Research article
27 Jan 2017
Research article
| 27 Jan 2017
Response of water vapour D-excess to land–atmosphere interactions in a semi-arid environment
Stephen D. Parkes et al.
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Cited
11 citations as recorded by crossref.
- Water fluxes mediated by vegetation: emerging isotopic insights at the soil and atmosphere interfaces M. Dubbert & C. Werner 10.1111/nph.15547
- Seasonal Patterns of Water Cycling in a Deep, Continental Mountain Valley Inferred From Stable Water Vapor Isotopes R. Fiorella et al. 10.1029/2017JD028093
- Spatial Shift of Aridity and Its Impact on Land Use of Syria M. Houmsi et al. 10.3390/su11247047
- Enhancing Understanding of the Hydrological Cycle via Pairing of Process‐Oriented and Isotope Ratio Tracers R. Fiorella et al. 10.1029/2021MS002648
- Variations in water use strategies of sand-binding vegetation along a precipitation gradient in sandy regions, northern China X. Ma et al. 10.1016/j.jhydrol.2021.126539
- Novel Keeling-plot-based methods to estimate the isotopic composition of ambient water vapor Y. Yuan et al. 10.5194/hess-24-4491-2020
- Assessing moisture sources of precipitation in the Western Pamir Mountains (Tajikistan, Central Asia) using deuterium excess T. Juhlke et al. 10.1080/16000889.2019.1601987
- Dryland climate change: Recent progress and challenges J. Huang et al. 10.1002/2016RG000550
- The utility of near-surface water vapor deuterium excess as an indicator of atmospheric moisture source Z. Wei & X. Lee 10.1016/j.jhydrol.2019.123923
- The role of dew and radiation fog inputs in the local water cycling of a temperate grassland during dry spells in central Europe Y. Li et al. 10.5194/hess-25-2617-2021
- Variation characteristics of stable isotopes in precipitation and the environmental factors that influence them in the Shiyang River Basin of China W. Jia et al. 10.1007/s12665-019-8307-z
10 citations as recorded by crossref.
- Water fluxes mediated by vegetation: emerging isotopic insights at the soil and atmosphere interfaces M. Dubbert & C. Werner 10.1111/nph.15547
- Seasonal Patterns of Water Cycling in a Deep, Continental Mountain Valley Inferred From Stable Water Vapor Isotopes R. Fiorella et al. 10.1029/2017JD028093
- Spatial Shift of Aridity and Its Impact on Land Use of Syria M. Houmsi et al. 10.3390/su11247047
- Enhancing Understanding of the Hydrological Cycle via Pairing of Process‐Oriented and Isotope Ratio Tracers R. Fiorella et al. 10.1029/2021MS002648
- Variations in water use strategies of sand-binding vegetation along a precipitation gradient in sandy regions, northern China X. Ma et al. 10.1016/j.jhydrol.2021.126539
- Novel Keeling-plot-based methods to estimate the isotopic composition of ambient water vapor Y. Yuan et al. 10.5194/hess-24-4491-2020
- Assessing moisture sources of precipitation in the Western Pamir Mountains (Tajikistan, Central Asia) using deuterium excess T. Juhlke et al. 10.1080/16000889.2019.1601987
- Dryland climate change: Recent progress and challenges J. Huang et al. 10.1002/2016RG000550
- The utility of near-surface water vapor deuterium excess as an indicator of atmospheric moisture source Z. Wei & X. Lee 10.1016/j.jhydrol.2019.123923
- The role of dew and radiation fog inputs in the local water cycling of a temperate grassland during dry spells in central Europe Y. Li et al. 10.5194/hess-25-2617-2021
Latest update: 01 Jul 2022
Short summary
Determining atmospheric moisture sources is required for understanding the water cycle. The role of land surface fluxes is a particular source of uncertainty for moisture budgets. Water vapour isotopes have the potential to improve constraints on moisture sources. In this work relationships between water vapour isotopes and land–atmosphere exchange are studied. Results show that land surface evaporative fluxes play a minor role in the daytime water and isotope budgets in semi-arid environments.
Determining atmospheric moisture sources is required for understanding the water cycle. The role...