Estimating Impacts of Agricultural Subsurface Drainage on Evapotranspiration Using the Landsat Imagery-Based METRIC Model

Agricultural subsurface drainage changes the field hydrology and potentially the amount of water available to the crop by altering the flow path and the rate and timing of water removal. Evapotranspiration (ET) is normally among the largest components of the field water budget, and the changes in ET...

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Main Authors: Kul Khand, Jeppe Kjaersgaard, Christopher Hay, Xinhua Jia
Format: Article
Language:English
Published: MDPI AG 2017-11-01
Series:Hydrology
Subjects:
Online Access:https://www.mdpi.com/2306-5338/4/4/49
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author Kul Khand
Jeppe Kjaersgaard
Christopher Hay
Xinhua Jia
author_facet Kul Khand
Jeppe Kjaersgaard
Christopher Hay
Xinhua Jia
author_sort Kul Khand
collection DOAJ
description Agricultural subsurface drainage changes the field hydrology and potentially the amount of water available to the crop by altering the flow path and the rate and timing of water removal. Evapotranspiration (ET) is normally among the largest components of the field water budget, and the changes in ET from the introduction of subsurface drainage are likely to have a greater influence on the overall water yield (surface runoff plus subsurface drainage) from subsurface drained (TD) fields compared to fields without subsurface drainage (UD). To test this hypothesis, we examined the impact of subsurface drainage on ET at two sites located in the Upper Midwest (North Dakota-Site 1 and South Dakota-Site 2) using the Landsat imagery-based METRIC (Mapping Evapotranspiration at high Resolution with Internalized Calibration) model. Site 1 was planted with corn (Zea mays L.) and soybean (Glycine max L.) during the 2009 and 2010 growing seasons, respectively. Site 2 was planted with corn for the 2013 growing season. During the corn growing seasons (2009 and 2013), differences between the total ET from TD and UD fields were less than 5 mm. For the soybean year (2010), ET from the UD field was 10% (53 mm) greater than that from the TD field. During the peak ET period from June to September for all study years, ET differences from TD and UD fields were within 15 mm (<3%). Overall, differences between daily ET from TD and UD fields were not statistically significant (p > 0.05) and showed no consistent relationship.
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spelling doaj.art-1a819b36db4b43c5a1e22f72a518d1ad2022-12-22T03:15:04ZengMDPI AGHydrology2306-53382017-11-01444910.3390/hydrology4040049hydrology4040049Estimating Impacts of Agricultural Subsurface Drainage on Evapotranspiration Using the Landsat Imagery-Based METRIC ModelKul Khand0Jeppe Kjaersgaard1Christopher Hay2Xinhua Jia3Biosystems & Agricultural Engineering Department, Oklahoma State University, Stillwater, OK 74078, USASouth Dakota Water Resources Institute, South Dakota State University, Brookings, SD 57007, USAIowa Soybean Association, Ankeny, IA 50023, USAAgricultural & Biosystems Engineering Department, North Dakota State University, Fargo, ND 58108, USAAgricultural subsurface drainage changes the field hydrology and potentially the amount of water available to the crop by altering the flow path and the rate and timing of water removal. Evapotranspiration (ET) is normally among the largest components of the field water budget, and the changes in ET from the introduction of subsurface drainage are likely to have a greater influence on the overall water yield (surface runoff plus subsurface drainage) from subsurface drained (TD) fields compared to fields without subsurface drainage (UD). To test this hypothesis, we examined the impact of subsurface drainage on ET at two sites located in the Upper Midwest (North Dakota-Site 1 and South Dakota-Site 2) using the Landsat imagery-based METRIC (Mapping Evapotranspiration at high Resolution with Internalized Calibration) model. Site 1 was planted with corn (Zea mays L.) and soybean (Glycine max L.) during the 2009 and 2010 growing seasons, respectively. Site 2 was planted with corn for the 2013 growing season. During the corn growing seasons (2009 and 2013), differences between the total ET from TD and UD fields were less than 5 mm. For the soybean year (2010), ET from the UD field was 10% (53 mm) greater than that from the TD field. During the peak ET period from June to September for all study years, ET differences from TD and UD fields were within 15 mm (<3%). Overall, differences between daily ET from TD and UD fields were not statistically significant (p > 0.05) and showed no consistent relationship.https://www.mdpi.com/2306-5338/4/4/49evapotranspirationsubsurface drainageremote sensingMETRIC
spellingShingle Kul Khand
Jeppe Kjaersgaard
Christopher Hay
Xinhua Jia
Estimating Impacts of Agricultural Subsurface Drainage on Evapotranspiration Using the Landsat Imagery-Based METRIC Model
Hydrology
evapotranspiration
subsurface drainage
remote sensing
METRIC
title Estimating Impacts of Agricultural Subsurface Drainage on Evapotranspiration Using the Landsat Imagery-Based METRIC Model
title_full Estimating Impacts of Agricultural Subsurface Drainage on Evapotranspiration Using the Landsat Imagery-Based METRIC Model
title_fullStr Estimating Impacts of Agricultural Subsurface Drainage on Evapotranspiration Using the Landsat Imagery-Based METRIC Model
title_full_unstemmed Estimating Impacts of Agricultural Subsurface Drainage on Evapotranspiration Using the Landsat Imagery-Based METRIC Model
title_short Estimating Impacts of Agricultural Subsurface Drainage on Evapotranspiration Using the Landsat Imagery-Based METRIC Model
title_sort estimating impacts of agricultural subsurface drainage on evapotranspiration using the landsat imagery based metric model
topic evapotranspiration
subsurface drainage
remote sensing
METRIC
url https://www.mdpi.com/2306-5338/4/4/49
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AT christopherhay estimatingimpactsofagriculturalsubsurfacedrainageonevapotranspirationusingthelandsatimagerybasedmetricmodel
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