Beijing Temperature Market Guide
ZBAA • Beijing Capital International Airport
Polymarket
Beijing, China's capital, presents a continental monsoon climate with dramatic seasonal contrasts. Protected by mountains to the north and west, the city experiences cold, dry winters influenced by Siberian air and hot, humid summers shaped by the East Asian monsoon.
Quick Facts
| Station Code | ZBAA |
|---|---|
| Location | Beijing, China |
| Coordinates | 40.0741°N, 116.5870°E |
| Elevation | 115 ft (35 m) |
| Timezone | CST (Asia/Shanghai) |
| NWS Office | China Meteorological Administration |
About ZBAA Weather Station
Beijing Capital International Airport (ZBAA) serves as a primary weather observation station for Beijing. Located about 32 kilometers northeast of central Beijing, the airport sits at 115 feet (35 meters) elevation on the North China Plain.
Beijing's position at the northern edge of the North China Plain, sheltered by mountains from direct Arctic air, creates a climate with extreme seasonality. Temperature observations follow China Meteorological Administration (CMA) standards.
The city's massive urban heat island effect significantly influences local temperatures.
Beijing's position at the northern edge of the North China Plain, sheltered by mountains from direct Arctic air, creates a climate with extreme seasonality. Temperature observations follow China Meteorological Administration (CMA) standards.
The city's massive urban heat island effect significantly influences local temperatures.
Climate Patterns
Beijing has a humid continental climate (Koppen: Dwa) with hot, humid summers and cold, dry winters - a monsoon-influenced continental type. The seasonal temperature range exceeds 40°C.
Summer (June-August) brings highs of 30-33°C (86-91°F) with significant humidity during the monsoon. Heat waves can push temperatures above 38°C. Winter (December-February) is cold and dry with highs around 2-5°C (36-41°F), though Siberian cold waves can bring temperatures below -10°C.
Spring brings frequent dust storms from the Gobi Desert, while autumn is often the most pleasant season.
Summer (June-August) brings highs of 30-33°C (86-91°F) with significant humidity during the monsoon. Heat waves can push temperatures above 38°C. Winter (December-February) is cold and dry with highs around 2-5°C (36-41°F), though Siberian cold waves can bring temperatures below -10°C.
Spring brings frequent dust storms from the Gobi Desert, while autumn is often the most pleasant season.
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Winter (December - February): Cold and dry with highs 1-5°C (34-41°F). Siberian high dominates. Cold waves bring temperatures below -15°C. Minimal precipitation.
Spring (March - May): Rapid warming with dust storms. Highly variable temperatures. Transition from winter to summer monsoon.
Summer (June - August): Hot and increasingly humid with highs 30-35°C (86-95°F). Monsoon brings rainfall in July-August. Heat waves exceed 38°C.
Autumn (September - November): Pleasant and clear. Gradual cooling. Often the best weather season. First frost in October.
Spring (March - May): Rapid warming with dust storms. Highly variable temperatures. Transition from winter to summer monsoon.
Summer (June - August): Hot and increasingly humid with highs 30-35°C (86-95°F). Monsoon brings rainfall in July-August. Heat waves exceed 38°C.
Autumn (September - November): Pleasant and clear. Gradual cooling. Often the best weather season. First frost in October.
Trading Tips for Beijing
The contrast between winter and summer extremes is dramatic. Track the position of the Siberian High in winter and the subtropical high in summer.
Dust storms in spring can dramatically affect air quality but have limited direct temperature impact. However, they indicate strong wind patterns.
Summer heat waves occur when the subtropical high extends northward over North China. These events can last several days with temperatures above 35°C.
Winter cold waves from Siberia can drop temperatures 15-20°C below normal within 24-48 hours. These are often the most extreme temperature events.
China Meteorological Administration provides forecasts. European and American models perform well for Beijing.
Dust storms in spring can dramatically affect air quality but have limited direct temperature impact. However, they indicate strong wind patterns.
Summer heat waves occur when the subtropical high extends northward over North China. These events can last several days with temperatures above 35°C.
Winter cold waves from Siberia can drop temperatures 15-20°C below normal within 24-48 hours. These are often the most extreme temperature events.
China Meteorological Administration provides forecasts. European and American models perform well for Beijing.
Data Release Schedule
Typical release times for key data products at ZBAA. Times shown in UTC.
| Data Type | Typical Time (UTC) | Variability |
|---|---|---|
| METAR Hourly observations |
Hourly at :53 | ±1 min |
6-Hour High/Low Reports
These METARs include 6-hour maximum and minimum temperatures, useful for tracking intraday temperature trends.
00:53 UTC
06:53 UTC
12:53 UTC
18:53 UTC
Note: Times are approximate and may vary. CLI reports are the official resolution source for temperature markets. See NWS Data Guide for more information.
Forecasting Challenges
Siberian Cold Waves: The intensity and duration of winter cold outbreaks can exceed forecasts.
Summer Heat Waves: Heat wave temperatures above 38°C require precise forecasting of synoptic patterns.
Urban Heat Island: Beijing's massive urban area creates significant temperature variations across the city.
Dust Storm Effects: Spring dust events create complex forecasting scenarios.
Summer Heat Waves: Heat wave temperatures above 38°C require precise forecasting of synoptic patterns.
Urban Heat Island: Beijing's massive urban area creates significant temperature variations across the city.
Dust Storm Effects: Spring dust events create complex forecasting scenarios.
Historical Temperature Records
Record High: 41.9°C (107.4°F) recorded in July 1999.
Record Low: -27.4°C (-17.3°F) recorded in February 1966.
Historical Note: Beijing's continental monsoon climate creates one of the largest seasonal temperature ranges for any major world capital, spanning nearly 70°C from record low to record high.
Record Low: -27.4°C (-17.3°F) recorded in February 1966.
Historical Note: Beijing's continental monsoon climate creates one of the largest seasonal temperature ranges for any major world capital, spanning nearly 70°C from record low to record high.
📡 Official Data Sources
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