王丽霞 1夏鹏宇 1杨潇 2潘飞燕 1罗旭1

作者信息

  • 1. 长安大学地质工程与测绘学院,陕西西安 710054
  • 2. 长安大学地球科学与资源学院,陕西西安 710054
  • 折叠

摘要

Abstract

[Objective]Human activities such as land use change,land engineering construction,and industrial and agricultural production have an important impact on surface evapotranspiration by changing the underlying surface properties,but the quanti-tative research on human driving forces is currently very limited.[Methods]Based on MODIS remote sensing images and meteor-ological data,the Surface Energy Balance System(SEBS)model and trend analysis method are used to explore the spatiotemporal evolution characteristics of evapotranspiration in the Weihe River Basin over a long time series from 2009 to 2019,and the response of evapotranspiration to human activities is quantitatively evaluated using the residual analysis method.[Results]The result showed that:(1)The fitting coefficients(R2),root-mean-square error(RMSE),and mean relative error(MRE)of evapotranspiration(ET)estimated by the SEBS model to the measured values obtained by the water balance method are 0.78,0.84 mm,and 34.1%,respectively.(2)From 2010 to 2018,the net decrease of cultivated land in the Weihe River Basin is about 1 622.5 km2,with a growth rate of-2.91%,mainly flowing into grassland;the net increase of construction land area is about 785.75 km2,with a growth rate of about 15.55%,mainly flowing into cultivated land,and the unused land had the least transfer.(3)The area where human activities have a promoting effect on ET in the Weihe River Basin accounts for about 45.41%of the total area,with the area where the contribution rate is above 80%accounting for about 30%;the area where hu-man activities have a suppressing effect on ET accounts for about 4.24%,with the contribution rate in the Guanzhong area above 80%.[Conclusion]The result show that:(1)The SEBS model has good applicability in the study area.(2)On the time scale,the actual evapotranspiration shows a fluctuating upward trend year by year,with a change rate of about 0.019 mm/a;on the spa-tial scale,the actual evapotranspiration shows a zonal distribution pattern of high in the southeast and low in the northwest.(3)During the study period,human activities has different driving effects on surface evapotranspiration,with the areas where evapo-transpiration is promoted mainly distributed in the middle reaches of the Jinghe,Beiluohe rivers and some areas upstream of the Weihe River,and the areas where evapotranspiration is suppressed mainly distribute in the Guanzhong area.

关键词

蒸散发/人类活动/SEBS模型/残差分析/渭河流域

Key words

evapotranspiration/human activities/SEBS model/residual analysis/Weihe River Basin

分类

天文与地球科学

引用本文复制引用

王丽霞,夏鹏宇,杨潇,潘飞燕,罗旭..渭河流域蒸散发时空反演及其对人类活动的响应[J].水利水电技术(中英文),2023,54(12):120-132,13.

基金项目

国家自然科学基金项目(41471452) (41471452)

陕西省自然科学基金项目(2021JM-161) (2021JM-161)

中央高校基本科研业务资助项目(300102269201,300102299206) (300102269201,300102299206)

水利水电技术(中英文)

OA北大核心CSTPCD

1000-0860

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