Now
☀️
31°
Loading current temperature, humidity, wind, and air quality context for Farshūţ, Qinā, Egypt.
Current temperature, humidity, wind, and air quality context for Farshūţ, Qinā, Egypt.
Clear sky
Feels like 27.7°C
Humidity
27%
Relative humidity
Wind
18 km/h
NW
UV
0
Low
Pressure
1011.7 hPa
Surface pressure
Now
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31°
03am
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30.4°
04am
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29.9°
05am
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29.2°
06am
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27.8°
07am
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28.4°
08am
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31°
09am
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33.8°
10am
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36.3°
11am
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38.3°
12pm
⛅
39.7°
01pm
🌤️
40.5°
02pm
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41°
03pm
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41.2°
04pm
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40.9°
05pm
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40.2°
06pm
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39.2°
07pm
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37.8°
08pm
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36°
09pm
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34.8°
10pm
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33.7°
11pm
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32.4°
12am
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31°
01am
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29.9°
Loading air quality context...
27.7°C
3° cooler than actual
27%
Dry
18 km/h
Direction: NW
0
Low
0%
Sky coverage
0 mm
Current rainfall
Farshūţ, nestled within the Qīnā Governorate of Egypt, occupies a geographically significant position in the Nile River Valley, approximately 120 kilometers north of Luxor. The city’s terrain is predominantly flat, characteristic of the fertile Nile Delta region, with elevations rarely exceeding 20 meters above sea level. This low-lying topography, while conducive to agriculture, presents challenges regarding air quality dispersion. Farshūţ is surrounded by expansive agricultural lands, primarily dedicated to cotton and sugarcane cultivation, which contribute to seasonal particulate matter from farming practices like burning crop residue. To the east, the landscape gradually transitions into the arid Eastern Desert, a stark contrast to the lush delta. The Nile River itself flows nearby, offering a potential mitigating factor through moisture and occasional breezes, though its influence is localized. The urban character of Farshūţ is a blend of traditional Egyptian architecture and modern development, with a growing population density impacting local air quality. The city’s location within a broader agricultural belt means it’s susceptible to pollutants originating from surrounding rural areas. The urban–rural gradient is relatively sharp, with the immediate vicinity of Farshūţ exhibiting higher concentrations of vehicular emissions and industrial activity compared to the surrounding farmland. The lack of significant topographic barriers further exacerbates the potential for pollutants to accumulate, particularly during periods of atmospheric stability. The regional position, within a densely populated and agriculturally intensive area, necessitates careful monitoring and mitigation strategies to safeguard air quality.
Farshūţ’s air quality experiences a distinct seasonal cycle heavily influenced by its climate and agricultural practices. The hot, dry months of May through September typically see the poorest air quality. Intense solar radiation promotes photochemical smog formation, while stagnant air masses and temperature inversions, common during this period, trap pollutants near the ground. Agricultural burning, a traditional practice for clearing fields after harvest, significantly contributes to particulate matter pollution during these months, particularly in late August and September. October and November mark a transitional period with slightly improved conditions as temperatures begin to cool and winds increase. Winter (December-February) generally offers the most favourable air quality, with cooler temperatures, more frequent wind dispersal, and reduced agricultural burning. However, fog events, common during these months, can temporarily trap pollutants, leading to localized episodes of reduced visibility and elevated particulate concentrations. Spring (March-April) witnesses a gradual increase in temperatures and a resurgence of agricultural activity, leading to a slow deterioration in air quality. The prevailing north-easterly winds play a crucial role in dispersing pollutants, but their effectiveness is diminished during periods of atmospheric stability. Sensitive groups, including children, the elderly, and individuals with respiratory conditions, should exercise caution during the hot, dry months and be mindful of potential fog events in winter. Outdoor activities are generally best enjoyed during the cooler months, particularly in the mornings before the onset of daytime heating and photochemical reactions.