Vs > Nemuro
| Lhasa, Tibet vs Nemuro Climate & Distance Between | |
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- The distance between Lhasa, Tibet, China and Nemuro, Japan is approximately 5,004 km or 3,109 mi.
- To reach Lhasa, Tibet in this distance one would set out from Nemuro bearing 271.1° or W and follow the great circles arc to approach Lhasa, Tibet bearing 236.8° or WSW .
- Lhasa, Tibet has a mid-latitude cool steppe climate (BSk) whereas Nemuro has a warm summer continental/ hemiboreal climate with no dry season (Dfb).
- The mean temperature is 1.6 °C (2.9°F) warmer.
- Average monthly temperatures vary by 4.8 °C (8.6°F) less in Lhasa, Tibet. The continentality subtype is truly oceanic as opposed to subcontinental.
- Total annual precipitation averages 615 mm (24.2 in) less which is equivalent to 615 l/m² (15.09 US gal/ft²) or 6,150,000 l/ha (657,476 US gal/ac) less. About 2/5 as much.
- The altitude of the sun at midday is overall 13.6° higher in Lhasa, Tibet than in Nemuro.
- Relative humidity levels are 11.1% lower.
- The mean dew point temperature is 0.6°C (1.1°F) lower.
Climate Comparison Table
The table shows values for Lhasa, Tibet relative to Nemuro. You can also view this comparison the other way around from the perspective of Nemuro vs Lhasa, Tibet.
| |
Jan |
Feb |
Mar |
Apr |
May |
Jun |
Jul |
Aug |
Sep |
Oct |
Nov |
Dec |
|
Annual |
| Average Max Temperature °C ( °F) |
+9 (+15) |
+11 (+20) |
+11 (+20) |
+9 (+16) |
+8 (+14) |
+8 (+15) |
+4 (+8) |
1 (+1) |
1 (+2) |
2 (+4) |
3 (+6) |
6 (+10) |
|
+6 (+11) |
| Average Temperature °C ( °F) |
+2 (+4) |
+6 (+12) |
+7 (+12) |
+5 (+9) |
+5 (+8) |
+5 (+9) |
+1 (+2) |
-3 (-5) |
-3 (-5) |
-3 (-5) |
-3 (-5) |
-1 (-2) |
|
+2 (+3) |
| Average Min Temperature °C ( °F) |
-2 (-4) |
+2 (+4) |
+2 (+4) |
+1 (+1) |
+1 (+2) |
+2 (+3) |
-1 (-2) |
-5 (-9) |
-5 (-9) |
-6 (-11) |
-6 (-11) |
-5 (-9) |
|
-2 (-3) |
| Average Precipitation mm (in) |
-46 (-2) |
-33 (-1) |
-62 (-2) |
-79 (-3) |
-74 (-3) |
-32 (-1) |
+17 (+1) |
+9 (+0) |
-82 (-3) |
-107 (-4) |
-79 (-3) |
-49 (-2) |
|
-615 (-24) |
| Number of Precipitation Days (% chance of precip. on a day ) |
-10 ( -32) |
-7.5 ( -27) |
-8 ( -26) |
-8.5 ( -28) |
-7 ( -23) |
-1 ( -3) |
+5 (+16) |
+2 (+6) |
-3 ( -10) |
-8 ( -26) |
-7.5 ( -25) |
-8 ( -26) |
|
-61.5 ( -17) |
| Average Daylight Hours & Minutes/ Day |
+1h 08' |
+0h 41' |
+0h 07' |
-0h 28' |
-1h 00' |
-1h 17' |
-1h 09' |
-0h 41' |
-0h 06' |
+0h 29' |
+1h 01' |
+1h 17' |
|
0h 00' |
| Sun altitude at solar noon on the 21st day (°) |
+13.7 |
+13.6 |
+13.7 |
+13.7 |
+13.7 |
+13.7 |
+13.6 |
+13.6 |
+13.6 |
+13.5 |
+13.5 |
+13.6 |
| +13.6 |
| Relative Humidity (%) |
-2 |
-3 |
-5 |
-12 |
-24 |
-26 |
-21 |
-18 |
-13 |
-11 |
+1 |
+1 |
|
-11.1 |
| Average Dew Point Temperature °C & (°F) |
+2 (+4) |
+5.6 (+10) |
+5 (+9) |
+2.5 (+5) |
-0.6 (-1) |
-0.2 (0) |
-2.8 (-5) |
-5.9 (-11) |
-4.9 (-9) |
-4.9 (-9) |
-2.1 (-4) |
-0.9 (-2) |
|
-0.6 (-1) |
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Lhasa, Tibet vs Nemuro 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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