基于遥感和gis地统计模型的地下水增强型降雨径流估算

IF 3.2 3区 地球科学 Q1 Environmental Science
Pradeep Kamaraj, Deepa Subramani, Dmitry E. Kucher, Muhammad Aslam, Yahia Said, Aqil Tariq
{"title":"基于遥感和gis地统计模型的地下水增强型降雨径流估算","authors":"Pradeep Kamaraj,&nbsp;Deepa Subramani,&nbsp;Dmitry E. Kucher,&nbsp;Muhammad Aslam,&nbsp;Yahia Said,&nbsp;Aqil Tariq","doi":"10.1002/hyp.70180","DOIUrl":null,"url":null,"abstract":"<div>\n \n <p>Groundwater decline in any region is a significant issue that has been rising daily. Rainfall and runoff assessment of the area gives groundwater management and sustainability ideas since the arid regions rely mainly on rainfall for groundwater recharge. Therefore, rainfall-runoff is one of the necessary studies to implement groundwater recharge. This study primarily focuses on rainfall-runoff estimation with the help of Geographic Information System (GIS) techniques. Three input variables, topographic, remote sensing, and Antecedent Moisture Condition (AMC), were adopted to define this Soil Conservation Service—Curve Number (SCS-CN) model. Texture-based soil categorization was used to create the hydrologic soil group (HSG) map. The dominance of D-type HSG was categorised as a high runoff region. The 10 years (2006–2015) of rainfall information were used to generate the rainfall spatial map based on the Theissen-Polygon method. The rainfall-runoff data shows that the higher rainfall (1477.5 mm) and runoff (470.8 mm) during 2007. The Land Use and Land Cover (LULC) map was created through the Indian Remote Sensing Satellite P6's Linear Imaging Self-Scanning Sensor-IIi (IRS-P6 LISS-III) image. In dry, normal, and wet circumstances, the corresponding curve numbers (CN) values were CN 1 = 62.3, CN 2 = 79.03, and CN 3 = 89.8. In addition, the mean surface runoff was calculated as 330.2 mm with an average runoff volume of 164.13 mm<sup>3</sup>, which was 13.91% of the overall average rainfall. The final results (rainfall and runoff) also strongly correlated (<i>r</i> = 0.857). Thus, this study can be a basis for many researchers in various water resource management studies.</p>\n </div>","PeriodicalId":13189,"journal":{"name":"Hydrological Processes","volume":"39 6","pages":""},"PeriodicalIF":3.2000,"publicationDate":"2025-06-16","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Rainfall-Runoff Estimation for Groundwater Enhancement Through Remote Sensing and GIS-Based Geostatistical Model\",\"authors\":\"Pradeep Kamaraj,&nbsp;Deepa Subramani,&nbsp;Dmitry E. Kucher,&nbsp;Muhammad Aslam,&nbsp;Yahia Said,&nbsp;Aqil Tariq\",\"doi\":\"10.1002/hyp.70180\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div>\\n \\n <p>Groundwater decline in any region is a significant issue that has been rising daily. Rainfall and runoff assessment of the area gives groundwater management and sustainability ideas since the arid regions rely mainly on rainfall for groundwater recharge. Therefore, rainfall-runoff is one of the necessary studies to implement groundwater recharge. This study primarily focuses on rainfall-runoff estimation with the help of Geographic Information System (GIS) techniques. Three input variables, topographic, remote sensing, and Antecedent Moisture Condition (AMC), were adopted to define this Soil Conservation Service—Curve Number (SCS-CN) model. Texture-based soil categorization was used to create the hydrologic soil group (HSG) map. The dominance of D-type HSG was categorised as a high runoff region. The 10 years (2006–2015) of rainfall information were used to generate the rainfall spatial map based on the Theissen-Polygon method. The rainfall-runoff data shows that the higher rainfall (1477.5 mm) and runoff (470.8 mm) during 2007. The Land Use and Land Cover (LULC) map was created through the Indian Remote Sensing Satellite P6's Linear Imaging Self-Scanning Sensor-IIi (IRS-P6 LISS-III) image. In dry, normal, and wet circumstances, the corresponding curve numbers (CN) values were CN 1 = 62.3, CN 2 = 79.03, and CN 3 = 89.8. In addition, the mean surface runoff was calculated as 330.2 mm with an average runoff volume of 164.13 mm<sup>3</sup>, which was 13.91% of the overall average rainfall. The final results (rainfall and runoff) also strongly correlated (<i>r</i> = 0.857). Thus, this study can be a basis for many researchers in various water resource management studies.</p>\\n </div>\",\"PeriodicalId\":13189,\"journal\":{\"name\":\"Hydrological Processes\",\"volume\":\"39 6\",\"pages\":\"\"},\"PeriodicalIF\":3.2000,\"publicationDate\":\"2025-06-16\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Hydrological Processes\",\"FirstCategoryId\":\"89\",\"ListUrlMain\":\"https://onlinelibrary.wiley.com/doi/10.1002/hyp.70180\",\"RegionNum\":3,\"RegionCategory\":\"地球科学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q1\",\"JCRName\":\"Environmental Science\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Hydrological Processes","FirstCategoryId":"89","ListUrlMain":"https://onlinelibrary.wiley.com/doi/10.1002/hyp.70180","RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q1","JCRName":"Environmental Science","Score":null,"Total":0}
引用次数: 0

摘要

任何地区的地下水下降都是一个日益严重的重大问题。该地区的降雨和径流评估为地下水管理和可持续性提供了思路,因为干旱地区主要依靠降雨来补给地下水。因此,降雨径流是实施地下水补给的必要研究之一。本研究主要集中于利用地理信息系统(GIS)技术估算降雨径流。采用地形、遥感和先行水分条件3个输入变量定义土壤保持服务曲线数(SCS-CN)模型。采用基于纹理的土壤分类方法创建水文土壤类群(HSG)图。以d型HSG为主的地区被划分为高径流区。利用2006-2015年10年的降水信息,基于Theissen-Polygon方法生成降水空间图。降雨径流量数据显示,2007年降水量(1477.5 mm)和径流量(470.8 mm)较高。土地利用和土地覆盖(LULC)地图是通过印度遥感卫星P6的线性成像自扫描传感器- iii (IRS-P6 LISS-III)图像创建的。在干燥、正常和潮湿情况下,相应的曲线数(CN)值为cn1 = 62.3, cn2 = 79.03, cn3 = 89.8。平均地表径流量为330.2 mm,平均径流量为164.13 mm3,占总平均降雨量的13.91%。最终结果(降雨和径流)也是强相关的(r = 0.857)。因此,本研究可作为许多研究者开展各种水资源管理研究的基础。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Rainfall-Runoff Estimation for Groundwater Enhancement Through Remote Sensing and GIS-Based Geostatistical Model

Groundwater decline in any region is a significant issue that has been rising daily. Rainfall and runoff assessment of the area gives groundwater management and sustainability ideas since the arid regions rely mainly on rainfall for groundwater recharge. Therefore, rainfall-runoff is one of the necessary studies to implement groundwater recharge. This study primarily focuses on rainfall-runoff estimation with the help of Geographic Information System (GIS) techniques. Three input variables, topographic, remote sensing, and Antecedent Moisture Condition (AMC), were adopted to define this Soil Conservation Service—Curve Number (SCS-CN) model. Texture-based soil categorization was used to create the hydrologic soil group (HSG) map. The dominance of D-type HSG was categorised as a high runoff region. The 10 years (2006–2015) of rainfall information were used to generate the rainfall spatial map based on the Theissen-Polygon method. The rainfall-runoff data shows that the higher rainfall (1477.5 mm) and runoff (470.8 mm) during 2007. The Land Use and Land Cover (LULC) map was created through the Indian Remote Sensing Satellite P6's Linear Imaging Self-Scanning Sensor-IIi (IRS-P6 LISS-III) image. In dry, normal, and wet circumstances, the corresponding curve numbers (CN) values were CN 1 = 62.3, CN 2 = 79.03, and CN 3 = 89.8. In addition, the mean surface runoff was calculated as 330.2 mm with an average runoff volume of 164.13 mm3, which was 13.91% of the overall average rainfall. The final results (rainfall and runoff) also strongly correlated (r = 0.857). Thus, this study can be a basis for many researchers in various water resource management studies.

求助全文
通过发布文献求助,成功后即可免费获取论文全文。 去求助
来源期刊
Hydrological Processes
Hydrological Processes 环境科学-水资源
CiteScore
6.00
自引率
12.50%
发文量
313
审稿时长
2-4 weeks
期刊介绍: Hydrological Processes is an international journal that publishes original scientific papers advancing understanding of the mechanisms underlying the movement and storage of water in the environment, and the interaction of water with geological, biogeochemical, atmospheric and ecological systems. Not all papers related to water resources are appropriate for submission to this journal; rather we seek papers that clearly articulate the role(s) of hydrological processes.
×
引用
GB/T 7714-2015
复制
MLA
复制
APA
复制
导出至
BibTeX EndNote RefMan NoteFirst NoteExpress
×
提示
您的信息不完整,为了账户安全,请先补充。
现在去补充
×
提示
您因"违规操作"
具体请查看互助需知
我知道了
×
提示
确定
请完成安全验证×
copy
已复制链接
快去分享给好友吧!
我知道了
右上角分享
点击右上角分享
0
联系我们:info@booksci.cn Book学术提供免费学术资源搜索服务,方便国内外学者检索中英文文献。致力于提供最便捷和优质的服务体验。 Copyright © 2023 布克学术 All rights reserved.
京ICP备2023020795号-1
ghs 京公网安备 11010802042870号
Book学术文献互助
Book学术文献互助群
群 号:604180095
Book学术官方微信