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
|
|
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
|
|
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
|
|
|
|
|
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
|