HR: 0800h
AN: U41A-0811 [Abstracts]
TI: Comprehensive Bias-free Precipitation Archive for Northern Eurasia: What it Can Declare About Changes
in the Arctic Fresh Water System?
AU: Razuvaev, V
EM: razuvaev@meteo.ru
AF: Russian Institute for Hydrometeorological Information, 6 Koroleva Street, Obninsk, 249020
Russian Federation
AU: * Groisman, P Y
EM: Pasha.Groisman@noaa.gov
AF: UCAR Project Scientist at NCDC, NCDC, Federal Building, 151 Patton Avenue, Asheville, NC 28801
United States
AU: Bulygina, O N
EM: bulygina@meteo.ru
AF: Russian Institute for Hydrometeorological Information, 6 Koroleva Street, Obninsk, 249020
Russian Federation
AU: Bogdanova, E G
EM: bilijn@main.mgo.rssi.ru
AF: Main Geophysical Observatory, 7 Karbysheva Street, St. Petersburg, 194021
Russian Federation
AU: Ilijn, B M
EM: bilijn@main.mgo.rssi.ru
AF: Main Geophysical Observatory, 7 Karbysheva Street, St. Petersburg, 194021
Russian Federation
AU: Enloe, J G
EM: jesse.enloe@noaa.gov
AF: STG, Inc., Federal Building, 151 Patton Avenue, Asheville, NC 28801
United States
AU: Yarosh, E S
EM: evgeney.yarosh@noaa.gov
AF: STG, Inc., Federal Building, 151 Patton Avenue, Asheville, NC 28801
United States
AB:
Recently, we compiled, preprocessed, and released for the scientific community an archive of in situ daily, 6-hourly, and
half-daily precipitation for the former USSR at 2188 stations for the period 1891 to 2001 (NCDC Data Set 9813). The archive
was compiled within the framework of several joint projects of All-Russian Research Institute for Hydrometeorological
Information-World Data Center and Main Geophysical Observatory of the Federal Service for Hydrometeorology and Environmental
Monitoring, Obninsk, Russian Federation, and NOAA National Climatic Data Center, Asheville, North Carolina. Variables in the
data set include (1) raw daily precipitation, (2) homogenized daily precipitation using the Groisman and Rankova, (2001,
Internat. J. Climatol.) technique, (3) comprehensively corrected daily precipitation using a technique developed by Bogdanova
et al (2002a,b, J. Hydrometeorol. and Russian Meteorol. and Hydrol.), and (4) raw sub-daily synoptic precipitation. Mostly
Russian data are present in the archive after 1991. Comprehensive correction of precipitation measurements require
information about trace precipitation, precipitation type, wind speed, air temperature, humidity, atmospheric pressure, gauge
type, station exposure, snow cover, and previous day weather characteristics. Therefore, it was a laborious enterprise to
implement the Bogdanova et al. algorithm. But, the ongoing debate about the causes of runoff changes to the Arctic Ocean and
the needs of the climate modeling community require an urgent delivery of the input information to those who are in charge
of resolving this controversy. The algorithm implementation en masse, provides new features about both climatology and
variations of precipitation in the high latitudes of Northern Eurasia. They will be presented at the Meeting.
UR: http://www4.ncdc.noaa.gov/ol/documentlibrary/datasets.html
DE: 1655 Water cycles (1836)
DE: 3354 Precipitation (1854)
SC: Union [U]
MN: Fall Meeting 2005