ClimateSearch

Ann, Rakhine

Myanmar · 120k people · 32 m elevation · Northern Hemisphere

Every month in detail

Thirty-year averages for each calendar month.

Monthly climate normals. Values shown as an em dash are missing from the source data.
MonthJanFebMarAprMayJunJulAugSepOctNovDec
Average high81°F (27°C)86°F (30°C)92°F (33°C)97°F (36°C)95°F (35°C)90°F (32°C)89°F (31°C)89°F (31°C)90°F (32°C)90°F (32°C)88°F (31°C)83°F (28°C)
Average low59°F (15°C)61°F (16°C)68°F (20°C)75°F (24°C)77°F (25°C)76°F (25°C)76°F (24°C)76°F (24°C)75°F (24°C)75°F (24°C)69°F (21°C)62°F (17°C)
Dew point57°F (14°C)58°F (14°C)65°F (18°C)72°F (22°C)76°F (24°C)76°F (25°C)76°F (25°C)76°F (24°C)76°F (24°C)75°F (24°C)68°F (20°C)61°F (16°C)
Rainfall0.1 in (3 mm)0.1 in (2 mm)0.2 in (5 mm)0.8 in (21 mm)10 in (253 mm)22.2 in (563 mm)25.1 in (637 mm)18 in (458 mm)15.9 in (404 mm)8.2 in (208 mm)1.3 in (32 mm)0.5 in (14 mm)
Rainy days001113252928241431
Snowfall0 in (0 cm)0 in (0 cm)0 in (0 cm)0 in (0 cm)0 in (0 cm)0 in (0 cm)0 in (0 cm)0 in (0 cm)0 in (0 cm)0 in (0 cm)0 in (0 cm)0 in (0 cm)
Sunshine271 h263 h284 h257 h173 h55 h40 h50 h91 h169 h234 h260 h

Scroll the table sideways for all twelve months.

Projected change, 2031–2050

Model projection, not an observation

How this city’s climate may change, measured against the same models’ own 1995–2014 output. Nothing here affects the match score above.

Change in summer afternoon highs

+1.3°F (+0.7°C)

Models range from +0.5°F (+0.3°C) to +2.3°F (+1.3°C)

Days above 90°F (32°C) a year

84 → 104

About 1.2× as many

Warming by month
  • January: +1.4°F (+0.8°C)
  • February: +1.4°F (+0.8°C)
  • March: +1.1°F (+0.6°C)
  • April: +1.5°F (+0.8°C)
  • May: +1.4°F (+0.8°C)
  • June: +1.8°F (+1.0°C)
  • July: +1.0°F (+0.6°C)
  • August: +1.0°F (+0.6°C)
  • September: +1.0°F (+0.6°C)
  • October: +1.1°F (+0.6°C)
  • November: +0.4°F (+0.2°C)
  • December: +0.8°F (+0.4°C)
Scenario
SSP5-8.5 (high emissions)
Models
4 · CMIP6 HighResMIP, downscaled

This is a high-emissions pathway — the upper end of plausible futures, not a central estimate. Changes are measured by each model against its own past output and then applied to the observed record, which cancels each model’s bias but not the genuine uncertainty about how much warming occurs. Where the models disagree widely, the range above is the honest answer.