Vs > Lhasa, Tibet
| Aracuai vs Lhasa, Tibet Climate & Distance Between | |
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- The distance between Aracuai, Brazil and Lhasa, Tibet, China is approximately 15,063 km or 9,360 mi.
- To reach Aracuai in this distance one would set out from Lhasa, Tibet bearing 275.9° or W and follow the great circles arc to approach Aracuai bearing 244.6° or WSW .
- Aracuai has a tropical wet and dry/ savanna climate with dry winters (Aw) whereas Lhasa, Tibet has a mid-latitude cool steppe climate (BSk).
- Aracuai is in or near the subtropical moist forest biome whereas Lhasa, Tibet is in or near the boreal moist forest biome.
- The mean temperature is 16.9 °C (30.4°F) warmer.
- Average monthly temperatures vary by 12.3 °C (22.1°F) less in Aracuai. The continentality subtype is truly hyperoceanic as opposed to truly oceanic.
- Total annual precipitation averages 420.7 mm (16.6 in) more which is equivalent to 420.7 l/m² (10.32 US gal/ft²) or 4,207,000 l/ha (449,756 US gal/ac) more. About 2 as much.
- The altitude of the sun at midday is overall 9.7° higher in Aracuai than in Lhasa, Tibet.
- Relative humidity levels are 2.8% higher.
- The mean dew point temperature is 16.7°C (30.1°F) higher.
Climate Comparison Table
The table shows values for Aracuai relative to Lhasa, Tibet. You can also view this comparison the other way around from the perspective of Lhasa, Tibet vs Aracuai.
| |
Jan |
Feb |
Mar |
Apr |
May |
Jun |
Jul |
Aug |
Sep |
Oct |
Nov |
Dec |
|
Annual |
| Average Max Temperature °C ( °F) |
+25 (+46) |
+24 (+44) |
+21 (+38) |
+16 (+29) |
+11 (+20) |
+7 (+12) |
+7 (+12) |
+9 (+16) |
+12 (+21) |
+15 (+27) |
+19 (+35) |
+23 (+42) |
|
+16 (+28) |
| Average Temperature °C ( °F) |
+28 (+50) |
+25 (+46) |
+22 (+39) |
+17 (+30) |
+12 (+21) |
+7 (+12) |
+6 (+11) |
+9 (+15) |
+12 (+21) |
+17 (+31) |
+23 (+41) |
+27 (+48) |
|
+17 (+30) |
| Average Min Temperature °C ( °F) |
+31 (+56) |
+28 (+51) |
+24 (+43) |
+19 (+34) |
+13 (+23) |
+7 (+12) |
+5 (+9) |
+7 (+13) |
+12 (+21) |
+20 (+35) |
+26 (+47) |
+30 (+54) |
|
+19 (+33) |
| Average Precipitation mm (in) |
+139 (+5) |
+83 (+3) |
+100 (+4) |
+34 (+1) |
-16 (-1) |
-69 (-3) |
-114 (-4) |
-118 (-5) |
-39 (-2) |
+96 (+4) |
+165 (+6) |
+160 (+6) |
|
+421 (+17) |
| Average Daylight Hours & Minutes/ Day |
+2h 33' |
+1h 35' |
+0h 17' |
-1h 06' |
-2h 16' |
-2h 51' |
-2h 35' |
-1h 36' |
-0h 15' |
+1h 08' |
+2h 18' |
+2h 51' |
|
0h 00' |
| Sun altitude at solar noon on the 21st day (°) |
+45.6 |
+33.2 |
+12.2 |
-11 |
-27.6 |
-34.1 |
-28 |
-11.3 |
+11.5 |
+33.4 |
+45.1 |
+46.5 |
| +9.7 |
| Relative Humidity (%) |
+5.1 |
+1.7 |
+0.4 |
+2.4 |
+13.3 |
+7.7 |
-1 |
-5.8 |
-8.7 |
+7.6 |
+4.9 |
+6.5 |
|
+2.8 |
| Average Dew Point Temperature °C & (°F) |
+27.3 (+49) |
+24.4 (+44) |
+20.7 (+37) |
+16.7 (+30) |
+14 (+25) |
+8 (+14) |
+5.4 (+10) |
+7 (+13) |
+9.3 (+17) |
+18.2 (+33) |
+22.8 (+41) |
+26.6 (+48) |
|
+16.7 (+30) |
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Aracuai vs Lhasa, Tibet Discussion
You are welcome to incorporate your thoughts on the differences in climate or other matters such as contrasts in culture, standard of living, demographics etc.
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