At which timescale does the complementary principle perform best in evaporation estimation?
<p>The complementary principle has been widely used to estimate evaporation under different conditions. However, it remains unclear at which timescale the complementary principle performs best. In this study, evaporation estimations were conducted at 88 eddy covariance (EC) monitoring sites at...
Main Authors: | , , |
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Format: | Article |
Language: | English |
Published: |
Copernicus Publications
2021-01-01
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Series: | Hydrology and Earth System Sciences |
Online Access: | https://hess.copernicus.org/articles/25/375/2021/hess-25-375-2021.pdf |
Summary: | <p>The complementary principle has been widely used to estimate evaporation
under different conditions. However, it remains unclear at which timescale
the complementary principle performs best. In this study, evaporation
estimations were conducted at 88 eddy covariance (EC) monitoring sites at
multiple timescales (daily, weekly, monthly, and yearly) by using sigmoid
and polynomial generalized complementary functions. The results indicate
that the generalized complementary functions exhibit the highest skill in
estimating evaporation at the monthly scale. The uncertainty analysis shows
that this conclusion is not affected by ecosystem type or energy balance
closure method. Through comparisons at multiple timescales, we found that
the slight difference between the two generalized complementary functions
only exists when the independent variable (<span class="inline-formula"><i>x</i></span>) in the functions approaches 1.
The results differ for the two models at daily and weekly scales. However,
such differences vanish at monthly and annual timescales, with few high <span class="inline-formula"><i>x</i></span>
values occurring. This study demonstrates the applicability of generalized
complementary functions across multiple timescales and provides a reference
for choosing a suitable time step for evaporation estimations in relevant
studies.</p> |
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ISSN: | 1027-5606 1607-7938 |