The accumulation defined as ''precipitation minus evaporation'' over Greenland has been simulated with the high-resolution limited-area regional climate model HIRHAM4 applied over an Arctic integration domain. This simulation is compared with a revised estimate of annual accumulation rate distribution over Greenland taking into account information from a new set of ice core analyses, based on surface sample collections from the North Greenland Traverse. The region with accumulation rates below 150 mm yr Ϫ1 in central-northwest Greenland is much larger than previously assumed and extends about 500 km farther to the south. It is demonstrated that good agreement between modeled and observed regional precipitation and accumulation patterns exists, particularly concerning the location and the values of very low accumulation in the middle of Greenland. The accumulation rates in the northern part of Greenland are reduced in comparison to previous estimates. These minima are connected with a prevailing blocking high over the Greenland ice sheet and katabatic wind systems preventing humidity transports to central Greenland. The model reasonably represents the synoptic situations that lead to precipitation. Maxima of precipitation and accumulation occur at the southwestern and southeastern coasts of Greenland and are connected with cyclonic activity and the main storm tracks around Greenland. The central region of the Greenland ice sheet acts as a blocking barrier on moving weather systems and prohibits cyclones moving from west to east across this region and, thus prevents moisture transports.
Abstract. This paper presents a comparison of two independent methods of estimating subseasonal accumulation across the interior of Greenland. These methods, highresolution snow pit studies and atmospheric modeling, have differing spatial and temporal resolution, but both can estimate net accumulation for subseasonal and shorter periods. The snow pit approach is based on a documented relationship between high-resolution snow pit profiles of oxygen stable isotope ratio (8•SO) and multiyear Special Sensor
Since 1933 in the Rostov region, the official registration of tularemia began. In 1964-1949 the highest incidence was noted. Since 1947, they have been vaccinated against tularemia. In 1966 to 1973, there were no cases of tularemia. In July-August 1993, a large outbreak of tularemia (more than 200 people) was recorded. Until early 2017, the epidemic situation in tularemia in the Rostov region, according to the data of long-term monitoring, was assessed as stable, but low coverage with vaccinations against tularemia, both in the population of endemic territories and in individuals of certain professional categories was recorded. In january 2017, two residents of Rostov-on-Don received a clinical diagnosis of «tularemia». In june and july 2017, three cases of tularemia were reported. The most effective mechanism for preventing the spread of tularemia remains vaccination of the population from the contingent of risk. We consider it advisable to conduct studies of the immunity to tularemia in the population vaccinated in the last five years, to significantly increase the reliability of short- and long-term prognosis for tularemia in the region.
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