Access the full text.
Sign up today, get DeepDyve free for 14 days.
Loading next page...
/lp/wiley/catchment-scale-evaporation-and-the-atmospheric-boundary-layer-wRNkN7d6XY
References (72)
-
H. Bruin (1983)
A Model for the Priestley-Taylor ParameterJournal of Applied Meteorology
-
W. Brutsaert, H. Stricker (1979)
An advection‐aridity approach to estimate actual regional evapotranspirationJ. Climate Appl. Meteorol., 15
-
W. Brutsaert, F. Chan (1978)
Similarity functions D for water vapor in the unstable atmospheric boundary layerBoundary-Layer Meteorology, 14
-
A. Lindroth (1984)
Gradient distributions and flux profile relations above a rough forestJ. Geophys. Res., 110
-
A. S. Thom (1975)
Vegetation and the Atmosphere, Principles, 1
-
W. Brutsaert, H. Stricker (1979)
An advection-aridity approach to estimate actual regional evapotranspiration.Water Resources Research, 15
-
Y. Mintz (1982)
Land Surface Processes in Atmospheric General Circulation ModelsProc. R. Soc. London Ser. A
-
J. D. Hewlett, J. C. Fortson, G. B. Cunningham (1977)
The effect of rainfall intensity on storm flow and peak discharge from forest landQ. J. R. Meteorol. Soc., 13
-
W. Kustas, W. Brutsaert (1986)
Wind profile constants in a neutral atmospheric boundary layer over complex terrainBoundary-Layer Meteorology, 34
-
D. J. Carson (1982)
Land Surface Processes in Atmospheric General Circulation ModelsAgric. Meteorol.
-
B. B. Hicks, G. D. Hess, M. L. Wesely (1979)
Analysis of flux‐profile relationships above tall vegetation—An alternative viewBoundary Layer Meteorol., 105
-
K. M. Loague, R. A. Freeze (1985)
A comparison of rainfall‐runoff modeling techniques on small upland watershedsQ. J. R. Meteorol. Soc., 21
-
K. G. McNaughton (1976)
Evaporation and advection, I, Evaporation from extensive homogeneous surfacesJ. Hydraul. Div. Am. Soc. Civ. Eng., 102
-
M. Raupach, J. Stewart, A. Thom (1979)
Comments on the paper ‘Analysis of flux‐profile relationships above tall vegetation ‐ an alternative view’ by B. B. Hicks, G. D. Hess and M. L. Wesely (Q.J., 105, 1074–1077) IQuarterly Journal of the Royal Meteorological Society, 105
-
J. Melgarejo, J. Deardorff (1974)
Stability Functions for the Boundary-Layer Resistance Laws Based upon Observed Boundary-Layer HeightsJournal of the Atmospheric Sciences, 31
-
B. Fiedler (1984)
An Integral Closure Model for the Vertical Turbulent Flux of a Scalar in a Mixed LayerJournal of the Atmospheric Sciences, 41
-
A. Perrier (1980)
Météorologie et EnvironnementJ. Atmos. Sci.
-
J. Garratt (1978)
Flux profile relations above tall vegetationQuarterly Journal of the Royal Meteorological Society, 104
-
O. T. Denmead, I. C. McIlroy (1970)
Measurements of non‐potential evaporation from wheatQ. J. R. Meteorol. Soc., 7
-
H. L. Penman (1948)
Natural evaporation from open water, bare soil, and grassJ. Atmos. Sci., 193
-
A. Perrier (1982)
Land Surface Processes in Atmospheric General Circulation ModelsJ. Atmos. Sci.
-
J. L. Monteith (1981)
Evaporation and surface temperatureBoundary Layer Meteorol., 107
-
Clark Liu, W. Brutsaert (1978)
A nonlinear analysis of the relationship between rainfall and runoff for extreme floodsWater Resources Research, 14
-
W. Brutsaert (1982)
Evaporation into the Atmosphere: Theory, History and ApplicationsJ. Climate Appl. Meteorol.
-
Tetsuji Yamada (1976)
On the Similarity Functions A, B and C of the Planetary Boundary LayerJournal of the Atmospheric Sciences, 33
-
L. Mahrt, J. Andre (1983)
On the Stratification of Turbulent Mixed LayersJournal of Geophysical Research, 88
-
J. Garratt (1980)
Surface influence upon vertical profiles in the atmospheric near-surface layerQuarterly Journal of the Royal Meteorological Society, 106
-
R. A. Freeze (1975)
A stochastic‐conceptual analysis of one‐dimensional groundwater flow in nonuniform homogeneous mediaBoundary Layer Meteorol., 11
-
S. Zilitinkevich, J. Deardorff (1974)
Similarity Theory for the Planetary Boundary Layer of Time-Dependent HeightJournal of the Atmospheric Sciences, 31
-
H. A. R. DeBruin (1983)
A model for the Priestley‐Taylor parameter αWater Resour. Res., 22
-
J. Wyngaard, S. Arya, O. Coté (1974)
Some Aspects of the Structure of Convective Planetary Boundary LayersJournal of the Atmospheric Sciences, 31
-
S. Arya, J. Wyngaard (1975)
Effect of Baroclinicity on Wind Profiles and the Geostrophic Drag Law for the Convective Planetary Boundary LayerJournal of the Atmospheric Sciences, 32
-
Andre (1979)
Sur la distribution verticale de l'humidité dans une couche limite convectiveJ. Rech. Atmos., 13
-
J. Wyngaard, R. Brost (1984)
Top-down and bottom-up diffusion of a scalar in the convective boundary layerJournal of the Atmospheric Sciences, 41
-
J. A. Mawdsley, W. Brutsaert (1977)
Determination of regional evapotranspiration from upper air meteorological dataQ. J. R. Meteorol. Soc., 13
-
C. H. B. Priestley, R. J. Taylor (1972)
On the assessment of surface heat flux and evaporation using large‐scale parametersJ. Atmos. Sci., 100
-
S. Arya (1977)
Suggested Revisions to Certain Boundary Layer Parameterization Schemes Used in Atmospheric Circulation ModelsMonthly Weather Review, 105
-
L. Mahrt, J. C. Andre (1983)
On the stratification of turbulent mixed layersJ. Atmos. Sci., 88
-
J. L. Monteith (1973)
Principles of Environmental PhysicsMonth. Weather Rev.
-
P. Rowntree, J. Bolton (1983)
Simulation of the atmospheric response to soil moisture anomalies over EuropeQuarterly Journal of the Royal Meteorological Society, 109
-
S. Ishijima (1977)
Observational Studies on the Similarity Functions C and D of the Convective Planetary Boundary Layer over the OceanJournal of the Meteorological Society of Japan, 55
-
S. Ishijima (1977)
Observational studies on the similarity functions C and D of the convective planetary boundary layer over the oceanWater Resour. Res., 55
-
J. Wyngaard (1984)
Toward Convective Boundary Layer Parameterization: A Scalar Transport ModuleJournal of the Atmospheric Sciences, 41
-
J. R. Garratt (1978)
Flux‐profile relationships above tall vegetationQ. J. R. Meteorol. Soc., 104
-
J. R. Garratt (1980)
Surface influence upon vertical profiles in the atmospheric near‐surface layerWater Resour. Res., 106
-
H. Penman (1948)
Natural evaporation from open water, bare soil and grassProceedings of the Royal Society of London. Series A. Mathematical and Physical Sciences, 193
-
W. Brutsaert, J. A. Mawdsley (1976)
The applicability of planetary boundary layer theory to calculate regional evapotranspirationJ. Atmos. Sci., 12
-
E. L. Peck (1978)
Hydrometeorology, Bull. Am. Meteorol. Soc.Q. J. R. Meteorol. Soc., 59
-
B. Hicks, G. Hess, M. Wesely (1979)
Analysis of flux‐profile relationships above tall vegetation ‐ an alternative viewQuarterly Journal of the Royal Meteorological Society, 105
-
B. H. Fiedler (1984)
An integral closure model for the vertical turbulent flux of a scalar in a mixed layerQ. J. R. Meteorol. Soc., 41
-
D. Nielsen, J. Biggar, K. Erh (1973)
Spatial variability of field-measured soil-water properties, 42
-
R. Freeze (1975)
A stochastic‐conceptual analysis of one‐dimensional groundwater flow in nonuniform homogeneous mediaWater Resources Research, 11
-
A. Lindroth (1984)
Gradient distributions and flux profile relations above a rough forestQuarterly Journal of the Royal Meteorological Society, 110
-
R. Clarke, G. Hess (1973)
On the Appropriate Scaling for Velocity and Temperature in the Planetary Boundary LayerJournal of the Atmospheric Sciences, 30
-
F. Morton (1976)
Climatological Estimates of EvapotranspirationJournal of Hydraulic Engineering, 102
-
R. J. Bouchet (1963)
Evapotranspiration reelle et potentielle, signification climatique, PublBoundary Layer Meteorol., 62
-
K. Mcnaughton (1976)
Evaporation and advection I: evaporation from extensive homogeneous surfacesQuarterly Journal of the Royal Meteorological Society, 102
-
R. O. Slatyer, I. C. McIlroy (1967)
Practical Microclimatology -
P. R. Rowntree, J. A. Bolton (1983)
Simulation of the atmospheric response to soil moisture anomalies over EuropeIzv. Acad. Sci. USSR Atmos. Oceanic Phys., 109
-
K. Loague, R. Freeze (1985)
A Comparison of Rainfall-Runoff Modeling Techniques on Small Upland CatchmentsWater Resources Research, 21
-
M. Raupach (1979)
Anomalies in flux-gradient relationships over forestBoundary-Layer Meteorology, 16
-
O. Denmead, I. McIlroy (1970)
Measurements of non-potential evaporation from wheatAgricultural Meteorology, 7
-
C. Priestley, R. Taylor (1972)
On the Assessment of Surface Heat Flux and Evaporation Using Large-Scale ParametersMonthly Weather Review, 100
-
W. Brutsaert, W. Kustas (1985)
Evaporation and Humidity Profiles for Neutral Conditions over Rugged Hilly Terrain, 24
-
J. Garratt, R. Francey (1978)
Bulk characteristics of heat transfer in the unstable, baroclinic atmospheric boundary layerBoundary-Layer Meteorology, 15
-
S. S. Zilitinkevich, D. L. Laikhtman, A. S. Monin (1967)
Dynamics of the atmospheric boundary layer, 3
-
A. Thom, J. Stewart, H. Oliver, J. Gash (1975)
Comparison of aerodynamic and energy budget estimates of fluxes over a pine forestQuarterly Journal of the Royal Meteorological Society, 101
-
M. R. Raupach, J. B. Stewart, A. S. Thom (1979)
Comments on the paper “Analysis of flux‐profile relationships above tall vegetation—An alternative view,”Izv. Akad. Nauk SSSR Fiz. Atmos. Okeana, 105
-
J. Mawdsley, W. Brutsaert (1977)
Determination of regional evapotranspiration from upper air meteorological dataWater Resources Research, 13
-
F. I. Morton (1976)
Climatological estimates of evapotranspirationQ. J. R. Meteorol. Soc., 102
-
J. Hewlett, J. Fortson, G. Cunningham (1977)
The effect of rainfall intensity on storm flow and peak discharge from forest landWater Resources Research, 13
-
W. Brutsaert, J. Mawdsley (1976)
The applicability of planetary boundary layer theory to calculate regional evapotranspirationWater Resources Research, 12
- Publisher
- Wiley
- Copyright
- Copyright © 1986 Wiley Subscription Services, Inc., A Wiley Company
- ISSN
- 0043-1397
- eISSN
- 1944-7973
- DOI
- 10.1029/WR022i09Sp0039S
- Publisher site
- See Article on Publisher Site
Abstract
Evaporation is an important component of the hydrological cycle; for example, over land surfaces it amounts on average to about 60% of precipitation. This means that for hydrological purposes such as water budget calculations, the prediction or forecasting of floods and droughts, and for dynamic weather forecasting and climate modeling, it is indispensable to have reliable information on land surface evaporation. In mapping a strategy for this, decisions must be made regarding the scales at which this phenomenon is best parameterized. The atmosphere has the capacity of integrating and smoothing the effects of small‐scale irregularities over larger areas. Therefore a more thorough understanding of turbulent transport mechanisms in the atmospheric boundary layer should lead to improved parameterization methods of evaporation at the regional and watershed scale.
Journal
Water Resources Research – Wiley
Published: Aug 1, 1986