Response of water vapour D-excess to land–atmosphere interactions in a semi-arid environment

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Response of water vapour D-excess to land–atmosphere interactions in a semi-arid environment is …
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scholarly articleQ13442814

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P356DOI10.5194/HESS-21-533-2017

P50authorAli ErshadiQ56578011
Matthew F. McCabeQ56578883
Lixin WangQ56579689
P2093author name stringScott Chambers
Stephen D. Parkes
Alan D. Griffiths
Alastair G. Williams
Josiah Strauss
Adrian Element
P2860cites workIsotopic Variations in Meteoric WatersQ28246821
GRIP deuterium excess reveals rapid and orbital-scale changes in Greenland moisture origin.Q30993404
Deuterium excess reveals diurnal sources of water vapor in forest air.Q33638613
Ground based radon-222 observations and their application to atmospheric studies.Q35832186
Deuterium excess in precipitation of Alpine regions - moisture recyclingQ42696418
Climatic controls on water vapor deuterium excess in the marine boundary layer of the North Atlantic based on 500 days of in situ, continuous measurementsQ56100205
Continuous measurements of atmospheric water vapour isotopes in western Siberia (Kourovka)Q56100208
Tibetan Plateau summer monsoon northward extent revealed by measurements of water stable isotopesQ56100622
Diagnosing the seasonal land–atmosphere correspondence over northern Australia: dependence on soil moisture state and correspondence strength definitionQ56576138
Regional climate simulation over Australia's Murray-Darling basin: A multitemporal assessmentQ56581321
Partitioning of evapotranspiration using a stable isotope technique in an arid and high temperature agricultural production systemQ57453030
The patterns and implications of diurnal variations in the d-excess of plant water, shallow soil water and air moistureQ57453048
The GEWEX LandFlux project: evaluation of model evaporation using tower-based and globally gridded forcing dataQ57894369
On the use of radon for quantifying the effects of atmospheric stability on urban emissionsQ57894856
Water isotope variations in the global ocean model MPI-OMQ58047046
Where Does the Irrigation Water Go? An Estimate of the Contribution of Irrigation to Precipitation Using MERRAQ58068164
Water extraction times for plant and soil materials used in stable isotope analysisQ58116285
Partitioning evapotranspiration – Testing the Craig and Gordon model with field measurements of oxygen isotope ratios of evaporative fluxesQ58242791
Moisture sources and synoptic to seasonal variability of North Atlantic water vapor isotopic compositionQ58265451
Continuous monitoring of summer surface water vapor isotopic composition above the Greenland Ice SheetQ58265478
Evidence of deuterium excess in water vapor as an indicator of ocean surface conditionsQ58304078
Examining the relationship between intermediate-scale soil moisture and terrestrial evaporation within a semi-arid grasslandQ58392717
Calibration of a land surface model using multiple data setsQ58392862
Deuterium excess as a proxy for continental moisture recycling and plant transpirationQ58413339
The nocturnal water cycle in an open-canopy forestQ58646372
P275copyright licenseCreative Commons Attribution 3.0 UnportedQ14947546
P6216copyright statuscopyrightedQ50423863
P433issue1
P921main subjectatmosphereQ8104
drylandsQ5309708
atmospheric water vaporQ39590365
P304page(s)533-548
P577publication date2017-01-27
P1433published inHydrology and Earth System SciencesQ15755050
P1476titleResponse of water vapour D-excess to land–atmosphere interactions in a semi-arid environment
P478volume21

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cites work (P2860)
Q57445762Dryland climate change: Recent progress and challenges
Q62552880Seasonal Patterns of Water Cycling in a Deep, Continental Mountain Valley Inferred From Stable Water Vapor Isotopes

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