ClimateSearch

As Salţ, Balqa

Jordan · 108k people · 852 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 high53°F (12°C)56°F (13°C)62°F (17°C)71°F (22°C)80°F (27°C)86°F (30°C)89°F (31°C)89°F (31°C)85°F (30°C)79°F (26°C)67°F (20°C)58°F (14°C)
Average low40°F (4°C)41°F (5°C)45°F (7°C)51°F (11°C)58°F (15°C)63°F (17°C)67°F (19°C)67°F (19°C)64°F (18°C)60°F (15°C)51°F (10°C)43°F (6°C)
Dew point35°F (2°C)35°F (2°C)37°F (3°C)38°F (3°C)42°F (6°C)49°F (9°C)54°F (12°C)56°F (14°C)53°F (12°C)46°F (8°C)39°F (4°C)36°F (2°C)
Rainfall4 in (102 mm)3.5 in (89 mm)2.4 in (61 mm)0.7 in (17 mm)0.3 in (8 mm)0 in (0 mm)0 in (0 mm)0 in (0 mm)0 in (0 mm)0.4 in (11 mm)1.6 in (41 mm)2.9 in (74 mm)
Rainy days887310000247
Snowfall0.1 in (0.3 cm)0.2 in (0.4 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)
Sunshine199 h194 h250 h283 h327 h365 h383 h376 h315 h276 h221 h196 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

+2.4°F (+1.4°C)

Models range from +2.1°F (+1.2°C) to +2.9°F (+1.6°C)

Days above 90°F (32°C) a year

46 → 64

About 1.4× as many

Warming by month
  • January: +1.7°F (+0.9°C)
  • February: +1.3°F (+0.7°C)
  • March: +2.9°F (+1.6°C)
  • April: +2.2°F (+1.2°C)
  • May: +1.3°F (+0.7°C)
  • June: +2.6°F (+1.4°C)
  • July: +2.2°F (+1.2°C)
  • August: +2.6°F (+1.5°C)
  • September: +2.8°F (+1.6°C)
  • October: +2.1°F (+1.2°C)
  • November: +1.4°F (+0.8°C)
  • December: +2.0°F (+1.1°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.