Glimpses of light snow appeared over Moscow on the night of November 16, reported through a Telegram channel by Evgeny Tishkovets, a leading expert at the Phobos meteorological center. He described the snowfall as a brief but noticeable change in the capital’s weather pattern, captured by observers and official stations alike.
According to Tishkovets, snowfall began around 6:00 at the Moscow weather station VDNKh. Across the Moscow region, the snow persisted for about half a day and was logged by meteorological stations in Pavlovsky Posad, Domodedovo, Sheremetyevo, Volokolamsk, Klin, Kolomna, and Cherusty. The combined readings from these areas suggested a coordinated, though modest, winter signal entering the metropolitan area and its surroundings.
During the night, the minimum temperature in the city hovered near the freezing mark, with values around +1.3°C reported in Moscow proper. In some outlying districts, however, temperatures dipped to around -1.7°C, signaling the first chilly pockets of the season as frosts began to bite in the soil and on exposed surfaces.
Earlier forecasts from forecaster Alexander Ilyin hinted at a transition toward colder conditions approaching the weekend. He suggested that frost and snow would start to make themselves felt in Moscow, marking the onset of the capital’s winter mood. The forecast noted that temperatures would briefly remain above freezing in the daytime up to November 16, then fall below it as night fell.
Based on the latest updates, daytime temperatures on November 16 were anticipated to range roughly from 0°C to +2°C, with nighttime readings dipping to around -1°C. These figures, published by multiple monitoring sites, aligned with the general expectation of a cooler shift as late autumn deepened, a pattern often observed as early-season soil cooling and dew point changes begin to influence the air mass over the city.
Looking ahead, forecasters anticipated an even more pronounced drop in temperatures on November 17. The day was forecast to bring a clear trend toward noticeably colder conditions, with daytime highs near -1°C to -6°C and nighttime temperatures possibly reaching around -4°C. Such a swing would emphasize the transition from late autumn to the first true winter feel for the capital and the surrounding region, accompanied by a higher likelihood of frost formation, ice on surfaces, and the need for early-day precautions by residents and travelers alike.
In terms of regional impact, meteorologists stressed that the cold air would accumulate gradually, with microclimates around lakes, rivers, and open plain areas experiencing more pronounced temperature dips. The variance between central Moscow and outer districts could become more noticeable with continued clear skies and light winds during the night, a scenario commonly seen in late autumn. Observers also noted that the Arctic warming phenomena discussed in broader climate discussions could influence the persistence and intensity of these early-season cold spells, though the current pattern remains consistent with typical November behavior for the region. Continued monitoring is advised as weather models are refined and more data comes in from ground stations and satellite analyses. For residents, practical tips include preparing for slippery road conditions, ensuring adequate heating safety checks, and keeping outdoor spaces ready for sudden temperature swings, rain, or light snow flurries that may occur in the coming days. This sequence of events underscores the importance of staying informed through trusted meteorological sources and adjusting daily plans accordingly. (Source: Phobos meteorological center)
Previous discussions about climate patterns, including inquiries into how Arctic warming may influence global weather, remain a context for understanding these fluctuations. The current observations provide a concrete example of how regional temperatures respond to shifting air masses and seasonal transitions, reinforcing the value of continuous weather monitoring as winter approaches. (Citation: regional meteorological analyses and ongoing climate research)