Abstract. This study examines the consistency and
representativeness differences of daily integrated water vapour (IWV) data
from ERA-Interim reanalysis and GPS observations at 120 global sites over a
16-year period (1995–2010). Various comparison statistics are analysed as a
function of geographic, topographic, and climatic features. A small (±1 kg m−2) bias is found in the reanalysis across latitudes (moist in
northern and southern midlatitudes and dry in the tropics). The standard
deviation of daily IWV differences is generally below 2 kg m−2 but
peaks in the northern and southern storm-track regions. In general, the
larger IWV differences are explained by increased representativeness errors,
when GPS observations capture some small-scale variability that is not
resolved by the reanalysis. A representativeness error statistic is proposed
which measures the spatiotemporal variability in the vicinity of the GPS
sites, based on reanalysis data at the four surrounding grid points. It
allows to predict the standard deviation of daily IWV differences with a
correlation of 0.73. In general, representativeness differences can be
reduced by temporal averaging and spatial interpolation from the four
surrounding grid points. A small number of outlying cases (15 sites) which
do not follow the general tendencies are further examined. It is found that
their special topographic and climatic features strongly enhance the
representativeness errors (e.g. steep topography, coastlines, and strong
seasonal cycle in monsoon regions). Discarding these sites significantly
improves the global ERA-Interim and GPS comparison results. The selection of
sites a priori, based on the representativeness error statistic, is able to detect 11
out of the 15 sites and improve the comparison results by 20 % to 30 %.