Arkansas weather live radar5/6/2023 He asked: “Why are representatives of Russia still among you? What are they doing at UNESCO?” Zelenskyy said 540 “objects of cultural heritage, cultural institutions and religious buildings” in Ukraine have been damaged or destroyed since Russia invaded Feb. In a speech Tuesday to UNESCO, Ukrainian President Volodymyr Zelenskyy also announced that Ukraine has nominated the embattled Black Sea city of Odesa to be inscribed on the agency’s World Heritage list. The burial site was the second found in Lyman so far, Kyrylenko said, adding that initial investigations suggested the bodies had been buried by local residents and not by Russians. The bodies were Ukrainian soldiers who had been buried together in a mass grave, the head of the Donetsk region’s military administration, Pavlo Kyrylenko, said in Lyman on Tuesday.Īnother 22 civilians have been exhumed from individual graves at the burial site, located on the edge of a cemetery in a forested area on the outskirts of Lyman. Ten body bags lay beside a roughly 100-foot (30-meter) trench from which authorities said 32 bodies have been exhumed so far in the city in Ukraine’s eastern Donetsk region. It was part of an arduous effort to piece together evidence of what happened under more than four months of Russian occupation. Since hail can cause the rainfall estimates to be higher than what is actually occurring, steps are taken to prevent these high dBZ values from being converted to rainfall.LYMAN, Ukraine - Covered head-to-toe in protective suits, forensic workers pulled several bodies wrapped in black plastic from a mass grave Tuesday in Ukraine’s devastated city of Lyman. Hail is a good reflector of energy and will return very high dBZ values. These values are estimates of the rainfall per hour, updated each volume scan, with rainfall accumulated over time. Depending on the type of weather occurring and the area of the U.S., forecasters use a set of rainrates which are associated to the dBZ values. The higher the dBZ, the stronger the rainrate. Typically, light rain is occurring when the dBZ value reaches 20. The scale of dBZ values is also related to the intensity of rainfall. The value of the dBZ depends upon the mode the radar is in at the time the image was created. Notice the color on each scale remains the same in both operational modes, only the values change. The other scale (near left) represents dBZ values when the radar is in precipitation mode (dBZ values from 5 to 75). One scale (far left) represents dBZ values when the radar is in clear air mode (dBZ values from -28 to +28). Each reflectivity image you see includes one of two color scales. The dBZ values increase as the strength of the signal returned to the radar increases. So, a more convenient number for calculations and comparison, a decibel (or logarithmic) scale (dBZ), is used. Reflectivity (designated by the letter Z) covers a wide range of signals (from very weak to very strong). "Reflectivity" is the amount of transmitted power returned to the radar receiver. The colors are the different echo intensities (reflectivity) measured in dBZ (decibels of Z) during each elevation scan.
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