Assessment of Different Complementary-Relationship-Based Models for Estimating Actual Terrestrial Evapotranspiration in the Frozen Ground Regions of the Qinghai-Tibet Plateau

Actual evapotranspiration (ETa) is important since it is an important link to water, energy, and carbon cycles. Approximately 96% of the Qinghai-Tibet Plateau (QTP) is underlain by frozen ground, however, the ground observations of ETa are particularly sparse–which is especially true in the permafro...

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Published in:Remote Sensing
Main Authors: Chengpeng Shang, Tonghua Wu, Ning Ma, Jiemin Wang, Xiangfei Li, Xiaofan Zhu, Tianye Wang, Guojie Hu, Ren Li, Sizhong Yang, Jie Chen, Jimin Yao, Cheng Yang
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2022
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Online Access:https://doi.org/10.3390/rs14092047
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author Chengpeng Shang
Tonghua Wu
Ning Ma
Jiemin Wang
Xiangfei Li
Xiaofan Zhu
Tianye Wang
Guojie Hu
Ren Li
Sizhong Yang
Jie Chen
Jimin Yao
Cheng Yang
author_facet Chengpeng Shang
Tonghua Wu
Ning Ma
Jiemin Wang
Xiangfei Li
Xiaofan Zhu
Tianye Wang
Guojie Hu
Ren Li
Sizhong Yang
Jie Chen
Jimin Yao
Cheng Yang
author_sort Chengpeng Shang
collection MDPI Open Access Publishing
container_issue 9
container_start_page 2047
container_title Remote Sensing
container_volume 14
description Actual evapotranspiration (ETa) is important since it is an important link to water, energy, and carbon cycles. Approximately 96% of the Qinghai-Tibet Plateau (QTP) is underlain by frozen ground, however, the ground observations of ETa are particularly sparse–which is especially true in the permafrost regions–leading to great challenge for the accurate estimation of ETa. Due to the impacts of freeze-thaw cycles and permafrost degradation on the regional ET process, it is therefore urgent and important to find a reasonable approach for ETa estimation in the regions. The complementary relationship (CR) approach is a potential method since it needs only routine meteorological variables to estimate ETa. The CR approach, including the modified advection-aridity model by Kahler (K2006), polynomial generalized complementary function by Brutsaert (B2015) and its improved versions by Szilagyi (S2017) and Crago (C2018), and sigmoid generalized complementary function by Han (H2018) in the present study, were assessed against in situ measured ETa at four observation sites in the frozen ground regions. The results indicate that five CR-based models are generally capable of simulating variations in ETa, whether default and calibrated parameter values are employed during the warm season compared with those of the cold season. On a daily basis, the C2018 model performed better than other CR-based models, as indicated by the highest Nash-Sutcliffe efficiency (NSE) and lowest root mean square error (RMSE) values at each site. On a monthly basis, no model uniformly performed best in a specific month. On an annual basis, CR-based models estimating ETa with biases ranging from −94.2 to 28.3 mm year−1, and the H2018 model overall performed best with the smallest bias within 15 mm year−1. Parameter sensitivity analysis demonstrated the relatively small influence of each parameter varying within regular fluctuation magnitude on the accuracy of the corresponding model.
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geographic Eta
Nash
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spelling ftmdpi:oai:mdpi.com:/2072-4292/14/9/2047/ 2025-01-17T00:15:49+00:00 Assessment of Different Complementary-Relationship-Based Models for Estimating Actual Terrestrial Evapotranspiration in the Frozen Ground Regions of the Qinghai-Tibet Plateau Chengpeng Shang Tonghua Wu Ning Ma Jiemin Wang Xiangfei Li Xiaofan Zhu Tianye Wang Guojie Hu Ren Li Sizhong Yang Jie Chen Jimin Yao Cheng Yang agris 2022-04-25 application/pdf https://doi.org/10.3390/rs14092047 EN eng Multidisciplinary Digital Publishing Institute Atmospheric Remote Sensing https://dx.doi.org/10.3390/rs14092047 https://creativecommons.org/licenses/by/4.0/ Remote Sensing; Volume 14; Issue 9; Pages: 2047 actual evapotranspiration complementary relationship permafrost seasonally frozen ground Qinghai-Tibet Plateau Text 2022 ftmdpi https://doi.org/10.3390/rs14092047 2023-08-01T04:51:39Z Actual evapotranspiration (ETa) is important since it is an important link to water, energy, and carbon cycles. Approximately 96% of the Qinghai-Tibet Plateau (QTP) is underlain by frozen ground, however, the ground observations of ETa are particularly sparse–which is especially true in the permafrost regions–leading to great challenge for the accurate estimation of ETa. Due to the impacts of freeze-thaw cycles and permafrost degradation on the regional ET process, it is therefore urgent and important to find a reasonable approach for ETa estimation in the regions. The complementary relationship (CR) approach is a potential method since it needs only routine meteorological variables to estimate ETa. The CR approach, including the modified advection-aridity model by Kahler (K2006), polynomial generalized complementary function by Brutsaert (B2015) and its improved versions by Szilagyi (S2017) and Crago (C2018), and sigmoid generalized complementary function by Han (H2018) in the present study, were assessed against in situ measured ETa at four observation sites in the frozen ground regions. The results indicate that five CR-based models are generally capable of simulating variations in ETa, whether default and calibrated parameter values are employed during the warm season compared with those of the cold season. On a daily basis, the C2018 model performed better than other CR-based models, as indicated by the highest Nash-Sutcliffe efficiency (NSE) and lowest root mean square error (RMSE) values at each site. On a monthly basis, no model uniformly performed best in a specific month. On an annual basis, CR-based models estimating ETa with biases ranging from −94.2 to 28.3 mm year−1, and the H2018 model overall performed best with the smallest bias within 15 mm year−1. Parameter sensitivity analysis demonstrated the relatively small influence of each parameter varying within regular fluctuation magnitude on the accuracy of the corresponding model. Text permafrost MDPI Open Access Publishing Eta ENVELOPE(-62.917,-62.917,-64.300,-64.300) Nash ENVELOPE(-62.350,-62.350,-74.233,-74.233) Sutcliffe ENVELOPE(-81.383,-81.383,50.683,50.683) Remote Sensing 14 9 2047
spellingShingle actual evapotranspiration
complementary relationship
permafrost
seasonally frozen ground
Qinghai-Tibet Plateau
Chengpeng Shang
Tonghua Wu
Ning Ma
Jiemin Wang
Xiangfei Li
Xiaofan Zhu
Tianye Wang
Guojie Hu
Ren Li
Sizhong Yang
Jie Chen
Jimin Yao
Cheng Yang
Assessment of Different Complementary-Relationship-Based Models for Estimating Actual Terrestrial Evapotranspiration in the Frozen Ground Regions of the Qinghai-Tibet Plateau
title Assessment of Different Complementary-Relationship-Based Models for Estimating Actual Terrestrial Evapotranspiration in the Frozen Ground Regions of the Qinghai-Tibet Plateau
title_full Assessment of Different Complementary-Relationship-Based Models for Estimating Actual Terrestrial Evapotranspiration in the Frozen Ground Regions of the Qinghai-Tibet Plateau
title_fullStr Assessment of Different Complementary-Relationship-Based Models for Estimating Actual Terrestrial Evapotranspiration in the Frozen Ground Regions of the Qinghai-Tibet Plateau
title_full_unstemmed Assessment of Different Complementary-Relationship-Based Models for Estimating Actual Terrestrial Evapotranspiration in the Frozen Ground Regions of the Qinghai-Tibet Plateau
title_short Assessment of Different Complementary-Relationship-Based Models for Estimating Actual Terrestrial Evapotranspiration in the Frozen Ground Regions of the Qinghai-Tibet Plateau
title_sort assessment of different complementary-relationship-based models for estimating actual terrestrial evapotranspiration in the frozen ground regions of the qinghai-tibet plateau
topic actual evapotranspiration
complementary relationship
permafrost
seasonally frozen ground
Qinghai-Tibet Plateau
topic_facet actual evapotranspiration
complementary relationship
permafrost
seasonally frozen ground
Qinghai-Tibet Plateau
url https://doi.org/10.3390/rs14092047