Articles | Volume 16, issue 2
https://doi.org/10.5194/essd-16-775-2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Special issue:
https://doi.org/10.5194/essd-16-775-2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Long-term monthly 0.05° terrestrial evapotranspiration dataset (1982–2018) for the Tibetan Plateau
Ling Yuan
State Key Laboratory of Tibetan Plateau Earth System, Environment and Resources (TPESER), Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing 100101, China
College of Earth and Planetary Sciences, University of Chinese Academy of Sciences, Beijing 100049, China
State Key Laboratory of Tibetan Plateau Earth System, Environment and Resources (TPESER), Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing 100101, China
National Observation and Research Station for Qomolongma Special Atmospheric Processes and Environmental Changes, Dingri 858200, China
China-Pakistan Joint Research Center on Earth Sciences, Chinese Academy of Sciences, Islamabad 45320, Pakistan
State Key Laboratory of Tibetan Plateau Earth System, Environment and Resources (TPESER), Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing 100101, China
College of Earth and Planetary Sciences, University of Chinese Academy of Sciences, Beijing 100049, China
College of Atmospheric Science, Lanzhou University, Lanzhou 730000, China
National Observation and Research Station for Qomolongma Special Atmospheric Processes and Environmental Changes, Dingri 858200, China
Kathmandu Center of Research and Education, Chinese Academy of Sciences, Beijing 100101, China
China-Pakistan Joint Research Center on Earth Sciences, Chinese Academy of Sciences, Islamabad 45320, Pakistan
Cunbo Han
State Key Laboratory of Tibetan Plateau Earth System, Environment and Resources (TPESER), Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing 100101, China
National Observation and Research Station for Qomolongma Special Atmospheric Processes and Environmental Changes, Dingri 858200, China
China-Pakistan Joint Research Center on Earth Sciences, Chinese Academy of Sciences, Islamabad 45320, Pakistan
Binbin Wang
State Key Laboratory of Tibetan Plateau Earth System, Environment and Resources (TPESER), Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing 100101, China
National Observation and Research Station for Qomolongma Special Atmospheric Processes and Environmental Changes, Dingri 858200, China
Kathmandu Center of Research and Education, Chinese Academy of Sciences, Beijing 100101, China
China-Pakistan Joint Research Center on Earth Sciences, Chinese Academy of Sciences, Islamabad 45320, Pakistan
Weiqiang Ma
State Key Laboratory of Tibetan Plateau Earth System, Environment and Resources (TPESER), Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing 100101, China
National Observation and Research Station for Qomolongma Special Atmospheric Processes and Environmental Changes, Dingri 858200, China
China-Pakistan Joint Research Center on Earth Sciences, Chinese Academy of Sciences, Islamabad 45320, Pakistan
Viewed
Total article views: 3,348 (including HTML, PDF, and XML)
Cumulative views and downloads
(calculated since 03 Aug 2022)
HTML | XML | Total | BibTeX | EndNote | |
---|---|---|---|---|---|
2,543 | 703 | 102 | 3,348 | 92 | 108 |
- HTML: 2,543
- PDF: 703
- XML: 102
- Total: 3,348
- BibTeX: 92
- EndNote: 108
Total article views: 1,877 (including HTML, PDF, and XML)
Cumulative views and downloads
(calculated since 06 Feb 2024)
HTML | XML | Total | BibTeX | EndNote | |
---|---|---|---|---|---|
1,469 | 342 | 66 | 1,877 | 69 | 79 |
- HTML: 1,469
- PDF: 342
- XML: 66
- Total: 1,877
- BibTeX: 69
- EndNote: 79
Total article views: 1,471 (including HTML, PDF, and XML)
Cumulative views and downloads
(calculated since 03 Aug 2022)
HTML | XML | Total | BibTeX | EndNote | |
---|---|---|---|---|---|
1,074 | 361 | 36 | 1,471 | 23 | 29 |
- HTML: 1,074
- PDF: 361
- XML: 36
- Total: 1,471
- BibTeX: 23
- EndNote: 29
Viewed (geographical distribution)
Total article views: 3,348 (including HTML, PDF, and XML)
Thereof 3,281 with geography defined
and 67 with unknown origin.
Total article views: 1,877 (including HTML, PDF, and XML)
Thereof 1,842 with geography defined
and 35 with unknown origin.
Total article views: 1,471 (including HTML, PDF, and XML)
Thereof 1,439 with geography defined
and 32 with unknown origin.
Country | # | Views | % |
---|
Country | # | Views | % |
---|
Country | # | Views | % |
---|
Total: | 0 |
HTML: | 0 |
PDF: | 0 |
XML: | 0 |
- 1
1
Total: | 0 |
HTML: | 0 |
PDF: | 0 |
XML: | 0 |
- 1
1
Total: | 0 |
HTML: | 0 |
PDF: | 0 |
XML: | 0 |
- 1
1
Cited
8 citations as recorded by crossref.
- Systematic analyses of the meteorological forcing and process parameterization uncertainties in modeling runoff with Noah-MP for the Upper Brahmaputra river basin X. Lei et al. 10.1016/j.jhydrol.2025.132686
- How much water vapour does the Tibetan Plateau release into the atmosphere? C. Zheng et al. 10.5194/hess-29-485-2025
- Temporal and spatial variations in evapotranspiration on the northern slope of the Kunlun Mountains based on multi-source datasets Y. Zhang et al. 10.1016/j.rcar.2025.02.006
- Analysis of land-atmosphere interactions and their influence on the energy and water cycle over the Tibetan Plateau Y. Ma et al. 10.1080/10095020.2024.2372504
- The energy-limited water loss of an alpine shrubland on the northeastern Qinghai-Tibetan Plateau, China F. Zhang et al. 10.1016/j.ejrh.2024.101905
- Principal Component Analysis (PCA) and feature importance-based dimension reduction for Reference Evapotranspiration (ET0) predictions of Taif, Saudi Arabia R. Bashir et al. 10.1016/j.compag.2024.109036
- Innovative approach for estimating evapotranspiration and gross primary productivity by integrating land data assimilation, machine learning, and multi-source observations X. He et al. 10.1016/j.agrformet.2024.110136
- Asymmetric environmental responses on evapotranspiration in Tibetan Plateau grassland L. Ma et al. 10.1016/j.scitotenv.2025.178699
8 citations as recorded by crossref.
- Systematic analyses of the meteorological forcing and process parameterization uncertainties in modeling runoff with Noah-MP for the Upper Brahmaputra river basin X. Lei et al. 10.1016/j.jhydrol.2025.132686
- How much water vapour does the Tibetan Plateau release into the atmosphere? C. Zheng et al. 10.5194/hess-29-485-2025
- Temporal and spatial variations in evapotranspiration on the northern slope of the Kunlun Mountains based on multi-source datasets Y. Zhang et al. 10.1016/j.rcar.2025.02.006
- Analysis of land-atmosphere interactions and their influence on the energy and water cycle over the Tibetan Plateau Y. Ma et al. 10.1080/10095020.2024.2372504
- The energy-limited water loss of an alpine shrubland on the northeastern Qinghai-Tibetan Plateau, China F. Zhang et al. 10.1016/j.ejrh.2024.101905
- Principal Component Analysis (PCA) and feature importance-based dimension reduction for Reference Evapotranspiration (ET0) predictions of Taif, Saudi Arabia R. Bashir et al. 10.1016/j.compag.2024.109036
- Innovative approach for estimating evapotranspiration and gross primary productivity by integrating land data assimilation, machine learning, and multi-source observations X. He et al. 10.1016/j.agrformet.2024.110136
- Asymmetric environmental responses on evapotranspiration in Tibetan Plateau grassland L. Ma et al. 10.1016/j.scitotenv.2025.178699
Latest update: 08 Mar 2025
Short summary
Accurately monitoring and understanding the spatial–temporal variability of evapotranspiration (ET) components over the Tibetan Plateau (TP) remains difficult. Here, 37 years (1982–2018) of monthly ET component data for the TP was produced, and the data are consistent with measurements. The annual average ET for the TP was about 0.93 (± 0.037) × 103 Gt yr−1. The rate of increase of the ET was around 0.96 mm yr−1. The increase in the ET can be explained by warming and wetting of the climate.
Accurately monitoring and understanding the spatial–temporal variability of evapotranspiration...
Special issue
Altmetrics
Final-revised paper
Preprint