Articles | Volume 24, issue 5
https://doi.org/10.5194/hess-24-2419-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/hess-24-2419-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
12 May 2020
Research article |
| 12 May 2020
| 12 May 2020
Tracking the global flows of atmospheric moisture and associated uncertainties
Copernicus Institute for Sustainable Development, Utrecht
University, 3508 TC Utrecht, the Netherlands
Stockholm Resilience Centre, Stockholm University,
10691 Stockholm, Sweden
Bolin Centre for Climate Research, 10691 Stockholm, Sweden
Arie Staal
Stockholm Resilience Centre, Stockholm University,
10691 Stockholm, Sweden
Bolin Centre for Climate Research, 10691 Stockholm, Sweden
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- The global potential of forest restoration for drought mitigation O. Tuinenburg et al. 10.1088/1748-9326/ac55b8
35 citations as recorded by crossref.
- Spatial distribution of oceanic moisture contributions to precipitation over the Tibetan Plateau Y. Li et al. 10.5194/hess-26-6413-2022
- Moisture sources of precipitation over the Pearl River Basin in South China X. Liu et al. 10.1002/joc.8447
- Quantifying the Fingerprint of Oceanic Moisture Source Conditions in Deuterium and 17O Excess Parameters of Precipitation Z. Xia 10.1029/2022GL101901
- Fate and Changes in Moisture Evaporated From the Tibetan Plateau (2000–2020) C. Zhang et al. 10.1029/2022WR034165
- African rainforest moisture contribution to continental agricultural water consumption M. Nyasulu et al. 10.1016/j.agrformet.2023.109867
- Global water availability boosted by vegetation-driven changes in atmospheric moisture transport J. Cui et al. 10.1038/s41561-022-01061-7
- Critical transitions in the Amazon forest system B. Flores et al. 10.1038/s41586-023-06970-0
- Forests buffer against variations in precipitation J. O'Connor et al. 10.1111/gcb.15763
- Atmospheric and Land Surface Contributions to Heatwaves: An Australian Perspective A. Hirsch & M. King 10.1029/2020JD033223
- Changes in atmospheric moisture transport over tropical South America: an analysis under a climate change scenario P. Arias et al. 10.1007/s00382-023-06833-4
- The role of low‐level circulation on water vapour transport to central and northern South America: Insights from a 2D Lagrangian approach J. Morales et al. 10.1002/joc.6873
- Local moisture recycling across the globe J. Theeuwen et al. 10.5194/hess-27-1457-2023
- Network motifs shape distinct functioning of Earth’s moisture recycling hubs N. Wunderling et al. 10.1038/s41467-022-34229-1
- Moisture Source–Receptor Network of the East Asian Summer Monsoon Land Regions and the Associated Atmospheric Steerings T. Cheng & M. Lu 10.1175/JCLI-D-19-0868.1
- Sustainable Agroforestry Landscape Management: Changing the Game M. van Noordwijk et al. 10.3390/land9080243
- Contributions of moisture sources to precipitation in the major drainage basins in the Tibetan Plateau Y. Li et al. 10.1007/s11430-021-9890-6
- Negligible Impact on Precipitation From a Permanent Inland Lake in Central Australia Z. Yang et al. 10.1029/2023GL103913
- Atmospheric moisture contribution to the growing season in the Amazon arc of deforestation J. O’Connor et al. 10.1088/1748-9326/ac12f0
- The Contribution of Transpiration to Precipitation Over African Watersheds S. Te Wierik et al. 10.1029/2021WR031721
- Global scenarios of irrigation water abstractions for bioenergy production: a systematic review F. Stenzel et al. 10.5194/hess-25-1711-2021
- Hydrological impacts of vegetation cover change in China through terrestrial moisture recycling D. Xie et al. 10.1016/j.scitotenv.2024.170015
- Comparing deuterium excess to large-scale precipitation recycling models in the tropics S. Cropper et al. 10.1038/s41612-021-00217-3
- A unified framework to estimate the origins of atmospheric moisture and heat using Lagrangian models J. Keune et al. 10.5194/gmd-15-1875-2022
- Characterizing potential sources and transport pathways of intense moisture during extreme precipitation events over the Tibetan Plateau O. Ayantobo et al. 10.1016/j.jhydrol.2022.128734
- Comparison of moisture sources of summer precipitation in 1998 and 2020 in the middle and lower reaches of Yangtze River basin J. Chen et al. 10.1002/joc.8040
- Shifts in regional water availability due to global tree restoration A. Hoek van Dijke et al. 10.1038/s41561-022-00935-0
- Moisture origins of the Amazon carbon source region A. Staal et al. 10.1088/1748-9326/acc676
- Comment on ‘The central role of forests in the 2021 European floods’ A. Staal & G. Koren 10.1088/1748-9326/acc260
- Irrigation of biomass plantations may globally increase water stress more than climate change F. Stenzel et al. 10.1038/s41467-021-21640-3
- Extreme precipitation events in the Mediterranean area: contrasting two different models for moisture source identification S. Cloux et al. 10.5194/hess-25-6465-2021
- On the moisture transport regimes for extreme precipitation over North China M. Zhang et al. 10.1016/j.atmosres.2024.107254
- Hysteresis of tropical forests in the 21st century A. Staal et al. 10.1038/s41467-020-18728-7
- High-resolution global atmospheric moisture connections from evaporation to precipitation O. Tuinenburg et al. 10.5194/essd-12-3177-2020
- Large‐Scale Afforestation Enhances Precipitation by Intensifying the Atmospheric Water Cycle Over the Chinese Loess Plateau L. Tian et al. 10.1029/2022JD036738
- The global potential of forest restoration for drought mitigation O. Tuinenburg et al. 10.1088/1748-9326/ac55b8
Latest update: 25 Apr 2024
Short summary
Several models exist to track water through the atmosphere from its evaporation location to the next rain location. These models are typically driven by atmospheric wind and humidity data. Recently, a new version of these driving data sets has become available, with a higher spatial resolution of about 25 km. Here, we test the assumptions of these atmospheric moisture tracking models, given the high-resolution forcing data and find that the vertical mixing assumptions are the most important.
Several models exist to track water through the atmosphere from its evaporation location to the...
