Vs > Lhasa, Tibet
 | Matsumoto vs Lhasa, Tibet Climate & Distance Between |  |
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- The distance between Matsumoto, Japan and Lhasa, Tibet, China is approximately 4,388 km or 2,727 mi.
- To reach Matsumoto in this distance one would set out from Lhasa, Tibet bearing 67.7° or ENE
 and follow the great circles arc to approach Matsumoto bearing 94.3° or E .
- Matsumoto has a humid subtropical climate (Cfa) whereas Lhasa, Tibet has a mid-latitude cool steppe climate (BSk).
- Matsumoto is in or near the cool temperate wet forest biome whereas Lhasa, Tibet is in or near the boreal moist forest biome.
- The annual mean temperature is 3.7 °C (6.7°F) warmer.
- Average monthly temperatures vary by 7.5 °C (13.5°F) more in Matsumoto. The continentality subtype is subcontinental as opposed to truly oceanic.
- Total annual precipitation averages 590 mm (23.2 in) more which is equivalent to 590 l/m² (14.48 US gal/ft²) or 5,900,000 l/ha (630,749 US gal/ac) more. About 2 2/5 as much.
- The altitude of the sun at midday is overall 6.6° lower in Matsumoto than in Lhasa, Tibet.
- Relative humidity levels are 0.4% higher.
- The mean dew point temperature is 3.7°C (6.6°F) higher.
Climate Comparison Table
The table shows values for Matsumoto relative to Lhasa, Tibet. You can also view this comparison the other way around from the perspective of Lhasa, Tibet vs Matsumoto.
| | |
Jan |
Feb |
Mar |
Apr |
May |
Jun |
Jul |
Aug |
Sep |
Oct |
Nov |
Dec |
|
Annual |
 | Average Max Temperature °C ( °F) |
+-2 (-4) |
-4 (-6) |
-3 (-5) |
+2 (+4) |
+3 (+6) |
+2 (+4) |
+7 (+12) |
+9 (+17) |
+5 (+9) |
+2 (+4) |
+2 (+4) |
+0 (0) |
|
+2 (+4) |
 | Average Temperature °C ( °F) |
+1 (+2) |
-2 (-3) |
-2 (-3) |
+2 (+4) |
+4 (+7) |
+4 (+7) |
+8 (+14) |
+10 (+17) |
+7 (+12) |
+4 (+8) |
+5 (+8) |
+4 (+6) |
|
+4 (+7) |
 | Average Min Temperature °C ( °F) |
+4 (+7) |
+1 (+2) |
+0 (+1) |
+3 (+6) |
+4 (+8) |
+5 (+9) |
+9 (+16) |
+10 (+18) |
+8 (+14) |
+6 (+11) |
+6 (+11) |
+6 (+10) |
|
+5 (+9) |
 | Average Precipitation mm (in) |
+28 (+1) |
+44 (+2) |
+65 (+3) |
+81 (+3) |
+68 (+3) |
+81 (+3) |
+17 (+1) |
-29 (-1) |
+88 (+3) |
+77 (+3) |
+46 (+2) |
+24 (+1) |
|
+590 (+23) |
 | Average Daylight Hours & Minutes/ Day |
-0h 29' |
-0h 18' |
-0h 03' |
+0h 12' |
+0h 26' |
+0h 33' |
+0h 30' |
+0h 18' |
+0h 02' |
-0h 12' |
-0h 26' |
-0h 33' |
|
0h 00' |
 | Sun altitude at solar noon on the 21st day (°) |
-6.6 |
-6.6 |
-6.6 |
-6.6 |
-6.6 |
-6.6 |
-6.5 |
-6.5 |
-6.5 |
-6.5 |
-6.5 |
-6.6 |
| -6.6 |
 | Relative Humidity (%) |
-4 |
-5 |
-8 |
-6 |
+3 |
+8 |
+4 |
+0 |
+5 |
+11 |
+0 |
-3 |
|
+0.4 |
 | Average Dew Point Temperature °C & (°F) |
+0.4 (+1) |
-2.2 (-4) |
-2.8 (-5) |
+0.9 (+2) |
+4.3 (+8) |
+5.4 (+10) |
+8.3 (+15) |
+9.2 (+17) |
+7.3 (+13) |
+6.3 (+11) |
+4.1 (+7) |
+2.6 (+5) |
|
+3.7 (+7) |
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Matsumoto 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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