Abstract

This study aims to improve the standard water balance evapotranspiration (WB ET) estimate, which is typically used as benchmark data for catchment-scale ET estimation, by accounting for net intercatchment groundwater flow in the ET calculation. Using the modified WB ET approach, we examine errors and shortcomings associated with the long-term annual mean (2002–2014) spatial patterns of three remote-sensing (RS) MODIS-based ET products from MODIS16, PML_V2, and TSEB algorithms at 1 km spatial resolution over Denmark, as a test case for small-scale, energy-limited regions. Our results indicate that the novel approach of adding groundwater net in water balance ET calculation results in a more trustworthy ET spatial pattern. This is especially relevant for smaller catchments where groundwater net can be a significant component of the catchment water balance. Nevertheless, large discrepancies are observed both amongst RS ET datasets and compared to modified water balance ET spatial pattern at the national scale; however, catchment-scale analysis highlights that difference in RS ET and WB ET decreases with increasing catchment size and that 90%, 87%, and 93% of all catchments have ∆ET < ±150 mm/year for MODIS16, PML_V2, and TSEB, respectively. In addition, Copula approach captures a nonlinear structure of the joint relationship with multiple densities amongst the RS/WB ET products, showing a complex dependence structure (correlation); however, among the three RS ET datasets, MODIS16 ET shows a closer spatial pattern to the modified WB ET, as identified by a principal component analysis also. This study will help improve the water balance approach by the addition of groundwater net in the ET estimation and contribute to better understand the true correlations amongst RS/WB ET products especially over energy-limited environments.

Highlights

  • MODIS16 and PML_V2 show a very similar ET spatial patterns; they vary in terms of absolute values

  • The ET-WBQ spatial patterns indicated a significant inconsistency over Denmark, with an energy-limited environment; it was improved especially for smaller catchments, when GW-net data was included in the ET-WBQ-GW estimate

  • The two-source energy balance model (TSEB), MODIS16, and PML_V2 ET estimates varied largely compared to ETWBQ-GW ; as a result, a large discrepancy was observed amongst the ET products at the national scale of Denmark

Read more

Summary

Introduction

Evapotranspiration (ET) (or its energy equivalent term, latent heat flux LE) is the transfer of water from the Earth’s surface to the atmosphere via soil and water surface evaporation and plant transpiration. Terrestrial ET amounts to approximately 70% of the total land surface’s precipitation [1,2]. It constitutes a cornerstone variable in both the land surface energy and water budgets [3,4]. Evapotranspiration is difficult to observe and model over water-limited—and in particular, energy-limited environments; this is due to the complex interactions amongst the climate–land–surface variables and the plant–atmosphere system [5].

Objectives
Methods
Results
Conclusion
Full Text
Published version (Free)

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call