Some considerations about the
Application of ogive analysis for quality control and spectral correction of eddy covariance fluxes
Christof Ammann, Albrecht Neftel
Content
Content
Motivation for spectral/ogive analysis: methodological flux measurement problems at the Swiss CarboEurope grassland site Some basics about ogives Application examples: High-frequency damping/correction Analysis for intermittency/stationarity of turbulence Conclusions
Site region
Measurement Site near Oensingen
0
N
annual distribution of wind directions
Site plots/fetch
Experimental Plots
200
0
N
150 100
EC systems
local SN scale [m]
Hi
50
g
y wa h
0
-50
- aerodyn. measurement height: z = 0.7 –1.2 m - sensor separation (lateral): s = 16 cm
-100
-150
-200 -300
-250
-200
-150
-100
-50
0
50
100
local WE scale [m]
Site wind
Nocturnal Wind Conditions
50.0 10
CO2 flux windspeed
8
CO2 flux [umol/m2/s]
windspeed ca. 1m above ground (Jun-Oct 2002)
6 0.0 4
frequency of occurrence [rel. units]
daytime nighttime
2
-50.0 20.07.2002 00:00
20.07.2002 12:00
21.07.2002 00:00
21.07.2002 12:00
22.07.2002 00:00
22.07.2002 12:00
0 23.07.2002 00:00
0
1
2
3
4
5
6
7
wind speed [m/s]
windspeed [m/s]
Site motivation
Motivation for spectral/ogive analysis
Relatively small fields low measurement height: strong high-frequency damping footprint problems (cf. talk by A. Neftel) Frequent calm nights weak/intermittent turbulence, non-stationary conditions enhanced dew formation (on open-path sensor)
? Are parameterised spectral models for the correction of high-frequency damping accurate enough? ? Are integral turbulence characteristics (e.g. /u*) specific enough for w optimum quality control?
Intro Ogive0
Wh tsa “ a i n ogive” ?
statistics: cumulative frequency distribution curve