{
  "fields": [{"id":"_id","type":"int"},{"id":"nome_misura","type":"text"},{"id":"desc_misura","type":"text"},{"id":"units","type":"text"}],
  "records": [
    [1,"Date","date and time, UTC time","yyyy-mm-dd hh:mm:ss"],
    [2,"Flux(10^-9 kg/sm2)","Daily fluxes are calculated from 2-hour average measurements. Ocean pCO2 data measured 5 m below water (di Sarra et al., 2023a)\r\nAtmospheric pCO2 obtained from ICOS atmospheric CO2 mixing ratio measurements carried out on the island available at https://www.icos-cp.eu.\r\nThe atmospheric CO2 partial pressure is obtained from the mixing ratio using the atmospheric pressure corrected using the water vapour partial pressure (estimated from sea surface temperature and salinity as described in Weiss and Price, 1980).\r\nSea temperature and salinity are measured 5 m below water (di Sarra et al., 2023b; di Sarra et al., 2023c)\r\nCO2 solubility is estimated using Weiss (1974).\r\nCO2 gas transfer velocity is computed using the Wanninkhof (2014) parameterization.\r\nWind speed is obtained from measurements carried out on the island (Sferlazzo et al., 2023).\r\nAs requested from the parameterization, averaged wind-speed over 15 m/s are discarded.\r\nUncertainty on the fluxes are computed using the linear approximation of the error propagation theory, using the python package uncertainties (Lebigot, 2023), starting from measurements accuracy and/or literature uncertanties on constants. ","10^-9 kg/sm2"],
    [3,"Flux_err(10^-9 kg/sm2)","","10^-9 kg/sm2"]
]}