Now
🌦️
28.4°
💧88%
Loading current temperature, humidity, wind, and air quality context for Neibu, Pingtung, Taiwan.
Current temperature, humidity, wind, and air quality context for Neibu, Pingtung, Taiwan.
Light drizzle
Feels like 33.6°C
Humidity
74%
Relative humidity
Wind
13.3 km/h
SSW
UV
6.85
High
Pressure
1005.9 hPa
Surface pressure
Now
🌦️
28.4°
💧88%
10am
🌦️
29.2°
💧93%
11am
🌧️
28.5°
💧96%
12pm
🌧️
26.2°
💧99%
01pm
🌦️
27.5°
💧100%
02pm
🌧️
27°
💧100%
03pm
🌧️
26.8°
💧100%
04pm
🌦️
26.7°
💧99%
05pm
🌦️
26.5°
💧96%
06pm
🌦️
26.1°
💧88%
07pm
🌦️
25.8°
💧77%
08pm
☁️
26°
💧69%
09pm
🌦️
26.1°
💧67%
10pm
🌦️
26.2°
💧67%
11pm
☁️
26.5°
💧69%
12am
🌦️
26.3°
💧73%
01am
🌦️
26.1°
💧78%
02am
🌧️
25.7°
💧82%
03am
🌦️
25°
💧85%
04am
🌧️
24.6°
💧88%
05am
🌦️
24.5°
💧90%
06am
🌦️
24.4°
💧92%
07am
🌧️
24.9°
💧93%
08am
🌦️
25.1°
💧94%
Loading air quality context...
33.6°C
5° warmer than actual
74%
Humid
13.3 km/h
Direction: SSW
6.85
High
47%
Sky coverage
0.1 mm
Current rainfall
Neibu, nestled within Pingtung County in southern Taiwan, presents a unique geographic context influencing its air quality. Situated at coordinates 22.6500, 120.5875, the city occupies a relatively low-lying area within the Hengchun Peninsula, though gently undulating terrain is common. The surrounding landscape is predominantly agricultural, characterized by extensive fields of fruit orchards (particularly mangoes and pomelos) and rice paddies. Neibu isn’t directly on the coast, but is approximately 15km inland from the Pacific Ocean, meaning maritime influences – humidity and occasional sea breezes – play a role in local weather patterns. The Central Mountain Range lies to the east, creating a rain shadow effect and influencing wind flow. While Neibu isn’t a major industrial hub, Pingtung County as a whole has pockets of light industry and aquaculture, contributing to regional emissions. The urban-rural gradient is quite pronounced; Neibu itself is a smaller city, quickly transitioning to rural farmland. This proximity to agricultural practices introduces potential for particulate matter from dust and seasonal burning of agricultural waste. The relatively sheltered location can also contribute to pollutant build-up, especially during periods of calm weather. Understanding these geographical factors is crucial for interpreting air quality trends in Neibu.
Neibu’s air quality follows a distinct seasonal pattern dictated by Taiwan’s subtropical monsoon climate. The winter months (November to February) often see the poorest air quality. This is due to the prevalence of the Northeast Monsoon, which brings cooler, drier air and can trap pollutants under temperature inversions, particularly in the mornings. Reduced rainfall during this period also limits natural cleansing. Spring (March to May) brings a gradual improvement as temperatures rise and rainfall increases, washing away accumulated pollutants. However, agricultural burning of crop residue after harvest can temporarily degrade air quality. Summer (June to August) is generally the cleanest period, with frequent heavy rainfall from the Southwest Monsoon effectively scrubbing the atmosphere. High humidity can also suppress dust. Autumn (September to October) sees a transition period, with decreasing rainfall and the potential for stagnant air masses. Typhoons, common during late summer and early autumn, can initially worsen air quality due to windblown dust, but subsequent rainfall provides significant improvement. Sensitive groups – children, the elderly, and those with respiratory conditions – should be particularly cautious during winter and spring. Avoiding strenuous outdoor activity on high-pollution days is advisable.