Use of MODIS satellite data and energy balance to estimate evapotranspiration

Authors

  • Jesús Enrique López Avendaño Universidad Autónoma de Sinaloa-Facultad de Agronomía. Carretera Culiacán-El dorado, km 17.5. Culiacán, Sinaloa. CP. 80000. Tel. (667) 8461084.
  • Tomás Díaz Valdés Universidad Autónoma de Sinaloa-Facultad de Agronomía. Carretera Culiacán-El dorado, km 17.5. Culiacán, Sinaloa. CP. 80000. Tel. (667) 8461084
  • Christopher Watts Thorp Universidad de Sonora. Boulevard Luis Encinas y Rosales S/N. Col. Centro, Hermosillo, Sonora. CP. 83000. Tel. (662) 2592108, 2592169, 5960297
  • Julio César Rodríguez Universidad de Sonora. Boulevard Luis Encinas y Rosales S/N. Col. Centro, Hermosillo, Sonora. CP. 83000. Tel. (662) 2592108, 2592169, 5960297
  • Teresa de Jesús Velázquez Alcaráz Universidad Autónoma de Sinaloa-Facultad de Agronomía. Carretera Culiacán-El dorado, km 17.5. Culiacán, Sinaloa. CP. 80000. Tel. (667) 8461084
  • Leopoldo Partida Ruvalcaba Universidad Tecnológica de Culiacán. Corredor Culiacán-Imala, Culiacán, Sinaloa. CP. 80014. Tel. (667) 1041599

DOI:

https://doi.org/10.29312/remexca.v8i4.6

Keywords:

Bell pepper, scintilometer method, triangular space method, vortex covariance system

Abstract

Evapotranspiration (ET) is an important factor for the  development and production of agricultural crops,  its value at local and regional level is determinant  for planning the management of water resources;  some techniques such as vortex covariance measure  evapotranspiration in a space-determined manner,  while others, such as those based on remote sensing and  scintilometry, do it on a regional scale. The objective  was to estimate ET using MODIS sensor data and an  energy balance, and to compare it against data obtained  with scintillometer and vortex covariance system. The  study was implemented in Culiacán Valley, México, on  a surface of Bell pepper crop, during 81 days of crop  development. Normalized difference index (NDVI)  and surface temperature data from the MODIS sensor, a  BLS450 scintillometer to estimate sensible heat flux, and  an IRGA EC-150 vortex covariance system to measure  latent heat flux, were used. The total ET obtained was  255.4, 275.2 and 262 mm for MODIS, scintiloter and  covariance of vortices, respectively; (RMSE), BIAS,  Willmottʼs concordance coefficient (d), and correlation  coefficient (R) were 0.44 mm d-1, -0.245 mm d-1, 0.8 y 0.75, respectively. The use of satellite data combined with  the energy balance on the land surface allows a reliable  estimation of evapotranspiration at a regional scale. 

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Published

2017-08-03

How to Cite

López Avendaño Jesús Enrique, Díaz Valdés Tomás, Christopher Watts Thorp, Rodríguez Julio César, Velázquez Alcaráz Teresa de Jesús, and Leopoldo Partida Ruvalcaba. 2017. “Use of MODIS Satellite Data and Energy Balance to Estimate Evapotranspiration”. Revista Mexicana De Ciencias Agrícolas 8 (4). México, ME:773-84. https://doi.org/10.29312/remexca.v8i4.6.

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