| DQR ID | Subject | Data Streams Affected |
|---|---|---|
| D090508.1 | GRW/ECOR/M1 - Reprocessed: ECOR Wind direction offset corrected | grw30ecorM1.b1 |
| D110118.2 | GRW/ECOR/M1 - Effects on ECOR CO2 Flux and Concentration By Aircraft | grw30ecorM1.b1 |
| Start Date | Start Time | End Date | End Time |
|---|---|---|---|
| 04/15/2009 | 1530 | 05/08/2009 | 1830 |
| Subject: | GRW/ECOR/M1 - Reprocessed: ECOR Wind direction offset corrected |
| DataStreams: | grw30ecorM1.b1 |
| Description: | The ECOR sonic anemometer was initially aligned to an east declination instead of a west declination. For the period stated, ECOR wind direction was 21 degrees too high. Data were reprocessed 20090602 and archived 20090619. |
| Measurements: | grw30ecorM1.b1:
|
| Start Date | Start Time | End Date | End Time |
|---|---|---|---|
| 04/15/2009 | 1530 | 10/11/2010 | 0800 |
| Subject: | GRW/ECOR/M1 - Effects on ECOR CO2 Flux and Concentration By Aircraft |
| DataStreams: | grw30ecorM1.b1 |
| Description: | Aircraft landings, departures, and running aircraft on the airport pad
were found to produce spikes in the half hourly CO2 flux and small spikes in CO2
concentration on many days during the entire deployment of the AMF1 at GRW. This influence
sometimes occurred multiple periods in a day;
this was typical of the year of data. The spikes range from only several micromoles s-1
m-2 to one hundred or more for flux (a typical spike was in the twenties) and near zero to
1.0 mmoles m-3 for CO2 concentration (typically around 0.15).
Occasionally an influence on water vapor density was detected, but this was fairly rare
and usually of very small magnitude.
----------------------------------------
DQR DATASTREAM(S):
grw30ecorM1.b1
cvar_rot_uc
cvar_rot_vc
cvar_rot_wc
cvar_tc
cvar_uc
cvar_vc
cvar_wc
fc
mean_c
var_c |
| Measurements: | grw30ecorM1.b1:
|