Vs > Ishinomaki
| Ma’An vs Ishinomaki Climate & Distance Between | |
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- The distance between Ma’An, Jordan and Ishinomaki, Japan is approximately 9,169 km or 5,698 mi.
- To reach Ma’An in this distance one would set out from Ishinomaki bearing 302.8° or WNW and follow the great circles arc to approach Ma’An bearing 229.6° or SW .
- Ma’An has a mid-latitude cool desert climate (BWk) whereas Ishinomaki has a humid subtropical climate (Cfa).
- The mean annual temperature is 6.1 °C (11°F) warmer.
- Average monthly temperatures vary by 5.2 °C (9.4°F) less in Ma’An. The continentality subtype is semicontinental as opposed to subcontinental.
- Total annual precipitation averages 1004.9 mm (39.6 in) less which is equivalent to 1004.9 l/m² (24.66 US gal/ft²) or 10,049,000 l/ha (1,074,305 US gal/ac) less. About 0 as much.
- The altitude of the sun at midday is overall 8.2° higher in Ma’An than in Ishinomaki.
Climate Comparison Table
The table shows values for Ma’An relative to Ishinomaki. You can also view this comparison the other way around from the perspective of Ishinomaki vs Ma’An.
| |
Jan |
Feb |
Mar |
Apr |
May |
Jun |
Jul |
Aug |
Sep |
Oct |
Nov |
Dec |
|
Annual |
| Average Temperature °C ( °F) |
+7 (+13) |
+9 (+15) |
+9 (+16) |
+8 (+14) |
+7 (+12) |
+6 (+11) |
+4 (+8) |
+2 (+4) |
+4 (+7) |
+6 (+10) |
+5 (+10) |
+6 (+11) |
|
+6 (+11) |
| Average Precipitation mm (in) |
-32 (-1) |
-40 (-2) |
-60 (-2) |
-88 (-3) |
-97 (-4) |
-109 (-4) |
-126 (-5) |
-124 (-5) |
-141 (-6) |
-105 (-4) |
-60 (-2) |
-25 (-1) |
|
-1005 (-40) |
| Average Daylight Hours & Minutes/ Day |
+0h 38' |
+0h 23' |
+0h 04' |
-0h 16' |
-0h 34' |
-0h 43' |
-0h 39' |
-0h 23' |
-0h 03' |
+0h 16' |
+0h 34' |
+0h 43' |
|
0h 00' |
| Sun altitude at solar noon on the 21st day (°) |
+8.3 |
+8.3 |
+8.4 |
+8.3 |
+8.3 |
+8.3 |
+8.2 |
+8.2 |
+8.2 |
+8.2 |
+8.2 |
+8.2 |
| +8.2 |
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Ma’An vs Ishinomaki 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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