SGP/ECOR/E6  - Reprocess: Incorrectly flagged (marked as "bad") H2O/CO2 data

Due to system clock instability on ECOR computers their system time is adjusted 
approximately once per hour; sometimes this adjustment leads to backward time jumps over midnight, 
into the previous day. In this case all the data based on CO2/H2O measurements might be 
erroneously marked as bad. Below is a list of times when that might have happen.

SITE    YEAR    MONTH   DAY     HOUR    MINUTE
06      2004    06      14      00      00

null

• Rotated covariance wc(cvar_rot_wc)
• mean co2 concentration (c)(mean_c)
• rotated covariance uc(cvar_rot_uc)
• skewness of variable q(skew_q)
• Covariance qc(cvar_qc)
• mean value of out of range values and spikes of c -9999 if no spikes(mean_spk_c)
• number of valid q samples(n_good_q)
• covariance uq(cvar_uq)
• covariance wq(cvar_wq)
• Rotated covariance uq(cvar_rot_uq)
• variance of q(var_q)
• rotated covariance wq(cvar_rot_wq)
• covariance vc(cvar_vc)
• mean value of out of range values and spikes of q -9999 if no spikes(mean_spk_q)
• kurtosis of variable q(kurt_q)
• 0=real or 1=dummy value of cp(real_cp)
• Water vapor mixing ratio observed by the Raman lidar(mr)
• latent heat flux(lv_e)
• variance of c(var_c)
• Number of c samples removed due to spikes(n_spk_c)
• Latent heat of vaporization(lv)
• Status of source for mixing ratio(real_mr)
• Rotated covariance vc(cvar_rot_vc)
• Covariance tc(cvar_tc)
• covariance of tq(cvar_tq)
• Covariance vq(cvar_vq)
• kurtosis of variable c(kurt_c)
• Number of q samples removed due to spikes(n_spk_q)
• Number of bad or out of range q samples(n_bad_q)
• rotated covariance vq(cvar_rot_vq)
• mean water vapor concentration (q)(mean_q)
• CO2 flux(fc)
• moist air density(rho)
• Covariance uc(cvar_uc)
• Covariance wc(cvar_wc)
• Number of bad or out of range c samples(n_bad_c)
• number of valid c samples(n_good_c)
• skewness of variable c(skew_c)
• 0=real or 1=dummy value of rho(real_rho)
• Status of source for latent heat of vaporization(real_lv)