Title: Data from Virtual Tall Towers
1Data from Virtual Tall TowersWhats Coming
Next
- David Tyndall
- Penn State Dept. of Meteorology
- ChEAS 2007
2- Talk Outline
- overview of virtual tall tower (VTT) methodology
- results from a few well-chosen sites
- future uses
- where this guy fits into the grander picture
3The VTT Method
- objective make an adjustment to near- surface
observations (30m) to get an estimate of
mid-CBL CO2 - note CBL -- BL must be convective!
- follows theory of Wyngaard Brost (1984)
assume
the vertical flux profile is linear
then
4The VTT Method
- assume that there are contributions from
surface flux (bottom-up) and entrainment flux
(top down) - pertinent parameters scalar surface flux,
w ( f heat flux, ABL height, T), h - via dimensional analysis
b
t
h1 ABL height cws vert flux _at_ surface cw1
vert flux _at_ ABL top
- summing top-down and bottom-up contributions
5The VTT Method
- assume cwtop (entrainment flux) constant
cwbottom (surface flux) - gb gt evalutated at WLEF
- ABL top found using empirical relation from Yi
et al. (2001) (ABL height from daily - integrated surface heat flux)
- application of VTT method requires accurate
precise measure of CO2, as well as CO2 flux,
ABL height, w
6VTT in Practice
- shakedown at WLEF applied VTT method to obs
taken at 30 m to predict 396 m CO2
WINTER
CORRECTIONS
RESIDUALS
7VTT in Practice
- shakedown at WLEF applied VTT method to obs
taken at 30 m to predict 396 m CO2
SPRING
CORRECTIONS
RESIDUALS
8VTT in Practice
- shakedown at WLEF applied VTT method to obs
taken at 30 m to predict 396 m CO2
SUMMER
CORRECTIONS
RESIDUALS
9VTT in Practice
- shakedown at WLEF applied VTT method to obs
taken at 30 m to predict 396 m CO2
FALL
CORRECTIONS
RESIDUALS
10VTT in Practice
- WLEF (1997 2003), obs 14m above canopy
11VTT in Practice
- Harvard Forest (1993 2004), obs 24m above canopy
12VTT in Practice
- NOBS (1994 2004), obs 17m above canopy
13VTT in Practice
- Hegyhatsal (2002 2005), obs 72m above canopy
14VTT Future Work
- other testbeds for VTT method?
- locations where low-level and upper-level CO2,
flux, met obs are available - Cabauw other tall towers?
- aircraft profiles?
- provide as data product
- for use as another
- constraint in inversions
- application to Ring II and
- other friendly inversions
15 Final Word where this guy fits in
- Meteo PhD candidate
- initially moved toward BL transport issues
- now moving toward BL-surface layer heterogeneity
interaction/dynamics and LES modelling
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17What are the values of gb gt?
- evalutated at WLEF tall tower using CO2 obs at
11 m, 30 m, 76 m, 122 m, 244 m, 396 m - best-fit functions found
Wang et al., in preparation
18What is the CBL height?
- CBL height found using Yi et al. (2001)
- empirical relationship developed using obs at
WLEF - ABL height a bG
- a 97.1 m
- b 25.5 m1/2/K1/2
Yi et al. 2001
19Corrections to Low-Level CO2 Measurements
Correction (ppm)
blue Harvard Forestred - WLEFgreen -
NOBSblue-green - Hegyhatsalblack - ARM-SGP
Year
20blue Harvard Forestred - WLEFgreen -
NOBSblue-green - Hegyhatsalblack - ARM-SGP
21Does it work at WLEF?
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26Does it work elsewhere?
Harvard Forest Corrections (1994 - 2004)
27Harvard Forest Corrected Mid-CBL CO2 (1994 -
2004)
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