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Willmar

United States · 2 July 2025

WillmarUnited States10:58 AM localChange location
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Average

24.5°C

low 18.7°C · high 30.7°C

Rainfall

1.1mm

rain recorded

Wind

2.1m/s

daily average

Humidity

66.5%

daily average

Cloud

10%

cover

Pressure

1013hPa

daily average

The temperature ranged from 18.7°C around 04:00 to 30.7°C around 18:00. Rain was recorded across 2 hours, from around 09:00 to 10:00 (1.1mm total).

How unusual was this day?

Compared against the same 135 calendar days (±7 days) across the other 9 years on file.

High temperature

86th percentile

Low temperature

66th percentile

Rainfall

65th percentile

Wind

17th percentile

A percentile of 100 means this was the hottest/wettest/windiest of the comparable days on file; 50 is right in the middle. This window's average temperature was 22.5°C, versus 24.5°C on this specific day.

Sun & daylight

Sunrise

05:37

Sunset

21:10

Day length

15h 32m

Hour by hour

Temperature (line) and hourly rainfall (bars), local time — America/Chicago.

↓ Download CSV
00:0006:0012:0018:0023:00

Cumulative rainfall through the day.

00:0006:0012:0018:0023:00
Local timeUTCTempFeelsRain mmWind m/sDirHumidity %Pressure hPa
00:0005:0020.7°C21.3°C02.1SSW761014
01:0006:0020.6°C21°C02.4SSW751013
02:0007:0020.6°C20.9°C02.4SSW741014
03:0008:0019.2°C19.5°C02.3SSW811013
04:0009:0018.7°C19°C02.3SSW841014
05:0010:0019°C18.6°C03.2SW821014
06:0011:0018.9°C18.5°C03.2SSW811014
07:0012:0019.3°C18.8°C03.2SSW781014
08:0013:0020.3°C20.7°C0.082.1SSW761014
09:0014:0022.6°C24.2°C0.41.1SSW711014
10:0015:0023.8°C26°C0.440.6SSE681014
11:0016:0025.3°C27.3°C0.031SSE641014
12:0017:0026.7°C28.4°C01.7SE601013
13:0018:0027.4°C28.5°C02.5SE561013
14:0019:0028.1°C29°C02.8SE551012
15:0020:0029.2°C30.2°C0.012.7SSE511012
16:0021:0029.8°C31.1°C0.012.3SSE501012
17:0022:0030.5°C31.9°C0.012.2SSE491012
18:0023:0030.7°C32.4°C01.6SE471012
19:0000:0029.9°C31.7°C0.091.4ESE501011
20:0001:0029°C31.3°C01.5ESE561011
21:0002:0026.9°C29.3°C02.1ESE681011
22:0003:0025.8°C28.1°C02.1ESE721012
23:0004:0025.6°C28°C02.3ESE741012

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Data source & coverage — ERA5 reanalysis, 2016–2025 (10 years)details
Source
ERA5 reanalysis, accessed via the Copernicus Climate Change Service (C3S) Climate Data Store
Data type
Reanalysis — a physically consistent reconstruction combining a forecast model with historical observations, not a live station reading or a forecast
Coverage
2016–2025 (10 years) for United States
Location
Willmar — 45.000°, -95.000°, ERA5 grid cell center, 14.0 km from requested point
Time zone
America/Chicago
What's shown here
The hourly and daily record for 2 July 2025 specifically — not a monthly average. See the Willmar climate overview for typical conditions.
Spatial resolution
0.25° (~25 km) distributed grid — ERA5's native model resolution is finer; this is the publicly distributed regridded product
Version / refreshed
Methodology v2026.07 · data last refreshed December 31, 2025
Limitations
A model reconstruction, not a station observation — hyper-local extremes (a single storm cell, an urban heat pocket) can differ from a nearby gauge. See the full methodology.
Attribution
Generated using Copernicus Climate Change Service information

Cite this data

Plain text
PastClimate (2026-07-20). Historical climate data for Willmar, United States (45.00°N, 95.00°W), derived from ERA5 (Hersbach et al., 2023, Copernicus Climate Change Service). Retrieved from https://www.pastclimate.com/
APA
PastClimate. (2026). Historical climate data for Willmar, United States [Data set]. Derived from ERA5 (Copernicus Climate Change Service). Retrieved July 20, 2026, from https://www.pastclimate.com/
MLA
"Historical Climate Data for Willmar, United States." PastClimate, derived from ERA5 (Copernicus Climate Change Service), July 20, 2026, www.pastclimate.com.
BibTeX
@misc{pastclimate,
  author = {PastClimate},
  title = {Historical climate data for Willmar, United States},
  year = {2026},
  note = {Derived from ERA5 (Hersbach et al., 2023), Copernicus Climate Change Service. Accessed 2026-07-20},
  url = {https://www.pastclimate.com/}
}

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