Articles | Volume 22, issue 4
https://doi.org/10.5194/hess-22-2311-2018
https://doi.org/10.5194/hess-22-2311-2018
Research article
 | Highlight paper
 | 
18 Apr 2018
Research article | Highlight paper |  | 18 Apr 2018

Regional evapotranspiration from an image-based implementation of the Surface Temperature Initiated Closure (STIC1.2) model and its validation across an aridity gradient in the conterminous US

Nishan Bhattarai, Kaniska Mallick, Nathaniel A. Brunsell, Ge Sun, and Meha Jain

Download

Interactive discussion

Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
Printer-friendly Version - Printer-friendly version Supplement - Supplement

Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
ED: Reconsider after major revisions (further review by editor and referees) (12 Feb 2018) by Bob Su
AR by Nishan Bhattarai on behalf of the Authors (12 Feb 2018)  Author's response   Manuscript 
ED: Referee Nomination & Report Request started (12 Feb 2018) by Bob Su
RR by Anonymous Referee #1 (13 Feb 2018)
RR by Anonymous Referee #3 (10 Mar 2018)
ED: Publish subject to minor revisions (review by editor) (10 Mar 2018) by Bob Su
AR by Nishan Bhattarai on behalf of the Authors (19 Mar 2018)  Author's response   Manuscript 
ED: Publish as is (19 Mar 2018) by Bob Su
AR by Nishan Bhattarai on behalf of the Authors (20 Mar 2018)
Download
Short summary
We report the first ever regional-scale implementation of the Surface Temperature Initiated Closure (STIC1.2) model for mapping evapotranspiration (ET) using MODIS land surface and gridded climate datasets to overcome the existing uncertainties in aerodynamic temperature and conductance estimation in global ET models. Validation and intercomparison with SEBS and MOD16 products across an aridity gradient in the US manifested better ET mapping potential of STIC1.2 in different climates and biomes.