The Tretyakov non-recording precipitation gauge has been used historic
ally as the official precipitation measurement instrument in the Russi
an (formerly the USSR) climatic and hydrological station network and i
n a number of other European countries. From 1986 to 1993, the accurac
y and performance of this gauge were evaluated during the WMO Solid Pr
ecipitation Measurement Intercomparison at 11 stations in Canada, the
USA, Russia, Germany, Finland, Romania and Croatia. The double fence i
ntercomparison reference (DFIR) was the reference standard used at all
the Intercomparison stations in the Intercomparison. The Intercompari
son data collected at the different sites are compatible with respect
to the catch ratio (measured/DFIR) for the same gauge, when compared u
sing mean wind speed at the height of the gauge orifice during the obs
ervation period. The Intercomparison data for the Tretyakov gauge were
compiled from measurements made at these WMO intercomparison sites. T
hese data represent a variety of climates, terrains and exposures. The
effects of environmental factors, such as wind speed, wind direction,
type of precipitation and temperature, on gauge catch ratios were inv
estigated. Wind speed was found to be the most important factor determ
ining the gauge catch and air temperature had a secondary effect when
precipitation was classified into snow, mixed and rain. The results of
the analysis of gauge catch ratio versus wind speed and temperature o
n a daily time step are presented for various types of precipitation.
Independent checks of the correction equations against the DFIR have b
een conducted at those Intercomparison stations and a good agreement (
difference less than 10%) has been obtained. The use of such adjustmen
t procedures should significantly improve the accuracy and homogeneity
of gauge-measured precipitation data over large regions of the former
USSR and central Europe.