Spatiotemporal analysis of crop water requirements in Lower Chenab Canal (LCC) Irrigation System for the better management of water resources

Agriculture production in Pakistan mainly depends on irrigation water, and about 90% of production relies on irrigation water. For better assessment and management of irrigation water requirements, an accurate estimation of evapotranspiration (ET) from agriculture area is essential. Also, ET is a ke...

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Veröffentlicht in:Arabian journal of geosciences 2021-03, Vol.14 (6), Article 424
Hauptverfasser: Usman, Muhammad, Hussain, Ejaz, Rabbani, Umair, Ghazi, Shahid, Irteza, Syed M., Gull, Shamaila
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container_title Arabian journal of geosciences
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creator Usman, Muhammad
Hussain, Ejaz
Rabbani, Umair
Ghazi, Shahid
Irteza, Syed M.
Gull, Shamaila
description Agriculture production in Pakistan mainly depends on irrigation water, and about 90% of production relies on irrigation water. For better assessment and management of irrigation water requirements, an accurate estimation of evapotranspiration (ET) from agriculture area is essential. Also, ET is a key climate variable linking water, energy, and carbon cycles. Conventional ET measurement techniques are point-based and representative of the local scale only. Satellite remote sensing with large area coverage and high temporal frequency provides measurements of several relevant biophysical parameters required for estimation of ET at regional scales. This study uses the Surface Energy Balance System (SEBS) model to calculate the daily actual ET (ET a ) across the Lower Chenab Canal (LCC) irrigation system using the MODIS data for clouds-free days. Land cover classification was used to study the temporal changes in ET for different crops. There is no flux tower in the study area for direct measurement of latent heat flux and sensible heat flux; SEBS model-derived ET a values were evaluated against reference crop ET (ET o ) that were calculated using FAO-56 Penman-Monteith method. SEBS-based ET a values were found to be lower compared to the referenced ET (ET o ). Higher ET o values were observed for a hypothetical reference crop that is well-watered and disease-free, unlike actual field conditions. Results showed ET a values are much closer to ET o in the winter season with the mean difference of 0.36 mm/day, while in the summer season, the mean difference was 1.5 mm/day. This study shows the potential of remote sensing–based derived ET a at high spatial and temporal resolution over heterogeneous crops instead of the point-based estimation methods. Mapping ET is also helpful for better understanding of hydrological processes because it is a major loss and its spatial and temporal quantification can help in water regulation and equitable distribution.
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For better assessment and management of irrigation water requirements, an accurate estimation of evapotranspiration (ET) from agriculture area is essential. Also, ET is a key climate variable linking water, energy, and carbon cycles. Conventional ET measurement techniques are point-based and representative of the local scale only. Satellite remote sensing with large area coverage and high temporal frequency provides measurements of several relevant biophysical parameters required for estimation of ET at regional scales. This study uses the Surface Energy Balance System (SEBS) model to calculate the daily actual ET (ET a ) across the Lower Chenab Canal (LCC) irrigation system using the MODIS data for clouds-free days. Land cover classification was used to study the temporal changes in ET for different crops. There is no flux tower in the study area for direct measurement of latent heat flux and sensible heat flux; SEBS model-derived ET a values were evaluated against reference crop ET (ET o ) that were calculated using FAO-56 Penman-Monteith method. SEBS-based ET a values were found to be lower compared to the referenced ET (ET o ). Higher ET o values were observed for a hypothetical reference crop that is well-watered and disease-free, unlike actual field conditions. Results showed ET a values are much closer to ET o in the winter season with the mean difference of 0.36 mm/day, while in the summer season, the mean difference was 1.5 mm/day. This study shows the potential of remote sensing–based derived ET a at high spatial and temporal resolution over heterogeneous crops instead of the point-based estimation methods. 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There is no flux tower in the study area for direct measurement of latent heat flux and sensible heat flux; SEBS model-derived ET a values were evaluated against reference crop ET (ET o ) that were calculated using FAO-56 Penman-Monteith method. SEBS-based ET a values were found to be lower compared to the referenced ET (ET o ). Higher ET o values were observed for a hypothetical reference crop that is well-watered and disease-free, unlike actual field conditions. Results showed ET a values are much closer to ET o in the winter season with the mean difference of 0.36 mm/day, while in the summer season, the mean difference was 1.5 mm/day. This study shows the potential of remote sensing–based derived ET a at high spatial and temporal resolution over heterogeneous crops instead of the point-based estimation methods. 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For better assessment and management of irrigation water requirements, an accurate estimation of evapotranspiration (ET) from agriculture area is essential. Also, ET is a key climate variable linking water, energy, and carbon cycles. Conventional ET measurement techniques are point-based and representative of the local scale only. Satellite remote sensing with large area coverage and high temporal frequency provides measurements of several relevant biophysical parameters required for estimation of ET at regional scales. This study uses the Surface Energy Balance System (SEBS) model to calculate the daily actual ET (ET a ) across the Lower Chenab Canal (LCC) irrigation system using the MODIS data for clouds-free days. Land cover classification was used to study the temporal changes in ET for different crops. There is no flux tower in the study area for direct measurement of latent heat flux and sensible heat flux; SEBS model-derived ET a values were evaluated against reference crop ET (ET o ) that were calculated using FAO-56 Penman-Monteith method. SEBS-based ET a values were found to be lower compared to the referenced ET (ET o ). Higher ET o values were observed for a hypothetical reference crop that is well-watered and disease-free, unlike actual field conditions. Results showed ET a values are much closer to ET o in the winter season with the mean difference of 0.36 mm/day, while in the summer season, the mean difference was 1.5 mm/day. This study shows the potential of remote sensing–based derived ET a at high spatial and temporal resolution over heterogeneous crops instead of the point-based estimation methods. Mapping ET is also helpful for better understanding of hydrological processes because it is a major loss and its spatial and temporal quantification can help in water regulation and equitable distribution.</abstract><cop>Cham</cop><pub>Springer International Publishing</pub><doi>10.1007/s12517-021-06758-4</doi></addata></record>
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subjects Agricultural production
Agriculture
Canals
Carbon cycle
Climate change
Crops
Earth and Environmental Science
Earth science
Earth Sciences
Energy balance
Enthalpy
Environmental regulations
Evapotranspiration
Fluctuations
Heat flux
Heat transfer
Hydrology
Irrigation
Irrigation systems
Irrigation water
Land cover
Latent heat
Measurement
Measurement techniques
Original Paper
Parameter estimation
Remote sensing
Sensible heat
Sensible heat transfer
Surface energy
Surface properties
Temporal resolution
Temporal variations
Water management
Water requirements
Water resources
Water resources management
title Spatiotemporal analysis of crop water requirements in Lower Chenab Canal (LCC) Irrigation System for the better management of water resources
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