SALSA Poster:

Estimation of Evaporation Rates for Riparian Vegetation, Hipps et al.

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Estimation of Evaporation Rates for Riparian Vegetation

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L.E. Hipps (1), D. Cooper (2), W. Eichinger (3)

1 Utah State University, Logan, UT
2 Los Alamos National Lab, Los Alamos, NM
3 University of Iowa, Iowa City, IA

email: larry@claret.agsci.usu.edu


IMPORTANT ISSUE

Water Use By Riparian Vegetation In Southwest US

 

PROBLEM

Narrow and heterogeneous nature of corridor

Typical micrometeorological approaches may be confounded by complex nature of surface


depiction of riparian zone 

MICROMETEOROLOGICAL DIFFICULTIES

      • Boundary layer will likely only partially develop over narrow, rough surface
      • Large spatial variations in scalars and fluxes
      • May be significant lateral fluxes of water vapor
      • Available energy cannot be routinely measured


concept of water vapor


PROBLEM

Standard micrometeorological approaches not very appropriate for this non-ideal situation

GOAL

To devise a legitimate approach for estimation of E in such a system


average e = flux


idealized profiles of humidy


at any height z


average evaporation


Summer 1997 -- SALSA Study

Water Vapor Lidar

Measures spatial distribution of atmospheric humidity

Sited alternately east then west of zone

Tethered Balloon

Wind and temperature measured in lower 50 m with tethered balloon several times in study

If winds blow across corridor and along Lidar transect, equation can be used to estimate E


SUGGESTIONS FOR FUTURE WORK

      • Site towers at both sides of zone. Must be about 30 m tall
      • Mount set of temperature, humidity, and wind sensors at 6-8 levels on each tower
      • When winds blow across zone, equation can be solved for E


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Agricultural Research Service, Southwest Watershed Research Center.

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