Last updated: January 18, 2025
The climate of Arkhangelskaya, Russian Federation, is classified under the Köppen-Geiger system as Dfc, indicative of a subarctic climate characterized by significant seasonal temperature variations. The region experiences extreme cold in January, with minimum temperatures plummeting to -46°C (-51°F), while the summer months witness a stark contrast, with July averages reaching up to 36°C (96°F). The yearly average temperature hovers around 3°C (37°F), highlighting the climatic diversity of this northern territory.
Arkhangelskaya, Russian Federation, exhibits distinct seasonal temperature patterns that reflect its subarctic climate. Winter months, particularly January and February, are marked by severe cold, with minimum temperatures plunging to -46°C (-51°F) in January and slightly less in February, while average temperatures hover around -10°C (15°F). As spring arrives, temperatures gradually rise, peaking in April when average temperatures reach 1°C (35°F), and maximum values can climb to 23°C (73°F). The warmth continues into summer, with July presenting the highest averages at 17°C (63°F) and maximums peaking at 36°C (96°F). However, fall ushers in a rapid cooling, as October displays a steep decline, averaging around 4°C (39°F), and temperatures continue to drop through November and December, signaling the return of winter conditions. This cyclical fluctuation underscores the stark contrasts in temperature that define the climate of Arkhangelskaya throughout the year.
Solovetsky experiences a significant temperature range throughout the year, with a minimum of -28°C (-18°F) in February, making winter particularly harsh, and a maximum of 19°C (66°F) in August, when summer peaks. This fluctuation highlights the extreme seasonal variations typical of the region, impacting both the climate and lifestyle of its inhabitants. For more details, you can refer to the monthly temperatures in Solovetsky.
Precipitation in Arkhangelskaya, Russian Federation, reveals a relatively stable distribution throughout the year, with a notable increase during the summer months. The winter months of January to April receive consistent precipitation, averaging around 42-43 mm (1.7 in) per month, accompanied by 10 to 12 rainy days. As spring transitions into summer, May marks the beginning of a significant uptick in rainfall, soaring to 61 mm (2.4 in) in May, and peaking at 100 mm (3.9 in) in July, which is the wettest month of the year. Both July and August see precipitation levels remaining high, at 97 mm (3.8 in).
As fall arrives, precipitation slightly decreases but remains relatively high, with October recording 85 mm (3.4 in) and November dropping to 60 mm (2.3 in). The number of rainy days also varies, with October experiencing the most with 16 days of rain. Monthly averages reflect an overall trend where the summer months frequently bring more precipitation, while winter remains drier but consistent. This pattern highlights the seasonal variability in Arkhangelskaya's climate, showcasing a wet summer contrasted against a stable, yet lower, winter precipitation.
In Arkhangelskaya, Russian Federation, sunshine duration exhibits a pronounced seasonal trend, reflecting the dramatic contrasts characteristic of its subarctic climate. The year begins with minimal sunshine, with January receiving only 31 hours of sunlight, a stark indicator of the long, dark winter months. However, as February approaches, there is a significant increase to 116 hours, paving the way for the gradual return of daylight. By March, the hours jump again to 228, and in April, sunshine hours reach 323 hours, marking the onset of spring and a steady climb towards the brighter days ahead.
As the seasons transition into summer, sunshine peaks in June, with an impressive 448 hours recorded, closely followed by July at 445 hours. This period of abundant sunlight is crucial for the region's flora and fauna, fostering growth and vitality. However, the descent begins in August with a notable decrease to 354 hours. The decline continues into the fall months, where September sees 251 hours, and by November, sunlight plummets again to only 50 hours. This cyclical pattern underscores the stark seasonal fluctuations in Arkhangelskaya's climate, emphasizing the vital role of sunlight in shaping both the environment and the lifestyle within this northern region.
The UV Index in Arkhangelskaya, Russian Federation, highlights significant seasonal variations, reflecting changes in sun exposure throughout the year. During the winter months, specifically January and February, the UV Index remains low at 1, indicating minimal risk of harm from unprotected sun exposure, with a burn time of 45 minutes. As spring unfolds, there is a gradual increase, with March reaching a moderate level of 3 and April climbing to 4. By May, outdoor activities should be approached with caution as the UV Index peaks at 5, requiring shorter burn times of 30 minutes.
Summer brings the highest UV readings, with both June and July recording an index of 6, which categorizes the exposure as high and reduces the safe burn time to just 25 minutes. As the days start to shorten, August sees a slight decrease to 5, while September returns to a moderate level of 4. The transition back to winter is marked by a drop in UV levels, falling to 2 in October and returning once again to low levels of 1 from November through December. This trend emphasizes the importance of sun protection during the sunnier months, especially considering the shorter burn times as the UV index rises.
UV Risk Categories
Daylight duration in Arkhangelskaya, Russian Federation, showcases dramatic seasonal fluctuations that are characteristic of its northern latitude. The year begins with minimal light, as January offers only 6 hours of daylight, followed by a slight increase to 8 hours in February. As spring approaches, daylight hours gradually extend, reaching 11 hours in March and 14 hours in April. By May, the region enjoys a remarkable 17 hours of daylight, marking a significant leap as the days grow longer.
The peak of summer occurs in June, when daylight maximizes at 19 hours, allowing for abundant outdoor activities and growth. Although daylight begins to wane slightly in July with 18 hours, it remains substantial. As summer transitions to fall, daylight decreases to 15 hours in August and continues to shorten, dropping to 12 hours in September. October sees a further decline to 9 hours, and by November, daylight dwindles back to 6 hours, culminating in December with just 4 hours—a stark reminder of the long, dark winters associated with this northern region. This cyclical pattern of daylight emphasizes the significant impact of seasonal changes on life in Arkhangelskaya, influencing everything from agriculture to daily activities.
The climate in Solovetsky, Russian Federation, is characterized by cold winters and mild summers. January sees average temperatures around -4°C (25°F), while July can reach a pleasant 12°C (54°F). Precipitation is spread throughout the year, with the wettest months occurring in August and October, recording approximately 78 mm (3.1 in) and 115 mm (4.5 in) respectively. The region enjoys considerable sunshine during summer, particularly in July with nearly 499 hours, contrasting sharply with the limited sunlight in December, which sees just 12 hours. For more details, visit Solovetsky climate.
In conclusion, the climate and environmental conditions of Arkhangelskaya, Russian Federation, are defined by striking seasonal variations that impact both temperature and sunlight exposure throughout the year. From the stark cold of winter, characterized by minimal daylight and low UV indices, to the extended hours of sunshine and heightened UV levels in the summer, the region presents unique challenges and opportunities. Understanding these climatic dynamics is essential for local residents and visitors alike, allowing them to adapt their activities and lifestyle accordingly. As climate patterns continue to evolve globally, the insights gleaned from Arkhangelskaya’s weather and environmental data serve as a vital reminder of the intricate relationship between geography and climate.