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, Deepa Subramani, Dmitry E. Kucher, Muhammad Aslam, Yahia Said, 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, Deepa Subramani, Dmitry E. Kucher, Muhammad Aslam, Yahia Said, 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}
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.
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.