Last updated: January 18, 2025
Sühbaatar, Mongolia, presents a unique climate defined by the Köppen-Geiger classifications of BSk (Cold Semiarid) and Dwb (Warm Summer Continental). This region experiences an extreme temperature range, with frigid winters plunging to a minimum of -40°C (-40°F) in January, while summers can escalate to sweltering highs of 38°C (101°F) in July. The annual average temperature hovers around 2°C (36°F), reflecting the stark contrasts characteristic of this region's weather patterns. Such climatic variability significantly influences local ecosystems and human activities, shaping the lifestyle and resilience of its inhabitants.
In Sühbaatar, Mongolia, temperature patterns exhibit pronounced seasonal variations, characterized by harsh winters and warm summers. January and December are particularly frigid, with minimum temperatures reaching as low as -40°C (-40°F) and -39°C (-37°F), respectively, while the average temperatures linger around -19°C (-3°F) and -17°C (1°F). As winter transitions into spring, temperatures gradually rise, with March showcasing a significant warming trend, where the average climbs to -4°C (25°F) and maximums can hit 21°C (69°F). This upward trend continues into April and May, culminating in July's peak temperatures, which soar to 38°C (101°F), while average temperatures stabilize around 21°C (71°F). The onset of autumn brings a cooler period, where temperatures begin to drop again by September, revealing a return to chilly conditions by November, thereby illustrating Sühbaatar's clear dichotomy between its extreme seasonal highs and lows.
Havirga experiences extreme temperatures, with a minimum of -39°C (-38°F) in January and a maximum of 37°C (99°F) in July, as detailed in the monthly temperatures in Havirga. Similarly, Dzuunbulag sees a minimum of -36°C (-32°F) in January and can reach up to 38°C (100°F) in July according to the monthly temperatures in Dzuunbulag. Bayasgalant presents slightly milder extremes, recording a minimum of -37°C (-35°F) in January and a maximum of 37°C (98°F) in July, as noted in the monthly temperatures in Bayasgalant.
Precipitation in Sühbaatar, Mongolia, is notably low during the winter months, with January and February receiving a mere 2 mm (0.1 in) and 3 mm (0.1 in), respectively. The winter is characterized by dry conditions, evident as both months report 0 days of measurable precipitation. As spring approaches, there is a gradual increase in rainfall, with March recording 5 mm (0.2 in) over 0 days and culminating in April with 12 mm (0.5 in) across just 2 days of precipitation, heralding the start of a wetter season.
The summer months bring a significant spike in precipitation, peaking in July and August with 71 mm (2.8 in) and 76 mm (3.0 in), respectively, each accompanied by around 10 days of rain. This period accounts for the majority of the annual rainfall, supporting local agriculture and ecosystems. Following the summer, precipitation declines again in September to 27 mm (1.1 in), before tapering off in the autumn months of October and November, which see 13 mm (0.5 in) and 9 mm (0.3 in) respectively, as Sühbaatar transitions back into its dry winter conditions.
Sühbaatar, Mongolia, experiences a distinct seasonal pattern in sunshine duration, with a remarkable increase as winter transitions to summer. Starting with a modest 207 hours of sunlight in January, the region gradually soaks up more rays with each passing month. February sees this number rise to 265 hours, and by March, it escalates further to 313 hours. The peak sunshine occurs during the summer months, with July shining the brightest at 363 hours. This trend showcases the region's shift from the stark, cold winters to the sun-drenched warmth of summer, providing an essential energy boost for the local environment.
As the season shifts from summer to autumn, Sühbaatar experiences a gradual decline in sunshine hours, yet the transition remains gentle compared to the winter months. August continues to bask in 336 hours, followed closely by September at 303 hours. By October, the areas start to cool off with 282 hours of sun exposure, which further dwindles to 254 hours in both November and December. This seasonal rhythm is vital for agriculture and local lifestyles, as the abundance of sunlight during the summer months plays a crucial role in supporting plant growth and overall ecosystem health while the shorter days of winter herald a return to hibernation for the region's flora and fauna.
The UV Index in Sühbaatar, Mongolia, reflects significant seasonal variations, with notable increases during the summer months when exposure levels reach their peak. In January, the UV Index is relatively low at 2, indicating minimal risk for harm from unprotected sun exposure, with a burn time of 45 minutes. This trend continues into February with a moderate index of 3, transitioning into higher risks as March arrives, marking the onset of spring with a substantial rise to 6 and a burn time of just 25 minutes. April maintains this elevated level at 7, prompting increased caution as sunshine becomes more intense.
As summer arrives, Sühbaatar experiences its highest UV levels, with indices soaring to 9 and 10 from May through August—classified as very high risk. During this period, the rapid decrease in burn time to 15 minutes necessitates protective measures against skin damage. In the subsequent months of September and October, the UV Index decreases to 7 and 5, marking a return to moderate exposure levels, while November and December lower further to 3 and 2, respectively. These fluctuations underscore the need for awareness regarding UV exposure throughout the year, particularly during peak summer months when protection is essential for outdoor activities.
UV Risk Categories
In Sühbaatar, Mongolia, daylight duration reveals a dynamic seasonal pattern, characterized by increasing light hours as winter transitions into spring and ultimately summer. Starting with just 9 hours of daylight in January, the days begin to lengthen, reaching 10 hours by February and extending to 11 hours in March. Notably, this increase accelerates into April as the region welcomes 13 hours of daylight, peaking at 14 hours in May. The longest days of the year occur in June and July, each providing 15 hours of natural light, which greatly enhances outdoor activities and contributes to a vibrant, energetic atmosphere.
As autumn approaches, daylight duration begins to taper off, starting at 14 hours in August and gradually decreasing to 12 hours by September. The days continue to shorten into October, dropping to 10 hours, and finally reducing to 9 hours in November and 8 hours in December. This gradual decline emphasizes the cyclical nature of daylight in Sühbaatar, impacting local lifestyles and activities significantly, particularly as the longer summer days provide ample opportunity for farming and recreation.
Baruun-Urt, Mongolia experiences extreme temperature variations throughout the year, with January averaging -20°C (-4°F) and July reaching an average of 21°C (71°F). This region sees the most precipitation in July and August, with around 71 mm (2.8 in) each month, while winter months remain quite dry. Sunshine is abundant, peaking at 362 hours in July, contributing to warm summer days. The climate is characterized by cold winters and warm summers, making it a region of significant contrast. For more details, visit Baruun-Urt climate.
Bayasgalant, Mongolia experiences extreme seasonal temperature variations, with January averages plunging to -20°C (-3°F) and July peaks reaching up to 20°C (69°F). The region is characterized by low annual precipitation, peaking at 82 mm (3.2 in) in July, contributing to its overall arid climate. Sunshine hours are abundant, with the sun shining for up to 370 hours in July, ensuring long, bright summer days. For more detailed climate information, visit Bayasgalant climate.
Chonogol, Mongolia experiences extreme seasonal variations, with harsh winters where January temperatures can plummet to -37°C (-34°F) and milder summers where July peaks at 38°C (101°F). Precipitation is minimal in the winter months, averaging only 3 mm in January, but increases significantly during the summer, especially in August, with 95 mm (3.7 in). Sunshine hours are abundant, especially from March to July, with July receiving the most at 363 hours. This significant variation in temperature and rainfall creates a distinctive climate, making it an interesting location for observation. For more details, visit Chonogol climate.
Dzuunbulag, Mongolia experiences a harsh continental climate, characterized by long, frigid winters and short, warm summers. January temperatures can plummet to -36°C (-32°F), while July peaks at a warm 38°C (100°F). Precipitation is relatively low, with most rainfall occurring in the summer months, particularly July and August, which receive about 70 mm (2.8 in) each. Sunshine hours are abundant, especially in summer, with July boasting 361 hours of sunlight. For more detailed information, visit Dzuunbulag climate.
Hanhohiy, Mongolia experiences a harsh climate with extreme temperature variations throughout the year. Winter months, particularly January and February, see average lows around -20°C (-4°F) and consistently below freezing temperatures, while summers from June to August are mild with averages reaching 21°C (70°F). Precipitation is low during colder months, peaking in July, when 83 mm (3.3 in) of rain falls, highlighting the area's dry climate overall. Despite the cold, sunshine is abundant, with July enjoying the most sun at 361 hours. For more detailed information, visit Hanhohiy climate.
The climate in Hatavch, Mongolia, is characterized by harsh, cold winters and warm summers. January sees temperatures plummet as low as -39°C (-38°F), gradually rising to highs of up to 37°C (99°F) in July. Precipitation is minimal during winter, increasing with summer rainfall peaking in July and August, when around 80 mm (3.2 in) is recorded. The area enjoys substantial sunshine, particularly in summer, with July receiving around 360 hours of sunshine. For more information, visit Hatavch climate.
Havirga, Mongolia, experiences extreme seasonal temperature variations, with January averaging around -20°C (-3°F) and soaring to 22°C (72°F) in July. The region has low annual precipitation, peaking in July and August with 64 mm (2.5 in) and 77 mm (3.0 in), respectively, while winters are notably dry. Sunshine is abundant, especially in summer, with the highest sunny days recorded in July at 365 hours. This continental climate, characterized by cold winters and warm summers, highlights the unique environmental conditions of Havirga. For more detailed information, visit Havirga climate.
Haylaastay, Mongolia experiences extreme temperatures throughout the year, with January averaging -20°C (-4°F) and reaching maximums of 0°C (33°F), while July peaks at around 22°C (71°F). Precipitation is minimal during the winter months, gradually increasing to its highest in July and August, with 74 mm (2.9 in) and 76 mm (3.0 in) respectively. Sunshine hours are plentiful, especially in summer, with July receiving 356 hours of sunlight, making it the sunniest month. This diverse climate supports a unique environment that can be explored further at Haylaastay climate.
The climate in Hongor, Mongolia, is characterized by harsh winters and warm summers. January sees temperatures plummet to a minimum of -40°C (-40°F) with minimal precipitation, while July peaks at a maximum of 36°C (98°F) accompanied by significant rainfall. The region experiences the most sunshine in July, totaling 364 hours, and the least in January with 209 hours. Precipitation increases from 3 mm (0.1 in) in January to 79 mm (3.1 in) during August, indicating a distinct wet season. For more detailed information, visit Hongor climate.
Ovoot, Mongolia experiences a harsh climate characterized by extremely cold winters and warm summers. January sees temperatures plummet to a minimum of -40°C (-40°F), with January and December averaging around -19°C (-2°F) and -18°C (0°F) respectively. The warmest months are July and August, where temperatures reach averages of 21°C (70°F) and 17°C (64°F) with notable rainfall peaking in July at 65 mm (2.5 in) and August at 79 mm (3.1 in). Despite the low precipitation overall, Ovoot enjoys abundant sunshine, especially in summer, with July receiving an impressive 364 hours of sunlight. For more detailed information, visit Ovoot climate.
Sergelen, Mongolia experiences a harsh continental climate characterized by extreme temperature variations throughout the year. January and February are particularly frigid, with average temperatures dropping as low as -19°C (-2°F) and -15°C (5°F), while July peaks at a warm 22°C (72°F) on average. Precipitation is minimal during the colder months, but July sees a significant increase, receiving around 64 mm (2.5 in) of rain. Sunshine is abundant, especially in summer, with July boasting the highest hours at 365. For more details, visit Sergelen climate.
Shireet, Mongolia experiences a continental climate characterized by harsh winters and warm summers. January sees extreme lows around -37°C (-34°F), while July reaches highs of 38°C (101°F). Precipitation is minimal in winter months, peaking in July with approximately 73 mm (2.9 in) of rainfall, contributing to the region's dry conditions. Sunshine varies throughout the year, with July enjoying the most at 364 hours. For a comprehensive overview, visit Shireet climate.
Ulaandel, Mongolia experiences a harsh, continental climate characterized by long, frigid winters and brief, warm summers. In January, temperatures plunge to an average of -19°C (-2°F), with lows reaching -38°C (-36°F). Summer months are significantly warmer, peaking in July with average temperatures of 21°C (70°F) and maximums of 36°C (97°F). Precipitation is relatively low in the winter, averaging around 3 mm per month, but increases during the summer, particularly in July and August, when it reaches up to 81 mm (3.2 in). For more details, visit Ulaandel climate.
In conclusion, Sühbaatar, Mongolia, is characterized by distinct climatic and environmental phenomena, including significant temperature fluctuations, varied precipitation patterns, and marked seasonal changes in sunshine duration and daylight. The region experiences harsh winters with extreme cold and low sunshine hours, giving way to warm summers with ample sunlight and heightened UV exposure. As daylight hours increase during the spring and peak in summer, residents benefit from longer periods of natural light, which are vital for agricultural activities and outdoor pursuits. Understanding these climatic patterns is crucial for the local population and can help inform strategies for adaptation and sustainable practices, ultimately fostering resilience in the face of ongoing environmental changes.